ALTO-QUEMADO_43-101-REPORT.pdf

Report on the Geology and Mineralization

of the Alto Quemado Gold-Copper Property

Near Arequipa, Peru

by

John Nebocat, P.Eng.

June 10, 2011

Prepared for Mawson Resources Ltd.

Table of Contents

1.0 Summary 12.0 Introduction 23.0 Reliance on Other Experts 24.0 Property Description and Location 25.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography 76.0 History 97.0 Geological Setting 11 7.1 Regional Geology 11 7.2 Property Geology 16 7.3 Structural Geology 238.0 Deposit Types 249.0 Mineralization 24 9.1 Ximena Vein 25 9.2 Fiorella Vein 26 9.3 La Banda Vein 26 9.4 La Lomada Vein 27 9.5 Union Vetas 27 9.6 Santa Maria Porphyry Zone 2710.0 Exploration 28 10.1 Surface Sampling—Santa Maria Target 28 10.2 IP Survey Interpretation 32 10.3 Surface Sampling: Veins and Reconnaissance 36 10.4 Underground Sampling: Ximena Vein 36 10.5 La Banda Vein 4411.0 Drilling 4612.0 Sampling Method and Approach 4613.0 Sample Preparation, Analyses and Security 4814.0 Data Verification 5015.0 Adjacent Properties 5116.0 Mineral Processing and Metallurgical Testing 5217.0 Mineral Resource and Mineral Reserve Estimates 5318.0 Interpretations and Conclusions 5319.0 Recommendations 5420.0 Budget 5421.0 References 55

Tables

Table 1. Claim Statistics 2Table 2. Ximena Vein Surface Samples, Mawson Resources 40Table 3. Ximena Vein Underground Samples, Mawson Resources 40Table 4. La Banda Vein Surface Samples, Mawson Resources 44Table 5. La Banda Vein Surface Samples, Mawson Resources 44Table 6. Projected Conceptual Target: Ximena and La Banda Veins, Mawson Resources 44Table 7. Comparison of J. Nebocat and Mawson Resources Samples, Ximena 2-3 Vein 50

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Table of Contents, Cont.d

Table 8. Comparison of BISA Samples with J. Nebocat Samples, Ximena 4 Vein 50

Figures

Fig. 1. Alto Quemado Project, Peru, Index Map 3Fig. 2. Alto Quemado Project, Peru, Department of Arequipa, Location Map 4Fig. 3. Alto Quemado Project, Peru, Claim Map 6Fig. 4. Alto Quemado Project, Peru, Regional Geology and Cretaceous Copper- Molybdenum-Gold Deposits 12Fig. 5. Alto Quemado Project, Peru, Tectonic Terranes, Southwestern Peru 14Fig. 6. Alto Quemado Project, Peru, Cretaceous to Eocene Porphyry Deposits 15Fig. 7. Alto Quemado Project, Peru, Property Geology 17Fig. 8. Alto Quemado Project, Peru, Local Geology 18Fig. 9. Alto Quemado Project, Peru, Structural Geology 19Fig. 10. Alto Quemado Project, Peru, Structural Controls, Zafranal Deposit 20Fig. 11. Alto Quemado Project, Peru, Santa Maria Zone, Sample Locations 29Fig. 12. Alto Quemado Project, Peru, Santa Maria Zone, Rock Samples—PPM Cu 30Fig. 13. Alto Quemado Project, Peru, Santa Maria Zone, Rock Samples—PPM Mo 31Fig. 14. Alto Quemado Project, Peru, Santa Maria Zone, Chargeability: 115 m Depth

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Fig. 15. Alto Quemado Project, Peru, Santa Maria Zone, Resistivity: 115 m Depth Slice 34Fig. 16. Alto Quemado Project, Peru, Santa Maria Zone, Magnetics: TMIsm RTE H 35Fig. 17. Alto Quemado Project, Peru, Regional Sampling by Company 37Fig. 18. Alto Quemado Project, Peru, Regional Sampling—Gold 38Fig. 19. Alto Quemado Project, Peru, Regional Sampling—Copper 39Fig. 20. Alto Quemado Project, Peru, Ximena 1 Vein 41Fig. 21. Alto Quemado Project, Peru, Ximena 2-3 Vein 42Fig. 22. Alto Quemado Project, Peru, Ximena 4 Vein 43Fig. 23. Alto Quemado Project, Peru, La Banda Vein 45

Appendices

Appendix I. Mawson Resources Analytical Database 56Appendix II. Selected Maps and Sections Prepared by Mawson Resources Ltd And Buenaventura Ingenieros S.A. 71Appendix III. Geophysical Images 78

Certificate of Author 83

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1.0 Summary

Mawson Resources Ltd. (the “Issuer”) entered into an option agreement with Altynor Peru SAC (“Altynor”) early in 2010 whereby the Issuer could earn 100% interest in the Alto Quemado property by acquiring 100% of the stock of Altynor. Altynor has an underlying purchase agreement with Alto Quemado Mining Company (AQMC). The 100% acquisition terms from arms length parties are based on making staged payments of US$50,000 on signing, US$550,000 on receipt of permits to drill and US$900,000 should the option with AQMC be triggered. Renegotiated terms between AQMC and Altynor state that Altynor must make a payment of €5.12M in 48 months to acquire 100% of the mining rights from AQMC. AQMC retains a net smelter return (NSR) payable at a rate between 1% and 3% dependent on the price of gold. Altynor holds the first right of refusal to purchase the NSR from AQMC.

The property is located in southern Peru in the Province of Caylloma within the Department of Arequipa, about 98 km northwest of the city of Arequipa. The property comprises seven mineral concessions totalling 3,800 hectares.

Gold mineralization was discovered fairly recently, during the mid-1990s, and the property has been exploited by informal, artisanal miners since that time. No modern, systematic exploration methods were employed prior to Altynor's involvement. Their exploration work included mapping and sampling the high grade, mesothermal Au-Cu veins and the nearby Santa Maria porphyry Cu-Mo target. An induced polarization survey was performed by the property vendor over the Santa Maria area in 1998. This data was later reprocessed by the vendor using 3-D inversion methods, and this data was rechecked by the Issuer, again using 3-D inversion techniques. The Issuer performed detailed mapping and extensive surficial and underground sampling in 2010.

The property consists of two main components: high grade, mesothermal veins along the western flank, and a partially buried porphyry Cu-Mo+/-Au target further east. The host rock is mostly an intrusive that has undergone tectonic deformation, resulting in a gneissic metamorphic texture.

There are several veins on the property, but the most significant ones exploited so far are the Ximena and La Banda veins which appear to be hosted by the same structure. This vein system has a combined length over 4 km with widths ranging from 0.3 m to 1.7 m, on average, but individual shoots can reach up to 5.4 m. There exists a conceptual target on this vein system that could average from 10 g/t to 15 g/t Au and 1.5% to 4% Cu over an average thickness of 1 m. This would equate to a minimum of 300,000 tonnes at the average grade cited above, or an in-situ potential of 200,000 gold-equivalent ounces. This estimated tonnage could likely be doubled to 600,000 tonnes.

The mapping, sampling and geophysical surveys performed over the Santa Maria zone have defined a zone of strong phyllic alteration and quartz stringers over an area roughly 800 m E-W by 450 m N-S. This area exhibits signs of strong leaching: limonite after pyrite and hematite after chalcocite. Pyrite, chalcopyrite and molybdenite were found in creeks at lower elevations largely below the level of surface weathering. Santa Maria is the most significant exploration target on the property and will be the main focus of exploration by Issuer in 2011. Alto Quemado sits along a belt containing several world-class porphyry copper-molybdenum deposits.

An exploration program, including at least 1,850 m of diamond drilling, is planned for 2011. This program is estimated to cost, including contingencies, US$762,300.

PGS Pacific Geological Services Page - 1

2.0 Introduction

Mawson Resources Ltd. (the “Issuer” or “Mawson”) acquired the Alto Quemado property (the “property”), located in southern Peru, from Altynor Peru SAC (“Altynor”) early in 2010. The Issuer comissioned the author to inspect the property and to compile all pre-existing data and current data generated by the Issuer's personnel.

Sources used in this report include: an in-house report and accompanying maps, sections and tables prepared by Mawson's Peruvian staff; a due diligence report by Buenaventura Ingenieros SA; a framework report written by Altynor for a pending 43-101 report that was not completed, including maps, drawings and appendices that accompanied said report; presentations and memoranda prepared by INGEMMET pertaining to the geology of southern Peru and the Zafranal porphyry copper-molybdenum deposit located west of the property; and various sources of maps, press releases and references found on the Internet.

The author visited the property on October 25th and 26th, 2010, sampling portions of the Ximena vein underground, the Fiorella vein, Union Vetas, la Lomada vein and the Santa Maria porphyry target areas on surface.

3.0 Reliance on Other Experts

No parts of the report were compiled by individuals not deemed to be qualified persons or equivalent. Altynor had a legal firm conduct a due diligence report in 2008 on the mineral concessions that comprise this property. Their findings indicated no liens, encumberances or debts were attached to said mineral concessions. The legal firm cautions that their research, drawn from the INGEMMET database of 2008, is only summary in nature. The author has not validated the findings of the legal firm.

4.0 Property Description and Location

The property is located in southern Peru in the Province of Caylloma within the Department of Arequipa. Access is via a good gravel road 56 km north of the the town of Pedregal which is situated along the Pan-American highway 98 km northwest of the city of Arequipa.

Alto Quemado consists of seven individual concessions totalling 3,800 hectares (ha); Table 1 lists some basic statistics.

Table 1. Claim Statistics

Concession Area (ha) Status Claim No. Date Granted Expiry Date

Alto Quemado 1 1000 Titled 10636195 02/01/95 *

Relleno 1 1000 “ “ 10332996 14/10/96 *

Soltero 1 1000 “ “ 10333496 14/10/96 *

Relleno 4 100 “ “ 10128103 04/04/03 *

Relleno 3 100 “ “ 10128003 04/04/03 *

Alto Quemado 2004 100 “ “ 10297404 17/09/04 *

* tenure is perpetual as long as the required annual fees are maintained (see below).


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MAWSON RESOURCES LTD.

ALTO QUEMADO PROJECT, PERU

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The concessions are centered roughly at UTM coordinates 813000E, 8225000N (PSAD56/18S) in the district of Lluta, province of Callyoma, department and region of Arequipa.

Due diligence prepared for Altynor by its Peruvian legal team indicated that a section of two concessions (Alto Quemado 1 & Alto Quemado 2004) have overlapping priority mineral rights owned by a separate owner who is not a party to the underlying option agreement with Alto Quemado Mining Company (AQMC). Fig. 3 shows the relative positions of these claims.

The General Mining Law of Perú is administered by the Ministry of Energy and Mines (Ministerio de Energia y Minas, “MEM” or “Ministry”). The law was changed in the mid-1990s to encourage the development of the country’s considerable mineral resources. The law defines and regulates different categories of mining activity, according to the stage of a project’s development.

Details of the law were consolidated in the ‘Single Revised Text of the General Mining Law’ of 1992 (Government document D.S. No. 014-92-EM, 19926). In summary, ownership of mineral claims is controlled by mining concessions that are established using UTM co-ordinates to define areas of interest that are measured in hectares. New concessions have to be orientated in a north-south direction; pre-existing concessions are based on the ‘punto de partido’ system and can be of any orientation. Mining titles are irrevocable and perpetual, as long as the required annual maintenance fees (derecho vigencia) are up-to-date and fully paid to MEM, by 30 June each year following granting of a concession. The fees are paid in advance. The annual fee for metallic mineral concessions is US$3/ha for each concession that is either actually acquired or pending (petitorio).

The concession holder must sustain a minimum level of annual commercial production greater than US$100/ha in gross sales before the end of the sixth year following the granting of the concession. If the concession has been put into production within the six year period, the annual rental fee remains the same, up to the beginning of year 9, when it increases to US$4/ha for years 9 to 14. The annual rental rises to US$10/ha for each year thereafter. If the concession has not been put into production within a six year period, the annual rental increases from the first semester of the seventh year to US$9 (US$3 for derecho vigencia, plus a US$6 penalty), until the minimum production level is met. If, by the start of the twelfth year from granting a concession, the minimum production level is not been achieved, the annual rental increases to US$23/ha (US$3 for derecho vigencia, plus a US$20 penalty). A concession holder can, however, be exonerated from paying penalties if he/she can demonstrate that at least ten times the penalty for the total concession was invested during the previous year. The investment must be documented and it must be accompanied by a copy of the relevant annual tax statement (‘declaración jurada de impuesto a la renta’) and payment of the annual fees. A concession will terminate if the annual rental is not paid either for three years in total over the period that the concession is held, or for two consecutive years over the period the concession is held.

To be enforceable, any and all transactions and contracts pertaining to a mining concession must be entered into a public deed and registered with the Public Mining Registry (Registro Publico de Mineria). The holder of a mining concession must also develop and operate his/her concession in a progressive manner, in compliance with applicable safety and environmental regulations, and in so doing take all necessary steps to avoid damage to third parties. The concession holder must also, at all times, allow free access to his/her concessions by those authorities responsible for assessing whether the concession holder is meeting all his/her obligations in law. (www.goldminerpulse.com).


http://www.goldminerpulse.com/

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ALTO QUEMADO PROJECT, PERUCLAIM MAP


SEE GRID PSAD56/18S MAY 15, 2010 3

Concessions owned by the Issuer

Concessions controlled bya third party not part of Issuer'sagreement with Altynor

Effective area held by the Issuer

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The issue of land tenure continues to be of significance in Perú, not least because the national cadastral system for agricultural land ownership is not always accurate. Nevertheless, the Government requires any property developer to either purchase the surface rights or make an appropriate agreement with the surface rights owner for access to a property. In the case of the holders of mining concessions, they are protected under the Perúvian Constitution and Civil Code. Their concession rights do not, however, confer ownership of the land - the owner of a mining concession must deal with the registered land owner to obtain the right of access to fulfill the production obligations inherent in the concession grant. All transactions and contracts pertaining to a mining concession must duly be registered with the Public Mining Registry in the event of subsequent disputes in law.

The Issuer does not control the surface rights on any of the concessions. All surface rights in Alto Quemado are held by the Proyecto Majes, Department of Arequipa (regional government). The Issuer is required to obtain the necessary permits to undertake exploration and exploitation activities; this has been done.

Environmental issues related to industrial activities in Peru are governed by the Consejo Nacional del Ambiente (CONAM). The Dirección General de Asuntos Ambientales of the Ministerio de Energía y Minas is the enforcing agency for mining. The Environmental and Natural Resources Law no. 613 of 1990 is in force, with regulations in Article 15 of Decreto Supremo 014-1992 and subsequent decrees. Environmental assessment reports are required for exploitation and mining. Effluent limits for mines are then published.

Further to the mineral tenure description above, claims are staked by a map/digital system—no ground location is required.

The reader is referred to Fig. 8 which shows the locations of the veins that are being worked by “Informales” (non-title holding miners). There are no tailings ponds or significant mine dumps as these workings are on narrow quartz veins (~ 1 metre wide on average) that are not generally exploited below 40 m depth. Similarly, there exist no known mineral resources or reserves on the property.

The Issuer signed a Letter of Understanding with arms length parties in March 2010 to acquire 100% of the stock of the optionor Altynor Peru SAC ("Altynor"); these terms were finalized in September 2010. Altynor holds an option to purchase 100% of the Alto Quemado gold-copper project from Alto Quemado Mining Company SAC ("AQMC"). The 100% acquisition terms from arms length parties are based on making staged payments of US$50,000 on signing, US$550,000 on receipt of permits to drill and US$900,000 should the option with AQMC be triggered.

The Issuer announced on April 27, 2011, renegotiated terms between AQMC and Altynor that state that Altynor must make a payment of €5.12M in 48 months to acquire 100% of the mining rights from AQMC. AQMC retains a net smelter return (NSR) payable at a rate between 1% and 3% dependent on the price of gold. Altynor holds the first right of refusal to purchase the NSR from AQMC.

5.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography

The property is accessible via the Panamerican highway from Arequipa, a distance of 98 km to the northwest to the town of Pedregal, a driving time of up to two hours, depending on traffic. From the main oval entering Pedregal a good quality gravel road heads northerly to the town of Huambo and beyond. Alto Quemado is accessed by this road to about the 53 km mark where a cairn of white-


painted rocks marks the road to the property, just 3 km further east. The drive from Pedregal to the property takes just over 1 hour.

Daily bus service connects Pedregal with Huanbo in each direction.

Arequipa is the second largest city in Peru and hosts an international airport with several flights a day to Lima and other cities in Peru. The Pacific Ocean port city of Matarani is located about 90 km south of Arequipa. Pedregal is a large town/small city boasting a population around 100,000. There appears to be adequate infrastructure and labour in Pedregal and environs to support on-going exploration and development on the property. Numerous buses pass by Pedregal along the Panamerican highway daily.

The small community of Lluta is located 10 km (air distance) to the north of the property and is accessible by a rough gravel road (20 km). This is the only significant human settlement within a 50 km radius from the property other than Pedregal. Most local inhabitants practice farming, ranching or are temporarily employed in small artisan mining operations in the region.

The physiography of the region is mountainous with mid-elevation rolling hills and valleys, typical of the western front of the Peruvian Andes, in a transition zone between the mountains and the coastal desert. Elevations within the property range from 2,900 m to 3,300 m with moderate relief. Bedrock exposures are common along ridgelines, steeper slopes and along the larger drainages (Benes, 2008).

Vegetation consists mostly of low perennial shrubs and cacti with occasional small trees in creek beds and gullies. Annual plants and grasses are present between December and March due to higher humidity and occasional rainfall.

Limited ranching (goats, cows) is present in the area. Indigenous species include fox, rabbit, wild chicken and small lizards, which are rarely seen.

The local climate is typical of a western Andes environment with cooler winters and mild to warm summers. Temperatures of -50C at night are not uncommon in the winters while summer temperatures range up to 250C. The rainy season in this part of the Andes is from December to March. There are no detailed precipitation records, but fog can be common throughout the rainy season, and rain may be accompanied by intense thunderstorms. Even during the rainy season precipitation is generally scarce, but during the rest of the year no clouds and intense sun conditions are the norm.

Exploration and development work can proceed on a year-round basis here. Coastal Peru is often plagued by flash floods during the rainy season, blocking road access for periods of time, but the road from Pedragal is mostly elevated outside of the drainage valley it follows.

Local resources include fresh water in one of the creek beds on the site, but at very low volumes; therefore, it will be necessary to transport more water to the site from outlying areas. The closest water source is the river at Lluta (20 km by road) or a community supply in the town of Pedregal (56 km by road). Although the site has been used by artisanal miners for the past several years, there is only limited infrastructure. At the entrance to the site there is a small house where security personnel and the area supervisor live permanently. Dirt roads with 4x4 access connect most of the sites where previous small-scale mining activities took place. No electricity is currently available at the site.


There appears to be adequate space to construct a mine, mill and suitable tailings ponds and waste dump sites. Relatively flat terrace areas exist between the camp/mine sites and the main access road which would minimize risk and environmental impact on the local drainages.

6.0 History

Gold mineralization at Alto Quemado was discovered relatively recently, during the mid-1990s. In 2001 artisanal miners completed the road connecting the property with a local access road to Pedregal and started a small scale mining operation at the Ximena vein.

Systematic exploration methods (stream sediment, soil geochemistry, trenching or drilling) were never applied at the property prior to Altynor's involvement. There was only generic geological mapping completed by the state at 1:100,000 scale. The main method for prospecting was grab sampling and the evaluation of a pan concentrate. Artisanal miners were targeting outcrops of quartz-hematite, quartz-sulphide and quartz-limonite veins. When visible gold was identified, miners sank shallow exploration shafts and started to follow veins by underground drifts. There are no records of systematic grade control during artisanal mining, and “ore” was identified visually. Economic “ore” was considered by the artisanal miners to be any mineralized material with grades over 30 g/t Au.

In May 1998, XIMESA S.R.L contracted Val D'Or Geofisica to perform ground magnetic and induced polarization (IP) surveys over the Santa Maria porphyry area centered a few hundred meters east of the precious metal veins.

The pole-dipole array was used with readings taken 50 m apart and separations to n=6, along lines oriented north-south. The total distance surveyed was 19.8 km. Instrumentation used included an Iris model ELREC-6 receiver and a HUNTEC MK-II transmitter.

Using the same lines, the magnetic survey spanned a total distance of 16.6 km with readings taken every 10 m. The instrument used for the magnetic survey was a GEM model GSM-19.

XIMESA S.R.L. commissioned Val D'Or in 2004 to reprocess and reinterpret the data using 3-D inversion modelling.

This data was again reprocessed and interpreted for the Issuer by D. McInnes in 2010, so no maps or images of these original results will be presented here. Val D'Or's conclusions indicated the following:

1) The IP results indicate an important concentration of disseminated sulphides throughout the survey area. Sulphides outcrop in the lower levels of the creeks, but the bulk of the mineralization is covered.

2) Low resistivity values are associated with high chargeability anomalies and areas of advanced argillic alteration.

The conclusions by McInnes support those made by Val D'Or.

Between the 6th and 14th of December, 2003, Buenaventura Ingenieros SA. (BISA) examined the property as part of a due diligence appraisal. Their focus seemed to be to evaluate the potential of the high grade veins. BISA took 132 rock samples which include 80 outcrop samples, 30 samples from the vein


workings, 20 samples representing hydrothermal alteration, 2 grab samples and 12 duplicates (Osorio, 2003).

During this time, in addition to sampling, they produced a regional geology map, a schematic cross-section of the regional geology, a longitudinal section from northwest of the Ximena 4 vein to southeast of La Banda vein, a long section of Ximena 4 vein, geochemical plans showing Cu, Mo and Au values, mostly from Santa Maria zone, and a reproduction of the Val D'Or geophysical survey results. The locations and results of their underground sampling was shown on the sections.

BISA concluded that the veins were too small to be of interest to their company and that the porphyry target may be a distal phenomenon. The lack of gold in the samples taken from the porphyry target seemed to be a negative point with them.

During 2006, AQMC performed a surface grab sampling program on the property. Of the 72 samples collected, 13 taken from the Ximena vein averaged 19.98 g/t Au and 2.48% Cu. These results were what interested Altynor enough to option the property from AQMC (Benes, 2008).

Prior to Altynor’s involvement, the miners were permitted by the owner of AQMC to mine only oxide ore. Consequently, due to this restriction, they were mining only to an average depth of 35 m.

During Altynor's initial visits to the property they found six primitive shafts and adits operating at four different veins. According to the supervisor of this operation, appointed by AQMC, they were producing some 100 t-150 t of oxide ore per month at an average grade between 30 g/t and 40 g/t Au. This ore was trucked 400 km north to the town of Chala where it was sold to the processing plant “Belen” owned by Minera Titan del Peru SRL. Altynor did not know the terms of the sale agreement with the plant nor did they have any records of sales.

This limited mining operation stopped with the execution of the Letter of Intent between Altynor and AQMC executed on November 9th 2007.

In 2007, Altynor completed a reconnaissance survey of the property and collected a total of 117 samples with the purpose of checking the results of sampling done by the previous owner and to extend the program to the deeper levels of Ximena, Fiorella and La Banda veins. From the total of 117 samples, 33 were collected from Ximena, 22 from Fiorella, 7 from La Banda, 18 from La Lomada, 19 from Santa Maria, 9 from Union Veta (segment connecting Ximena and La Banda) and 9 samples collected during reconnaissance mapping outside of the vein areas.

Altynor compiled the sampling done in 2006 and 2007 in an extensive report including maps, sections and tables from which the author obtained considerable background information.

A 1:5,000 scale geology map was also completed in 2007. Altynor stated that mapping helped in finding new vein splays and further defining the Santa Maria porphyry target. Mapping also suggested that vein mineralization favours the “basement metamorphic” rocks as a host, but not exclusively; and in some cases when it extends into igneous rocks, the style of mineralization changes from vein to stockwork, as in the case of La Lomada. Overall strike and geometries of individual veins indicate that a long-lived NW trending deep crustal structure, which defines not only the block of “metamorphic basement” rocks, but also the emplacement of later intrusives, played the principal role in the regional metallogeny and genesis of Alto Quemado’s gold-copper system.


Portal Resources, during their due diligence assessment of the property in 2008, collected 112 surface rock samples; most were from the main areas of interest.

During 2010, Mawson created a 1:5,000 scale geology map, a 1:1,000 scale surface map of the vein areas, a 1:500 scale map of the underground workings and a 1:25,000 scale regional map of the property. A total of 505 samples were collected: 400 from surface outcroppings, 65 from the veins underground, 13 soil samples and 27 sample standards and sample blanks were included for quality control.

Overall, the Issuer was satisfied with the results obtained.

There exist no known mineral resources or reserves on the property. No appreciable amount of modern exploration has yet been done on the property prior to the Issuer's involvement to advance it to the drilling stage. Production from the narrow veins (~1 m average thickness) is not known, but considering the size of the veins, what was observed underground and on the dumps, mining within the last 10 years has probably amounted to no more than the 1000's to 10,000's of tonnes order of magnitude.

7.0 Geological Setting

7 .1 Regional Geology

Southern Peru has a long history of mining and exploration, being the district that hosts the country's most significant porphyry copper +/- molybdenum deposits. World class deposits in the area SE and NW of Arequipa include Toquepala, Cuajone, Quellaveco, Cerro Verde and others.

In terms of the regional tectonic setting, the project lies in the Western Cordillera of southern Peru which comprises segments of Proterozoic and Paleozoic basement rocks (Arequipa terrane), Cretaceous and Tertiary volcanic and sedimentary rocks, together with the Coastal Batholith, which forms an elongate belt of granitic rocks extending along Peru's coastal region from Arequipa to Trujillo.

The Coastal Batholith is over 100 km wide and extends discontinuously for 1,500 km north-south. It was created by the subduction of the Nazca Plate beneath the South American Plate during the Late Cretaceous to Early Tertiary time with the resulting melting and magmatic fractionation of crustal and upper mantle rocks. The most productive metallogenic cycles responsible for gold-copper and porphyry deposits (e.g. Cerro Verde) are the Cretaceous magmatic event (Peruvian orogeny) and late Paleogene-Neogene magmatic cycles: Incaic I, Incaic II and Quechua, responsible for Yanachocha, Tintaya, Cerro de Pasco, Antamina and other deposits.

Within the project area the intrusive rocks are composed mostly of calc-alkaline tonalites and granodiorites belonging to the Arequipa segment of the Coastal batholith. These had been previously attributed to the Tiabaya super unit of the batholith, dated between 86 and 74 Ma, but recent age dates derived from a coarse grained granodiorite in the Ocoña valley have yielded potassium-argon dates from biotite of 137 +/- 1.8 Ma and 136 +/- 1.7 Ma (Schildgen, 2009). These appear to be the same intrusives found along the southern edge of Alto Quemado.

These units are intruded by small stocks of quartz monzonite, dacites and porphyritic dykes. These later intrusives are believed to be contemporaneous with the mineralized porphyries along the “X” metallogenic belt, including Puquio (77.48 +/- 0.53 Ma to 75.34 +/- 0.40 Ma) and Pucacorral Sur (82



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Ma). The mineralized intrusives at the nearby Zafranal deposit, namely the Zafranal diorite and microdiorite, have yielded similar ages (Mamani & Rivera, 2011), and these rocks appear similar to the quartz monzonite and monzodiorites found at Alto Quemado.

The Peruvian department of mines and geology (INGEMMET) has been conducting advanced mapping and research in the Arequipa area and environs in recent years. The following summary is extracted from a Powerpoint presentation made by INGEMMET (Carlotto, et al, 2010) for their 30th

anniversary. It deals with the tectonic evolution and metallogenesis from the Proterozoic to Cenozoic in southern Peru.

During Proterozoic time, the Arequipa terrane was accreted to the Amazonian craton, flanked by the Paracas terrane to the north and the Antofalla terrane to the south. This event is believed to have occured c. 1000 Ma during the Sunsas or Grenville orogeny.

In the early Paleozoic, subduction ocurred under the Arequipa block, bounded to the northwest by the Abancay deflection that separates the Arequipa terrane to the SE from the Paracas terrane to the NW. An Ordovician magmatic arc was formed due to the subduction, behind which was created the Altiplano retroarc basin and a clastic platform resting on the Amazonian craton. The Cincha-Lluta-Incapuquio fault system developed during this time, separating the Arequipa block from the Altiplano retroarc basin.

During Permo-Triassic time, the Mitu group was deposited and contemporaneous intrusives were unroofed in the Eastern Cordillera.

In the Mesozoic, between 200 Ma and 65 Ma, renewed subduction occurred, creating a magmatic/volcanic arc. Between this arc and the Cuzco-Alto-Puno rise, or arch, the Arequipa, or Occidental, basin was deposited. At the same time the Oriental basin was being formed east of the Cuzco-Alto-Puno arch.

Continued subduction in the late Mesozoic initiated NW-SE directed, dextral, transpressive movement along the Cincha-Lluta-Incapuquio fault system. To the NW the fault merges with the ENE-WSW trending Iquipi fault system (see Figs. 5 & 6).

The most important porphyry Cu-Mo+/-Au deposits were formed during Paleocene-Eocene time; these include Cerro Verde, Toquepala, Cuajone, Quellaveco, Palca and La Mancha. These deposits roughly follow the Cincha-Lluta-Incapuquio fault system.

Alto Quemado and the nearby Zafranal porphyry deposit occur near the southern end of a belt of Cretaceous age porphyry deposits that overlaps laterally with the belt of Paleocene-Eocene porphyries described above (Fig. 6). The location of this belt of porphyries is believed to have been largely controlled by the transpressive Incapuquio-(Cincha-Lluta) fault system (Rivera, 2010).

The Zafranal porphyry deposit is located about 15 km due west of Alto Quemado. Recent interpretations by Minera AQM Copper Peru, SAC suggest that the porphyry was emplaced as a lenticular body within an east-west trending tectono-morphic fault that splays off the Incapuquio-Cincha-Lluta fault system. The Zafranal porphyry system is located within a “jog” of this east-west




TECTONIC TERRANES

SOUTHWESTERN PERU


N.A. N.A. MAY 15, 2011 5


After Carlotto, et al, 2010


CRETACEOUS TO EOCENE

PORPHYRY DEPOSITS


N.A. N.A. MAY 15, 2011 6



After Carlotto, et al, 2010

0 300 Km

Department boundary

Major city

Paleocene boundary

Cretaceous boundary

Cretaceous porphyry (radiometric date)

Cretaceous porphyry question

Paleocene Porphyry (major mine)

Puquio sub-boundary

Zafranal sub-boundary

LEGEND

transpressive fault splay, and faults internal to the porphyry, which trend about 1350AZ, indicate a dextral movement along this major structure (Figs. 9 & 10).

A roughly 7 km wide by 170 km long belt of foliated and metamorphic rocks, previously interpreted as Proterozoic gneisses, occurs immediately south of the Cincha-Lluta/Incapuquio fault system. Within the areas of Zafranal and Alto Quemado properties, the rock is foliated with alternating facies of granite and diorite. The granitic phase is pink, rich in potassic feldspar, and the quartz grains have an undulating extinction viewed in thin section. The dioritic phase is mafic with plagioclase, hornblende and/or pyroxene and magnetite. These rocks have undergone chlorite-epidote grade metamorphism. Microscopically, the rock has a cataclastic texture and nowhere exhibits regional scale metamorphic paragenesis as is found in the Macizo de Arequipa basement (Chavez, 2010). The Issuer has interpreted the “gneissic” rocks found at Alto Quemado to be entirely of this cataclastic or mylonitic tectonic event that pre-dates the emplacement the oldest undeformed intrusion found on the property (+/- 136 Ma); xenoliths of the deformed rocks have been observed within the granodiorite that intrudes them.

The NW-SE trending Cincha--Lluta fault system is the northernmost extension of the Incapuquio faults that controlled the emplacement of the giant Paleocene porphyry Cu-Mo deposits found in southern Peru: Cerro Verde (1.0 BT @ 0.51% Cu); Chapi (191 MT @ 0.60% Cu); El Calatos (926 MT @ 0.37% Cu, 0.03% Mo); Cuajone (1.2 BT @ 0.64% Cu); Quellaveco (1.5 BT @ 0.60% Cu, 0.02% Mo) and Toquepala (2.1 BT @ 0.61% Cu). This system is also the northern extension of the Domeyko fault system in Chile that controlled the emplacement of world-class Eocene-Oligocene porphyry deposits such as Collahuasi (4.1 BT @ 0.83% Cu), Quebrada Blanca (1.1 BT @ 0.72% Cu), El Abra (1.6 BT @ 0.62% Cu), Chuquicamata (17.1 BT @ 0.65% Cu), La Escondida (4.9 BT @ 0.92% Cu) among others.

These series of NW-SE trending faults displayed a normal movement during Jurassic and Cretaceous times, controlling the deposition of the Arequipa basin. However, in the late Cretaceous (c. 85 Ma), a reversal in tectonic directions placed Proterozoic (?) lithologies atop the Mesozoic rocks of the Arequipa basin along the northern block.

The Iquipi, or major Clavelinas-Iquipi fault system, is a belt up to 90 km wide east-west at latitude 160S. This is also a transition zone between two geologic domains—the Paracas domain to the north and the Arequipa domain to the south, identified in part through Pb and Nd isotope studies (Mamani, et al, 2008, 2010).

7 .2 Property Geology

The regional property map made by BISA in 2003 shows the upper Jurassic Yura group, consisting mainly of sandstone, quartzite and lesser shale, occuring in the northeastern part of the property. This is in turn overlain by the lower Cretaceous Murco formation consisting of red to grey shales and sandstones. Both these units are deemed to be in fault contact with granodiorite to the south, believed to belong to the Coastal Batholith of late Cretaceous to early Tertiary age.


Andahua Formation:Quaternary basaltUnconformityMurco Formation:red sandstone, shale

YURA GROUPHualhuani Formation:quartz arenitesGramadal & Labra Formations:gray shales & sandstones, thinbedded limestone

Quartz monzoniteMonzonite & dioriteGranodioriteGranodiorite (batholith - 136 Ma)Deformed intrusiveFine grained grained granodiorite?

FaultsMesothermal veins

Foliation in deformed intrusive

Claim perimeter 0 2.0 4.0 Km

Sedimentary & Volcanic Rocks Intrusive Rocks



PROPERTY GEOLOGY


SEE BAR PSAD 56/18S MAY 15, 2011 7


35°

40°

50°

55°

40°

LA BANDA VEIN

SANTA MARIAPORPHYRY TARGET

LA LOMADA VEIN

Totorayoc FaultUNION VETAS

FIORELLA VEIN

Guanaco Fault

Zorro Andino Fault

XIMENA VEINToro Bravo FaultVenado Fault

Viscacha Fault

812000 m E810000 m E

8224000 m N

8222000 m N

2,900

3,000

3,100

3,200

3,300

3,400

3,500

3,200

3,30

0

45°45°45°45°45°45°45°45°45°

Veins

Faults

Orientation of TectonicBanding

Monzodiorite/Diorite Dyke

Granodiorite (Cretaceous?)

Quartz Monzonite Dyke

Deformed Intrusive

Granodiorite (Batholith, 136 M

FIGURE:

ALTO QUEMADO PROJECT, PERULOCAL GEOLOGY


PROJECTION: DATE:


SCALE:

PGS Pacific G


Cincha-Lluta/Incapuquio Fault

35°

40°

50°

55°

40°

LA BANDA VEIN


LA LOMADA VEINTotorayoc Fault

UNION VETAS

FIORELLA VEIN

Guanaco Fault

Zorro Andino Fault

XIMENA VEINToro Bravo FaultVenado Fault

Viscacha Fault

2,900

3,000

3,100

3,200

3,300

3,400

3,500

3,200

3,30

0

814000 m E812000 m E810000 m E

8224000 m N

8222000 m N

8226000 m N

808000 m E

Hualhuani Formation:quartz arenites

UnconformityUnconformityUnconformityUnconformityUnconformityUnconformityUnconformityUnconformityUnconformity

Murco Formation:red sandstone, shale

YURA GROUP

Road

Claim perimeter

Andahua Formation:Quaternary basalt

LEGEND

45°45°45°45°45°45°45°45°45°

Veins

Faults





Deformed Intrusive

Granodiorite (Batholith, 136 Ma)

FIGURE:

ALTO QUEMADO PROJECT, PERUSTRUCTURAL GEOLOGY


PROJECTION: DATE:


SCALE:


STRUCTURAL MODEL

CINCHA-LLUTA/

INCAPUQUIO SYSTEM

CLAVELINAS-IQUIPI SYSTEM

Fiorella

CINCHA-LLUTA/

INCAPUQUIO SYSTEM

Toro Bravo Fault

Venado Fault

Guanaco Fault

Ximena



STRUCTURAL CONTROLS

ZAFRANAL DEPOSIT


SEE GRID PSAD 56/18S MAY 15, 2011 10

PG

SP

acificG

eolo

gical

Serv

icesP

age

20 After Carlotto, et al, 2010

BISA describes the intrusive as a holocrystalline granodiorite, locally grading into granite or tonalite, noticed particularly on the Santa Maria hill. They do not describe these rocks as having an extensive oriented, metamorphic appearance, but they do mention that the mafic minerals show some lineation at the Santa Maria zone. Diorite is noted as occuring in the creeks flanking this hill (Osorio, 2003).

Two types of dykes, one felsic, the other more intermediate in composition, were noted.

Altynor described the local geology at Alto Quemado as consisting of highly metamorphosed rocks of the de la Costa complex represented by gneisses, granite-gneisses, amphibolites, quartzite andmicas schist, interpreted as being originally sedimentary rocks regionally metamorphosed into amphibolite facies. The state geological map indicates that the de la Costa complex consists of Proterozoic metamorphic rocks locally intruded by Ordovician granites and granite-gneisses. Altynor was of the opinion that the representation of Ordovician granites on the state geological map is exaggerated as these can be distinguished only with difficulties from Proterozoic metamorphic rocks. This interpretation has for the most part been discounted.

To the east and north of de la Costa block, the property geology is dominated by Cretaceous intrusive represented by quartz diorite, granodiorite and tonalite. Typically, the contact between intrusive and metamorphic rocks is structural with the intrusive rocks representing the early phase of Incaic I granitic complex. The second phase is represented by small intrusive stocks and dikes of gabbro-diorite, diorite and monzodiorite.

Altynor defined two systems of NW trending faults which border a graben-line structure from southwest and northeast. The two faults are slightly oblique with respect to each other, which might result in graben closing towards the northwest. They speculated further that the left-lateral shear movement along the fault at the SW border (Cerro Quemado shear zone) caused intensive block fragmentation, which together with the development of secondary splay faults, controlled emplacement of later gold-copper mineralization. Possibly, similar movements along the fault at the northeast border resulted in the development of secondary faults cross-cutting mineralization.

Beside the structural control, it appears that lithology also played an important role in the localization of mineralization. It is apparent that the best developed continuous sections of mineralization are hosted by the foliated rocks; veins in granites are typically narrower and contain lower grades.

The Issuer's detailed mapping has confirmed, and in parts, completed altered the interpretations made by previous explorers. As noted by others, the oldest rocks on the property belong to the Yura group along the northern part of the property. The Yura consists dominantly of white quartzites in beds from 0.2 m to 2.0 m thickness and are believed to be part of the Haulhauni formation which is underlain by shales with subordinate interbeds of fine sandstone and siltstone belonging to the Murco formation. This latter formation is in direct contact with the deformed intrusive caused by the Cincha-Lluta fault which in this area trends E-W.

The deformed intrusive is the principal unit that outcrops on the property. It forms a roughly inverted triangular wedge bounded to the north by the Cincha-Lluta fault and to the south by the NW-SE trending Toro Bravo fault.

The Issuer's geologists have provided a different interpretation regarding the “metamorphic” rocks on the property. It is their contention that the metamorphic fabric in the crystalline rocks is a result of


tectonic deformation along a large scale east-west trending fault system, as was described by others in the previous section of this report. The author noticed that these deformed rocks are not generally well indurated but rather friable. There appears to be a lighter coloured phase (granitic composition) that intercalates with a darker phase (dioritic origin). Also, the “metamorphic” mineralogy is not high grade, megascopically consisting of amphiboles and random clots of epidote; this was described earlier as well It is conjectured that this is the same structure that passes through the Zafranal deposit 15 km to the west.

These deformed, cataclastic and mylonitic rocks are intruded by a younger granodiorite body to the south and southeast. This intrusion does not have the same foliated/banded fabric as the rocks described previously. The granodiorite is equigranular and contains hornblende and biotite that are weakly altered to chlorite and epidote.

Two types of dykes cut through both of these units: a quartz monzonite porphyry and a monzodiorite phase. It was not observed if one of these dykes cuts across the other, but the diorite dyke is seen paralleling the late-stage quartz veins in several places.

The quartz monzonite porphyry dykes trend NW-SE to E-W and occupy the Guanaco fault. The dykes range in width from a few to tens of metres, and along the Guanaco fault cut the Santa Maria porphyry zone. They contain moderate amounts of “D type” veins consisting of quartz-pyrite-chalcopyrite-molybdenite; pyrite and chalcopyrite are replaced by hematite. These appear to be intra-mineral dykes (Ligarda, et al, 2011).

The monzodiorite porphyry occurs as dykes trending NW-SE and/or as stocks cutting both the older deformed intrusion and the younger granodiorite. Petrographic studies show it contains abundant plagioclase and elongated light to dark green hornblende phenocrysts. Alteration consists of epidote and chlorite replacement of hornblende, and feldspars show incipient replacement by phyllosilicates of up to 40%. Kaolinite is not observed, and pyrite is rare, being replaced by geothite.

Both of these dykes are related to mineralization at Alto Quemado where they crosscut the older deformed intrusive. Strong phyllic alteration is developed along their margins. The Issuer has found two 80 m wide monzodiorite dykes about 500 m east of their base camp exhibiting strong phyllic and minor secondary biotite alteration along their contacts with the deformed host rock. This may indicate a hidden porphyry target at depth; the Santa Maria chargeability anomaly, although weak, extends to here.

In addition, it was observed that all the high grade Au-Cu veins are directly associated with porphyritic diorite/monzodiorite dykes, containing weak to moderate chlorite alteration. These dykes range from a few to 10 m in width and occur along faults trending in different directions.

The granodiorite is a fresh light coloured and coarse-grained unit that was described above. It is located in the southwestern part of the property and is in faulted contact with the older deformed intrusive. It had been previously grouped with the Tiabaya super unit of the Coastal batholith, but recent age dates have given it a much older date, in the 137-136 Ma range.

Along the contact with the older intrusion exists a 50 m wide intra-granodiorite zone that has been


strongly foliated to schist; this is believed to be similar to the tectonic setting along the Iquipi fault at the Zafranal project. Here, it is called the Toro Bravo fault (see Figs. 8 & 9).

7.3 Structural Geology

The project is located at the confluence of the NW-SE trending Cincha-Lluta/Incapuquio fault system and the E-W trending Clavelinas-Iquipi system. The interaction between these two structural regimes has created a region of “pull apart” tectonics whereby mineralized structures such as Ximena and Fiorella veins occupy faults behaving as Reidel shear planes. It was this setting that allowed late Cretaceous (?) intrusions and subsequent mineralization to be emplaced (Romero, et al, 2002). These major faults had a polyphase history during the entire Andean orogeny, and as a result of changes in the directions of converging tectonic plates, making accurate models of the kinematics is difficult.

The following fault systems have been recognized on or near the property:

• NW-SE system: Cincha-Lluta/Incapuquio, Toro Bravo and Viscacha• E-W system: Clavelinas-Iquipi, Guanaco and Venado• WNW-ESE system: Ximena, Fiorella and La Banda veins• N-S system: Zorro Andino and Totorayoc

The only NW-SE fault of the Cincha-Lluta/Incapuquio system identified on the property is Toro Bravo. It is a faulted contact between the older deformed intrusions to the NE and the younger, coarse grained granodiorite to the SW. Along this contact exists a roughly 50 m wide corridor of schistose rock that is believed to be very similar to what is found at the Iquipi fault zone at the Zafranal deposit to the west.

Near the top end of the project, the Cinch-Lluta thrust fault changes direction from its more normal NW-SE trend to an E-W trend. The Issuer has recognized two other faults parallel to this E-W trend. To the north, the Guanaco fault forms the northern boundary of observed alteration at the Santa Maria zone, and the fault is occupied by a quartz monzonite dyke. About 600 m to the south from here exists another parallel fault called Venado. This fault seems to have controlled the emplacement of narrow milky-white quartz veins and has affected sinistral fault movement along the Ximena and Fiorella veins.

This collection of structures creates a significant exporation target as they appear to be of the same style that controls the mineralization at the Zafranal deposit 15 km to the west.

The WNW-ESE system has controlled the structures that host the hydrothermal breccias and mineralized veins along the Ximena, Fiorella, La Banda and La Lomada veins. Also, they seem to be the principal host to many of the microdiorite, quartz monzonite, monzodiorite and diorite dykes found on the property; the movement seems to be sinistral.

The N-S trending system, which varies to NNW-SSE, is an important but post-mineral system. One of these, called Zorro Andino, occurs near the Veta Union showing (see Fig. 8). There exists here a 30 m wide shear zone along which the western limit of phyllic alteration from the Santa Maria zone is observed. The western side of this shear zone is believed to be down-dropped, and it is possible


that the extension of the Santa Maria porphyry target may exist at depth on this side, as indicated by the deeper level chargeability and resistivity anomalies. Microdiorite dykes occur along this fault trend.

The persistent foliation observed in the deformed intrusive, despite being somewhat chaotic, has a general E-W direction and a dip generally steeper than 300 to the north. This direction is parallel to the documented Clavelinas-Iquipi fault system and is believed to be the controlling dynamic metamorphism in the area (Ligarda, et al, 2011).

8.0 Deposit Types

Alto Quemado’s mineralized system is a mesothermal, low-sulfidation to intermediate gold-copper, quartz-sulphide and sulphide vein type. Besides vein type, the property also has some geological characteristics typical for a porphyry gold-copper system analogous to the Pimenton deposit in Chile (Benes, 2008).

The principal veins have a known combined length of over 4 km with widths ranging from 0.3 m to 1.70 m. Individual ore shoots can reach widths of up to 5.40 m. The average width of the mineralized structure (vein, mineralization and alteration envelope) is about 1.0 m. The Issuer has identified three important vein structures: Ximena, with a strike of 2.0 km, Fiorella over 1.2 km strike and La Banda with a strike of 0.9 km. A fourth vein, called La Lomada, is narrow (<0.6 m) and has two branches striking over 0.6 km length. Other minor veins exist in the project area but are not considered to have any economic potential.

The Santa Maria porphyry Cu-Mo-(Au) target has a phyllic alteration envelope 800 m E-W by 450 m N-S. Surface rock samples in the leached layer yielded results between 250 ppm and 800 ppm Cu; Mo values were also anomalous, locally exceeding 30 ppm.

9.0 Mineralization

The mineralization is comprised of (a) economic minerals - pyrite, chalcopyrite (CuFeS2), chalcocite

(Cu2S), bornite (Cu

5FeS

4), covellite (CuS), malachite, azurite, native gold and (b) gangue minerals -

quartz, sericite, chlorite, epidote, K-feldspar, micas, kaolin, carbonate, barite, hematite, limonite. Supergene enrichment is present as covellite>chalcocite (after chalcopyrite and bornite), and oxides derived from copper, iron and manganese including malachite, azurite, chrysocolla, geothite, jarosite, hematite (after chalcocite) and neotocite. There exists a zone of secondary enrichment where chalcocite replaces chalcopyrite over a vertical range between 10 m and 20 m. Gangue minerals consist of coarse cyrstalline quartz, chlorite, epidote, sericite and lesser carbonates and barite. Sulfide content within the veins is relatively high for hydrothermal mineralization, in the range of 10% to 40%. Chalcocite, bornite and covellite dominate the zone of secondary enrichment, while chalcopyrite prevails in the primary sulfide zone. Textures vary from massive to veinlets to disseminated. Gold is visible with a grain size of 0.1 mm-0.3 mm. The ratio between Au/Ag varies from 1:1 in low grade material (<10 g/t Au) up to 5:1 in high grade. Copper content differs for various veins from 1% up to 20%. The zone of weathering is well developed here as it is common for regions with high temperatures and large variations in humidity. The thickness of oxide mineralization varies from 20 m up to 60 m (Benes, 2008).

In the Santa Maria porphyry target area and adjacent Totorayac Creek are found traces of chalcopyrite,


pyrite and molybdenite in narrow quartz veinlets enveloped with strong sericite (phyllic) alteration. Incipient leaching has largely destroyed the surficial sulphides, but there is evidence of hematite derived from chalcocite. This indicates strong leaching in the system subsequent to a phase of supergene enrichment. In the streambeds are also found malachite, chalcanthite, neotocite and traces of chalcocite.

9.1 Ximena Vein

Ximena is the most important mineralized structure at the property; it has a strike of between 1100

azimuth and 1200 azimuth and a dip between 650 and 800 to the northeast. However, its aggregate surface exposure is only 1.4 km, and thicknesses vary from 0.3 m to 1.7 m.

Ximena, like all the veins at Alto Quemado, is emplaced along fault structures which channeled mineralizing fluids as well as hydrothermal breccias with a specularite (hematite) matrix supporting angular silicified clasts. Locally these are associated with propylitized microdiorite dykes parallel to the veins and locally forming richer mineralized shoots.

Petrographic work has identified two generations of brecciation, including a phase of pyrite before the introduction of chalcopyrite. Quartz is early with respect to sulphides, filling veins and the matrix of the hydrothermal breccias in the first phase. Pyrite occurs as grains between the quartz and as breccias. A second generation of brecciation is represented by late chlorite with respect to sulphides. The brecciated pyrite is filled with chalcopyrite that has replaced it. Incipient supergene enrichment is represented by weak replacement of chalcopyrite with chalcocite and covellite; the covellite replaces the chalcocite. The ratio of covellite to chalcocite is high, suggesting only a weak enrichment (Chavez, 2010).

Samples collected by Altynor at Ximena range from 8 g/t Au to 65 g/t Au with a maximum of 181g/t Au and an average of 42 g/t Au, 13.4 g/t Ag and 9.3% Cu.

The longitudinal section in Appendix II, created by BISA, shows a very generalized contact zone between the sulphide-rich horizon at depth and the leached layer above; Altynor drew their interpretations in part from the work done by BISA.

Due to limited access, Altynor systematically sampled only the vein itself containing quartz-sulfide matrix and were not able to properly evaluate the mineralization contained in the wall rock and splay faults.

The current work by the Issuer confirms that primary areas of interest along the Ximena structure are the Ximena 1, Ximena 2, Ximena 3 and Ximena 4 vein workings (see Fig. 9). These workings have an aggregate strike length of 400 m and an average width of about 1.0 m. Only modest values of Au and Cu were obtained from surface, the best being: 0.40 m @ 4.5 g/t Au and 0.2% Cu (sample 217815); 2.4 m @ 1.00 g/t Au and 0.7% Cu (sample 217957). However, 20 m below the surface, Au and Cu values improve markedly: 1.70 m @ 9.50 g/t Au and 14.20% Cu (samples 218314-218316); 1.30 m @ 9.55 g/t Au and 5.78% Cu (samples 218310-218311); 1.90 m @ 7.80 g/t Au and 9.79% Cu (samples 218310, 218321); 1.10 m @ 7.40 g/t Au and 0.31% Cu (samples 218336-218337).

The mining activities undertaken here have been carried out by informal miners (informales) authorized by the property owner (R. Bejarano).


9.2 Fiorella Vein

The Fiorella vein appears to be controlled by the splay structure associated with Ximena vein and trends between 1200 azimuth and 1400 azimuth with dips between 600 and 750 north. The vein has a known length of 1.2 km, and its thickness varies from 0.3 m to 1.2 m with an average of 0.70 m. The cumulative outcrop exposure of the vein is 0.75 km.

This vein has not been extensively worked by the artisanal miners, reaching depths of only 3 m - 4 m. The central part of the vein has an ore shoot about 130 m long with widths from 0.30 m to 1.20 m. The surface sampling done by the Issuer yielded values of up to 2.50 g/t Au and 0.30% Cu; however, it is possible that the grades may improve with depth just as they did at Ximena.

Altynor's sampling at the surface yielded results that ranged between 1.5 g/t and 6.6 g/t Au with one sample running as high as 60 g/t Au, and the average value from all their surface samples ran 13.15 g/t Au, 4.5 g/t Ag and 0.95% Cu.

Another ore shoot exists at the southeast end of the vein that seems to be connected with the Ximena vein. Both are crossed by an E-W fault in this area where the grade also improves: 1.10 m @ 11.4 g/t Au and 1.10% Cu (sample 217974).

9.3 La Banda Vein

La Banda is located some 800 m SE from the Ximena vein and appears to be its southern continuation (Figs. 8 & 9). It can be followed continuously for 0.9 km and has a general trend of 1100 azimuth, breaking locally to 0800 azimuth, with dips from 500 to 700 to the north. The vein's widths vary from 0.8 m to 5.4 m, averaging 1.1 m. Its geometry differs from Ximena by having less sharp vein contacts, swelling, and extensions of mineralization into the wall rock reaching in some areas up to 5 m – 6 m thickness. The footwall contains a silicified and propylitized diorite dyke in addition to hydrothermal breccias. Both the altered dyke and breccias increase the size potential for mineralization at La Banda.

The vein has been worked by artisanal miners at its eastern end for just over 120 m length and up to 42 m depth. In this sector exist anomalous values for Au and Cu in surface samples; the best weighted value is 5.4 m @ 2.10 g/t Au and 1.60% Cu (samples 217890 – 217896). At depth occur better values, such as 1.2 m @ 16.52 g/t Au and 3.5% Cu (samples 218339 – 218340); 0.85 m @ 85.16 g/t Au and 0.72% Cu (samples 218341 – 218342); 1.0 m @ 8.76 g/t Au and 3.40% Cu (sample 218349).

The rest of the vein's surface outcrops yielded fairly low levels in Au, but it is anomalous in Cu, yielding values between 0.10% and 0.50% Cu over 500 m length and 1.0 m width, on average. This vein, like the others, has the potential to improve with depth in the area of these low grade surface samples.

According to the supervisor of artisanal miners, gold grades in ore produced from La Banda ranged from 40 g/t to 60 g/t Au. Altynor's sampling returned 46.8 g/t Au, 18.15 g/t Ag and 1.41% Cu, but they did not state if this was the average of the 7 samples they collected.

Reconnaissance mapping indicates that the apparent vertical extent of mineralization, in topography along the dip of the vein, is more than 150 m.


9.4 La Lomada Vein

In this area there are several narrow, parallel veins of which only two are significant. Both of these trend at 1300 azimuth with dips between 700 and 850 to the NE. The total length is about 600 m, but the veins are narror, ranging from 0.2 m to 0.8 m and averaging 0.4 m. The Au and Cu values are constant with the best value returning 0.33 m @ 29.50 g/t Au and 0.23% Cu (sample 218204); 0.30 m @ 12.10 g/t Au and 0.70% Cu (sample 218238).

This is one of the areas visited by the author during the field inspection. It would appear that the term “linear stockwork”, coined by Altynor in their report, overstates the distribution of silicification and alteration, and there appears to be basically just two parallel veins about 40 m apart with fairly barren looking rock between them.

9.5 Union Vetas

It was originally believed that the Ximena and Fiorella veins joined in this area, hence the name. However, mapping has revealed that this area is actually part of the deformed intrusive sitting on top of the granodiorite much like a roof pendant. The nearby Zorro Andino fault, trending 1600 azimuth, has imparted parallel structures here, giving the appearance of veins. Gold and copper values are not significant, so this area has low potential for exploration.

9.6 Santa Maria Porphyry Zone

Santa Maria is located some 500 m NE from Union Vetas, the splay of Fiorella vein from Ximena vein (Figs. 8 & 9). Included in this zone are the occurences called “Santa Maria”, “Quebrada Totorayoc”, “Nandito” and “El Chato” to the east. It is defined by a strong phyllic alteration and quartz stringer zone over an area 800 m E-W by 450 m N-S. Alteration includes the destruction of mafic minerals and the formation of white phyllosilicates (dominantly muscovite) and rutile. The size and abundance of phyllosilicates suggests a hydrothermal origin (Chavez, 2010). The protolith appears to be the older deformed intrusive, and the interpreted mineralizing intrusion does not outcrop.

The area of the phyllic alteration displays strong leaching and production of goethite after pyrite; the amount of pyrite, pre-oxidation, is estimated around 3% to 5% of the rock volume. Due to the strong oxidation, the only surviving sulphides (pyrite > chalcopyrite) are those that have been encapsulated in quartz. Hematite, derived from chalcocite, was noted as disseminations and within quartz stringers, suggesting that there was moderate to strong leaching of copper minerals in the system. In Totorayoc creek, about 70 m vertically below, to the east, is found a quartz monzonite porphyry with quartz veinlets containing pyrite, chalcopyrite and molybdenite and enveloping halos of sericite/muscovite. Pyrite and chalcopyrite is also replaced by hematite. The supergene enrichment blanket (chalcocite) is not expected to be highly developed by the evidence of covellite > chalcocite replacing pyrite and chalcopyrite. The presence of chalcocite-derived hematite on surface is another indication that the supergene blanket has been at least partially removed due to weathering.

Previously, Altynor's reconnaissance/gridded surface sampling yielded elevated concentrations of gold of up to 300 ppb and copper values of up to 500 ppm – 1000 ppm, and BISA obtained from their smaller grid values of Mo ranging from 50 ppm to 100 ppm and more restricted values of Cu ranging from 600 ppm to 900 ppm. They also obtained two low order anomalous Au results ranging 100 ppb to 200 ppb, neither of which correlated with the Cu/Mo anomalies. The anomalies did, however, lie within the


phyllic/silicic alteration zone.

Portal Resources, during their due diligence assessment of the property in 2008, collected 112 surface rock samples, but most were from the main areas of interest. These rock samples yielded an average of 1.58 g/t Au with a high of 30.7 g/t Au and a low of 0.003 g/t Au. Copper values showed an average of 0.15% Cu with a high of 5.03% Cu and a low near the detection limit (8 ppm).

The sampling done by the Issuer yielded values between 250 ppm and 800 Cu, and Mo values greater than 30 ppm. As mentioned previously, this geochemical anomaly is underlain by significant chargeability and magnetic “low” anomalies. A 3-D inversion model made by McInnes (2010) has yielded a “potential” solid of +/- 200 million tonnes, open to the east, west and at depth; the pole-dipole spacing used did not allow deeper penetration.

10.0 Exploration

Throughout much of 2010, the Issuer has performed detailed geological mapping (1:5,000 scale) of the main target area from Ximena vein in the west to the Santa Maria zone to the east, encompassing an area of about 3 km north-south by 3 km east-west. Fig. 8 is a simplified rendition of the detailed map they produced, which was viewed by the author. In addition, a 1:25,000 scale map of the entire property, a 1:1,000 scale map of the mesothermal Au-Cu area and a 1:500 scale section map of the Ximena-La Banda veins were completed. The geology has been digitized in Mapinfo GIS format.

Two programs of geochem sampling were also completed: a grid based lithogeochem survey over the Santa Maria zone and a follow-up sampling program of the various precious metal veins, from both surface and underground. A total of 465 rock samples and 13 soil samples were collected from the property. Of these rock samples, 400 were from the surface and 65 samples were taken underground from the various mines. In addition, the Issuer introduced 27 sample standards for quality control/quality assurance purposes.

The IP data from the 1998 Val D'Or survey was reprocessed, again using 3-D inversion modeling, and intrepreted by an independent consulting geophysicist based in Australia.

The underground mine workings that were developed by the informal miners between 2001 and 2003 were rehabilited; new stairways were placed, and wooden poles were place as supports and for access in the open stopes and raises.

Twenty-two short trenches were excavated along the surface projections of Ximena, Fiorella and La Banda Union veins with the intention of finding new zones covered by overburden.

10.1 Surface Sampling – Santa Maria Target

Samples were collected on a fairly systematic grid pattern at a nominal 50 m spacing along lines spaced 100 m apart, but terrain, access and cover dictated the actual locations. A total of 110 samples were collected. Rock chips were taken at each site over a 5 m distance at Santa Maria zone, and 5 m channel samples were collected along Totorayoc Creek. After channels were cut using a motorized diamond saw. Figs. 11 to 13 show the locations of the samples plus graphical representations of the values for Cu and Mo. An area roughly 800 m east-west by up to 600 m north-south was sampled.


3

50°

5° 8115

00

8120

00

8223000

8105

00

8110

00

8223500

LA BAND


LA

Totorayoc Fault

UNION VETAS

FIORELLA VEIN

Guanaco Fault

Zorro Andino Fault

A VEIN

Fault

73909

73899-73902

73903-73905

73910

73907

73908

73906

FIGURE:

ALTO QUEMADO PROJECT, PERUSANTA MARIA ZONESAMPLE LOCATIONS


PROJECTION: DATE:

SEE GRID PSAD56/18S MAY 15, 2011 11SCALE:

LEGEND

J. Nebocat Sample

Santa Maria Rock Samples

PGS Pacific G


50°

55°LA BANDA VEIN


LA LO

torayoc Fault

UNION VETAS

FIORELLA VEIN

Guanaco Fault

rro Andino Fault

A VEIN

Fault

8115

00

8120

00

8223000

8105

00

8110

00

8223500

PPM Cu

2,500

1,250250

FIGURE:

ALTO QUEMADO PROJECT, PERUSANTA MARIA ZONE

ROCK SAMPLES -- PPM CU


PROJECTION: DATE:


PGS Pacific G


3

50°

5° 8115

00

8120

00

8223000

8105

00

8110

00

8223500

LA BANDA VEIN


LA LO

torayoc Fault

UNION VETAS

FIORELLA VEIN

Guanaco Fault

orro Andino Fault

A VEIN

Fault

PPM Mo

80

408

FIGURE:


ROCK SAMPLES -- PPM MO


PROJECTION: DATE:


PGS Pacific G


Two of the samples taken from Quebrada (creek) Totorayoc were from high grade veins, yielding 1.44 g/t and 2.59 g/t Au; these were excluded from the statistical dataset pertaining to the porphyry Cu-Mo target area. Copper values range from 28 ppm to 8,590 ppm and averaged 467 ppm. Most of these came from deformed intrusive host rock, but some represent the younger granodiorite.

Molybdenum values range from detection limits (<1 ppm) up to 105 ppm and averaged 15 ppm. Most of the anomalous values coincide with the Cu anomalies, but the highest Mo results seem to be more concentrated about the central portion of the target area, whereas the anomalous Cu values extend a bit further out. The highest Mo results are found within a NW-SE by SW-NE oval shaped zone roughly 400 m by 300 m.

Gold values averaged 11 ppb (mg/t) and ranged from detection levels to 101 ppb (0.101 ppm, or 0.101 g/t).

Values for Ag, As, Bi, Pb, Sb and Zn are generally low or below their detection limits.

10.2 IP Survey Interpretation

The 1998 Val D'Or geophysical survey data was reprocessed using 3-D inversion modelling and reinterpreted by David McInnes, an independent geophysicist based in Australia. A complete set of depth slice images for the chargeability, resistivity and magnetic models is presented in Appendix III.

Figs. 14 & 15 are a representative set of the chargeability and resistivity anomalies at -115 m depth. What is clearly evident here, and at all depth slices, is the very strong correlation between high chargeability and low resistivity anomalies within the target area. The chargeability anomaly at this level is about 1,100 m long east-west by 500 m wide north-south, and the resistivity anomaly has similar dimensions.

Also of interest is a smaller chargeability anomaly about 200 m WSW of the main zone. Located under the Fiorella vein and at waypoint 131, it is suggested by the Issuer's geologists that this might be a faulted offset of the Santa Maria zone. There exists a NW-SE trending gully between them, interpreted to be a large fault zone, and the pattern made by the geophysical surveys supports this hypothesis.

The magnetic data shows generally low values centered over the main Santa Maria IP anomaly but with a sharp boundary along the SW side separating it from a body with a stronger magnetic signature. The low magnetic response over the porphyry target might reflect the destruction of magnetite caused by hydrothermal alteration from a mineralized porphyry system at depth (Fig. 16).

The body with the stronger magnetic signature to the south and southwest does not appear to be related to the granodiorite as the outline of the magnetic body in no way simulates the mapped outline of the intrusion. In addition, there appears to be a more linear, or tabular feature with a stronger magnetic response that trends NE-SW directly under the Fiorella and Ximena veins in the direction of Santa Maria. The smaller, isolated chargeability anomaly that sits between the veins coincides with the central part of this magnetic feature.


3

50°

5° 8115

00

8120

00

8223000

8105

00

8110

00

8223500

73899-73902

73903-73905

7390673907

73908

73909

73910

FIGURE:


CHARGEABILITY - 115 M DEPTH SLICE


PROJECTION: DATE:SCALE:

LEGENDSanta Maria Rock Samples

J. Nebocat Samples

SEE GRID PSAD56/18S MAY 15. 2011 14

PGS Pacific G


3

50°

5° 8115

00

8120

00

8223000

8105

00

8110

00

8223500

73899-73902

73903-73905

73906

73907

73908

73909

73910

FIGURE:


RESISTIVITY - 115 M DEPTH SLICE




J. Nebocat Samples


PGS Pacific G


3

50°

5° 8115

00

8120

00

8223000

8105

00

8110

00

8223500

73899-73902

73903-73905

7390673907

73908

73909

73910

FIGURE:


MAGNETICS - TMIsm RTE H




J. Nebocat Samples


PGS Pacific G


10.3 Surface Sampling: Veins and Reconnaissance

A total of 333 rock samples were taken by Mawson over a wide area of the property, but the bulk of these (264) came from the surface exposures of the precious metal-bearing veins.

Without discriminating these samples according to lithological type, etc., the global statistics of samples collected from the veins yield a range of values from detection limit (<0.05 ppm Au) to 32.6 ppm (g/t) Au, averaging 1.2 ppm (g/t) Au. Similarly, copper values ranged from detection limits to 140,050 ppm Cu (14.05%) with an average of 3,600 ppm (0.36%) Cu. Figs. 17 to 19 show the locations and symbolic plots for these results. Sample widths of the veins ranged up to 2 m but averaged around 0.7 m to 0.8 m.

The samples collected by Mawson confirm the ranges and orders of magnitude of results obtained by Altynor and BISA.

10.4 Underground Sampling – Ximena Vein

The Ximena vein has undergone the most development and exploitation by the informale miners on the property. It is sub-divided into four distinct vein zones, namely Ximena 1, Ximena 2-3 and Ximena 4. The Issuer has resampled sections of Ximena 1 and Ximena 2-3; the Ximena 4 section was in the process of being resampled during the author's visit.

The Issuer took a total of 46 samples from the Ximena vein system; 9 were taken by the informal miners and 37 were collected under the supervision of Mawson's geologists. Samples were taken from the backs (roof) or the floor if necessary, to crosscut the main structure. In some occasions the width of the working is less than the entire width of the vein and/or the wall rocks. Without taking any of these factors into consideration, the global average of these samples is 27.70 g/t Au, with a maximum of 695 g/t Au and a minimum of 0.13 g/t Au. Copper values were also high, averaging 4.23% Cu, with a maximum of 23.60% Cu and a minumum of 0.01% Cu. The highest Cu values are attributed to the supergene enrichment zone where chalcopyrite is replaced by chalcocite and covellite.

Silver values are slightly anomalous compared with the surface results, averaging 8.45 g/t Ag with a maximum of 32 g/t Ag and a minimum below the detection limit (<0.2 g/t Ag).

Other potential indicator/accessory elements, such as As, Mo, Pb and Sb returned very low values.Tables 2 & 3 list the pertinent results from these areas, and Figs. 20 to 22 show their locations.

The Issuer sampled up to 30 m depth along the Ximena vein within these zones. Their samples appear to be either in the oxide or mixed oxide/sulphide zones of the veins. As was suggested by Altynor, there does seem to be a leaching of gold from surface and a corresponding enrichment at depth. Copper values show a definitely depletion at surface, but how much of the copper at depth is due to enrichment or just primary sulphide content is not certain.

The Issuer has determined that the weighted average of the underground samples averages 9.31 g/t Au and 4.22% Cu across 0.91 m width along a 500 m strike length.



35°

40°

50°

55°

40°

2,900

3,000

3,100

3,200

3,300

3,400

3,500

3,200

3,30

0

LA BANDA VEIN


LA LOMADA VEIN

Totorayoc Fault

UNION VETAS

FIORELLA VEIN

Guanaco Fault

Zorro Andino Fault

XIMENA VEINToro Bravo Fault Venado Fault

Viscacha Fault

8120

00

8140

00

8160

00

8226000

8224000

8222000

8100

00

8060

00

8080

00




YURA GROUP

Road

Claim perimeter


45°45°45°45°45°45°45°45°45°

Veins

Faults





Deformed Intrusive


FIGURE:

ALTO QUEMADO PROJECT, PERUREGIONAL SAMPLING BY COMPANY


PROJECTION: DATE:


SCALE:

MAWSON Samples

RBB Samples

ALTYNOR Samples

"UNKNOWN" Samples

BISA Samples



35°

40°

50°

55°

40°

2,900

3,000

3,100

3,200

3,300

3,400

3,500

3,200

3,30

0

LA BANDA VEIN


LA LOMADA VEIN

Totorayoc Fault

UNION VETAS

FIORELLA VEIN

Guanaco Fault

Zorro Andino Fault


Viscacha Fault

8120

00

8140

00

8160

00

8226000

8224000

8222000

8100

00

8060

00

8080

00




YURA GROUP

Road

Claim perimeter


45°45°45°45°45°45°45°45°45°

Veins

Faults





Deformed Intrusive


FIGURE:

ALTO QUEMADO PROJECT, PERUREGIONAL SAMPLING--GOLD


PROJECTION: DATE:


SCALE:

MAWSON SAMPLES - PPM AU

3015

3

MAWSON Samples

RBB Samples

ALTYNOR Samples

"UNKNOWN" Samples

BISA Samples



35°

40°

50°

55°

40°

2,900

3,000

3,100

3,200

3,300

3,400

3,500

3,200

3,30

0

LA BANDA VEIN


LA LOMADA VEIN

Totorayoc Fault

UNION VETAS

FIORELLA VEIN

Guanaco Fault

Zorro Andino Fault


Viscacha Fault

8120

00

8140

00

8160

00

8226000

8224000

8222000

8100

00

8060

00

8080

00




YURA GROUP

Road

Claim perimeter


45°45°45°45°45°45°45°45°45°

Veins

Faults





Deformed Intrusive


FIGURE:

ALTO QUEMADO PROJECT, PERUREGIONAL SAMPLING--COPPER


PROJECTION: DATE:


SCALE:

MAWSON SAMPLES-- PPM CU

20,00010,000

2,000

MAWSON Samples

RBB Samples

ALTYNOR Samples

"UNKNOWN" Samples

BISA Samples


Table 2. Ximena Vein Surface Samples, Mawson Resources

WIDTH (m) Au_g/t Cu_% Au x m Cu x m Au_Equiv x m Zona

217803-10 6.30 0.41 0.10 0.59 2.58 2.58 0.63 3.73 XIM 1 SUPERFICIE217813-21 6.05 0.75 0.23 1.17 4.54 4.54 1.39 7.07 XIM 2-3 SUPERFICIE217954-60 6.65 0.48 0.50 1.39 3.19 3.19 3.32 9.24 XIM 4 SUPERFICIE217860-61 1.70 0.21 0.01 0.23 0.36 0.36 0.02 0.39 XIMENA SUPERFICIE218255-56 1.50 2.85 1.03 4.72 4.28 4.28 1.54 7.08 XIMENA SUPERFICIE218246-47 1.80 1.29 0.07 1.42 2.32 2.32 0.13 2.55 XIMENA SUPERFICIE217801 1.10 0.76 0.02 0.80 0.83 0.83 0.03 0.88 XIMENA SUPERFICIE218299 0.55 1.33 0.09 1.49 0.73 0.73 0.05 0.82 XIMENA SUPERFICIE218257-59 3.40 0.84 0.12 1.06 2.86 2.86 0.41 3.60 XIMENA SUPERFICIE218253-54 1.30 1.82 0.31 2.38 2.37 2.37 0.40 3.10 XIMENA SUPERFICIE217824 0.50 1.09 0.23 1.51 0.54 0.54 0.12 0.75 XIMENA SUPERFICIE217858-59 0.75 0.31 0.70 1.58 0.23 0.23 0.52 1.19 XIMENA SUPERFICIE217962-63 1.10 0.19 0.01 0.21 0.21 0.21 0.01 0.23 XIMENA SUPERFICIE

2.52 0.77 0.26 1.24 25.04 8.57 40.62

SAMPLES NUMBERS

Au EQUIV

ANCHO POR LEY DE Au

MUESTRA TOMADA EN:

Translations:

• Ancho Por Ley de Au = width times grade Au• Muestra Tomada en = sample taken at...• Zona = zone

Table 3. Ximena Vein Underground Samples, Mawson Resources


218301 0.60 13.90 0.16 14.20 8.34 8.34 0.10 8.52 XIM 1 UNDERGROUND218302 0.30 12.25 2.77 17.29 3.68 3.68 0.83 5.19 XIM 1 UNDERGROUND218303 0.20 1.41 6.06 12.43 0.28 0.28 1.21 2.49 XIM 1 UNDERGROUND218304 0.40 0.59 4.84 9.39 0.24 0.24 1.94 3.76 XIM 1 UNDERGROUND218305 0.35 34.10 0.58 35.16 11.94 11.94 0.20 12.31 XIM 1 UNDERGROUND218306 0.20 30.50 0.36 31.16 6.10 6.10 0.07 6.23 XIM 1 UNDERGROUND218307 1.00 2.27 2.67 7.12 2.27 2.27 2.67 7.12 XIM 2-3 UNDERGROUND218308-09 1.15 6.19 4.82 14.95 7.12 7.12 5.54 17.20 XIM 2-3 UNDERGROUND218310-11 1.30 9.55 5.78 20.06 12.42 12.42 7.51 26.08 XIM 2-3 UNDERGROUND218312 0.80 9.90 7.44 23.43 7.92 7.92 5.95 18.74 XIM 2-3 UNDERGROUND218314-18 2.83 5.95 9.93 24.00 16.84 16.84 28.10 67.93 XIM 2-3 UNDERGROUND218319-21 1.90 7.80 9.79 25.60 14.82 14.82 18.60 48.64 XIM 2-3 UNDERGROUND218322 0.70 4.57 6.36 16.13 3.20 3.20 4.45 11.29 XIM 2-3 UNDERGROUND218323 0.90 2.78 4.71 11.34 2.50 2.50 4.24 10.21 XIM 2-3 UNDERGROUND218324 1.00 1.09 4.24 8.80 1.09 1.09 4.24 8.80 XIM 2-3 UNDERGROUND218325 0.75 7.44 6.43 19.13 5.58 5.58 4.82 14.35 XIM 2-3 UNDERGROUND218326-27 1.20 5.89 0.26 6.36 7.07 7.07 0.31 7.64 XIM 4 UNDERGROUND218328 0.25 144.00 0.03 144.05 36.00 36.00 0.01 36.01 XIM 4 UNDERGROUND218329-30 1.20 6.32 0.32 6.90 7.58 7.58 0.38 8.28 XIM 4 UNDERGROUND218331-32 1.30 15.99 0.13 16.23 20.79 20.79 0.17 21.09 XIM 4 UNDERGROUND218333-34 1.40 9.40 0.11 9.60 13.16 13.16 0.15 13.44 XIM 4 UNDERGROUND218335 0.45 12.40 0.33 13.00 5.58 5.58 0.15 5.85 XIM 4 UNDERGROUND218336-37 1.10 7.36 0.37 8.03 8.10 8.10 0.41 8.84 XIM 4 UNDERGROUND218338 0.60 1.78 0.30 2.32 1.07 1.07 0.18 1.39 XIM 4 UNDERGROUND

0.91 9.31 4.22 16.97 203.66 92.25 371.39

SAMPLES NUMBERS

Au EQUIV

ANCHO POR LEY DE Au

MUESTRA TOMADA EN:


217806

217806217803

217804217807

217808

217809

217810

217811

218305

218306

218301

218301

218302

218304

218303

XIMENA 1

10 m

Mawson Resources sample site



XIMENA 1 VEIN


SEE BAR N.A. MAY 15, 2011 20


10m.

218307

218323

218322

218324

218312

218308

218309

218310-11

218314-18

218319-21

217815 217817

217815

217814217816

217817

217818

217819

217821

217813



XIMENA 2-3 VEIN


SEE BAR N.A. MAY 15, 2011 21

10 m

218301

Mawson Resources sample site

Nebocat sample site


XIMENA 3

XIMENA 273903-73905

73903-73905

3100 m

810,3

50

E

810,3

00

E

810,2

50

E

8,223,150 N

8,223,100 N



XIMENA 4 VEIN


SEE BAR N.A. MAY 15, 2011 22

218335

73899

86515

Mawson sample site

BISA sample site

Nebocat sample site


86501-03

86509-11 86512-1386514

86515 86516

86517-19?

86504-06 86507-08

73899-90073901-02

218326-27

218328 218329-30218331-32

218335

218336-37

218338

218333-34

10.5 La Banda Vein

A total of 19 samples were collected from La Banda vein workings; all samples were taken under the supervision of the Issuer's geologists. Here, again, the values underground are significantly higher than at surface. Gold values have a global average of 25.30 g/t Au with a maximum of 267 g/t Au and a minimum of 0.07 g/t Au. Copper averaged 2.42% Cu with a maximum of 8.02% Cu and minimum of 0.18% Cu. Silver, like at Ximena vein, is much more anomalous at depth, averaging 7.3 g/t Ag with a high of 41.7 g/t Ag. Mo is slightly higher than at Ximena (up to 78 ppm), but the other indicator/accessory elements are also low or near detection limits.

Tables 4 & 5 and Fig. 23 show the results and locations of these samples, respectively.

Mawson's geological team calculated the average grade and width of the underground samples at La Banda to be 15.09 g/t Au and 1.53% Cu over 1.08 m along a strike length of 120 m.

Table 4. La Banda Vein Surface Samples, Mawson Resources


217890-96 5.40 2.09 1.60 5.00 11.29 11.29 8.64 27.00 LA BANDA SUPERFICIE218272 0.50 0.40 0.16 0.69 0.20 0.20 0.08 0.35 LA BANDA SUPERFICIE218276 1.55 0.44 0.10 0.62 0.68 0.68 0.16 0.96 LA BANDA SUPERFICIE218282-83 3.00 0.03 0.01 0.05 0.09 0.09 0.03 0.14 LA BANDA SUPERFICIE217994 0.60 0.07 0.45 0.89 0.04 0.04 0.27 0.53 LA BANDA SUPERFICIE218266 0.90 0.17 0.23 0.59 0.15 0.15 0.21 0.53 LA BANDA SUPERFICIE

1.99 1.04 0.79 2.47 12.45 9.38 29.51

SAMPLES NUMBERS

Au EQUIV

ANCHO POR LEY DE Au

MUESTRA TOMADA EN:

Table 5. La Banda Vein Underground Samples, Mawson Resources


218339-40 1.20 16.52 3.50 22.88 19.82 19.82 4.20 27.46 LA BANDA UNDERGROUND218341-42 0.85 85.16 0.72 86.47 72.39 72.39 0.61 73.50 LA BANDA UNDERGROUND218343 0.60 44.80 0.60 45.89 26.88 26.88 0.36 27.53 LA BANDA UNDERGROUND218345-46 2.10 1.86 0.56 2.88 3.91 3.91 1.18 6.04 LA BANDA UNDERGROUND218347-48 0.90 1.56 0.92 3.23 1.40 1.40 0.83 2.91 LA BANDA UNDERGROUND218349 1.00 8.76 3.26 14.69 8.76 8.76 3.26 14.69 LA BANDA UNDERGROUND218350-51 1.50 5.34 0.96 7.09 8.01 8.01 1.44 10.63 LA BANDA UNDERGROUND218352-53 0.70 3.43 2.29 7.59 2.40 2.40 1.60 5.32 LA BANDA UNDERGROUND218354-55 0.90 3.95 1.63 6.91 3.56 3.56 1.47 6.22 LA BANDA UNDERGROUND

1.08 15.09 1.53 17.88 147.13 14.95 174.30

SAMPLES NUMBERS

Au EQUIV

ANCHO POR LEY DE Au

MUESTRA TOMADA EN:

Table 6. Projected Conceptual Target: Ximena and La Banda Veins, Mawson Resources

VEIN THICKNESS STRIKE DEPTH SG TONNES Au (g/t) Cu (%) Au Equiv Au onz Cu tonnes Au EQUIV onzXIMENA 0.91 500 200 2.8 254,800 9.31 4.22 16.97 76,268 10,753 139,018LA BANDA 1.08 120 200 2.8 72,576 15.09 1.53 17.88 35,211 1,110 41,721

327,376 111,478 11,863 180,739

Table 6 is a summary of the average grades, widths and projected lengths and depths of Ximena and La Banda veins as calculated and estimated by the Issuer. The author is of the opinion that these figures represent a realistic exploration target that could average from 10 g/t to 15 g/t Au and 1.5% to 4% Cu


A

B

C

D

C'

C"

3040 m

3020 m

3060 m

3080 m

8,222,450 N

811,8

00

E

811,8

50

E

8,222,400 N

811,9

00

E

29 30

31

32

33

34

35

218335

Mawson sample site


75°70°

73°

75°

218354-55

218352-53

218350-51

218349218347-48

218345-46

218343

218341-42

218339-40

218263

218261

218260218274

218273

218272

218271

217890

217891217893

217896

217898217897

217895

217892

217894

217890

217895

218261

218272



LA BANDA VEIN


SEE GRID N.A. MAY 15, 2011 23

over an average thickness of 1 m. This would equate to a minimum of 300,000 tonnes at the average grade cited above, or an in-situ potential of 200,000 gold-equivalent ounces. This estimated tonnage could likely be doubled to 600,000 tonnes, or an in-situ gold-equivalent potential resource of 400,000 ounces.

The potential quantity and grade estimates presented herein are conceptual in nature, there has been insufficient exploration to define a “Mineral Resource” as defined in NI 43-101, and it is uncertain if further exploration will result in the target being delineated as a Mineral Resource.

All work done on the property as described in this section of the report was conducted by the Issuer and/or the Issuer's employees.

11.0 Drilling

There has been no drilling performed on this property by the Issuer, as yet, and there is no record or evidence of any other party having drilled it previously. This is a relatively new discovery in Peru, being found within the last 10 years.

12.0 Sampling Method and Approach

The sampling methodology used by AQMC was not known to Altynor, nor is there any record of it available to the Issuer or the author of this report. Likewise, BISA did not provide details regarding sampling other than mentioning the widths of their samples. Altynor provided comprehensive details of their methodology:

“....During the reconnaissance survey completed by Altynor in 2007, the following sampling methods were used: (a) continuous chip/channel – 91 samples; (b) short chip – 3 samples; (c) grab – 19 samples; (d) bulk sampling of mined ore- 4 samples; and (e) metallurgical – 3 samples. As the most common method we used continuous chip/channel sampling (3 cm deep x 5 cm wide channel) perpendicular to the vein strike. The length of individual sample intervals depended on the thickness of veins, but did not exceed 1.0 m with the weight of sample between 2 and 3 kg. If the access permitted so, we also took samples from wall rock, except for some areas underground, where the width of vein exceeded the width of drifts.

From the total of 91 continuous chip samples, 36 were taken from underground workings and 55 from surface outcrops. At surface, if possible, we have taken channel samples over the whole width of mineralization including veins and wall rock. In such case, the full length of the sample interval was at Ximena 5 m (145687-145692); at La Banda 4.5 m (145633-145637) and at Fiorella 4 m (145640-145646).

A limited amount of 6 samples from the deepest parts of Ximena 3 and Fiorella (145604-145607; 145616-145617) were collected by the supervisor of RBB [AQMC] with assistance of artisanal miners without the presence of Altynor due to safety conditions at the mine. Grab samples were used in cases where veins were outcropping only partially or veins were disintegrated at surface. Typically, the weight of grab samples was 2-2.5 kg.

Bulks samples were taken from ore which was stored and dried at surface prior transportation to the plant. Before shipping; the ore was spread at the area of around 20 m sq. We selected a section of 1.5 m x


1.5 m which was divided into 25 squares (30 cmx30 cm). From each square we took a small sample of 100-150 g of ore. The total of 25 such small samples amounted to one bulk sample of 2.5-3.5 kg.

Short chip samples were used when the thickness of veins was not more than 10 cm- 20 cm. In such cases, sampling was done along the strike of the vein with 1.0 m interval providing for the weight of 2.5 kg. This method was used rarely and only 3 samples were collected. Finally, while doing reconnaissance survey, we conducted a screening of pan concentrate from duplicates of some chip and grab samples. This work was done in field and helped us to understand better the mineralogy and identify the content of free gold.For metallurgical testing, we took 3 samples from Ximena representing 3 types of ore with the weight of 5 kg each. Sample No. 145518 was oxide ore from Ximena 4; sample No. 145519 was quartz-sulfide (pyrite_chalcopyrite) ore from Ximena 3 and No. 145520 was quartz-chalcocite-chalcopyrite ore from the zone of secondary enrichment at Ximena 3...”

The Issuer took a combination of chip, channel and grab samples during their regional sampling program, but the bulk of these were channel samples. The channels ranged up to 2 m in width.

Underground samples were channel samples across the width of the veins and adjacent wallrock, where present. Sampling was done with a hammer and chisel with a tarpaulin used to collect the samples; the samples were placed into plastic bags and sealed.

The surficial veins would have been sampled by the same methodology, except a tarpaulin would not have been used.

For the gridded rock sampling survey of the Santa Maria zone, random rock chips were collected at each station from about a 5 m diameter, but individual sample widths ranged from 1.1 to 6.0 m. As mentioned previously in the Exploration section of this report, a total of 93 sample were taken from the Santa Maria area.

Of the 333 surface samples taken outside of Santa Maria zone, 55 came from the Fiorella vein, 62 from the La Banda vein, 23 from the Union veta zone, 48 from La Lomada vein, 104 from Ximena vein and 31 were regional samples taken from various parts of the property. The regional surface samples were spaced up to 8.7 km apart east-west by 2.8 km north-south, but the bulk of them were from the central target areas of the property, a distance rough 2.8 km east-west by 1.6 km north-south, or encompassing an area roughly 430 hectares.

No drilling has yet been done on the property; hence, there are no factors that need to be considered regarding sample recoveries, etc. that would affect drill results.

Sampling of the veins was done perpendicular to their strike both underground and on surface. Certain surface vein samples, where the ground was either badly broken or poorly exposed, would not necessarily be representative of the true thickness of the vein(s). The samples taken from the porphyry target were either linear, as channels or contiguous chips, or taken as random grabs within a certain radius about a survey station. As a porphyry generally has an isotropic rhombohedral to irregular stockwork pattern within the pyritic halo, sampling directions should not play a significant factor in biasing the results.

Lithologic types and descriptions were provided in the History, Geology and Exploration sections of this report. In summary, the Santa Maria zone is hosted mainly by metamorphosed felsic to intermediate intrusives that have been overprinted by an apparent porphyry copper-molybdenum bearing intrusive at


depth which has imparted phyllic and silicic alteration on these rocks and have been subsequently argillized.

The quartz-sulphide veins are hosted along major fault structures that cut these same host rocks west and south of the Santa Maria porphyry zone. Within the Ximena vein there occur some fairly massive sulphides alongside the quartz. At Ximena 2-3, the author observed semi-massive chalcopyrite-pyrite in the footwall side of the quartz vein and lesser disseminated sulphides in the hanging wall portion. Much of the wallrock was sheared and altered to clay, chlorite and locally talc? The sulphide-rich zones contain significantly higher concentrations of gold than the quartz-dominant zones, nonetheless, the quartz veins also contain gold values running to several g/t.

Table 3, above, shows a composite of five samples taken by the Issuer from the Ximena 2-3 vein (218314-218318) that averaged 9.50 g/t Au and just over 14% Cu over 1.70 m in first three of the samples from the footwall side. The footwall sample is dominantly sulphide, it returned 17.35 g/t Au and 23.60% Cu over 0.5 m. The author replicated these five samples with three check samples which are discussed in the Data Verification section, following.

Aside from a few other sites along these veins, there exist no drillholes or trenches over which numerous contiguous samples were taken.

13.0 Sample Preparation, Analyses and Security

BISA used two laboratories for the samples they collected in 2003:

1. CIMM PERU SA analyzed all their samples (132) for Au and ICP for 34 elements.

2. SGS de Peru SAC analyzed the duplicate samples (12).

They performed some basic statistics, comparing the suite of duplicate samples, and found the results satisfactory.

The samples taken by Altynor were bagged and labeled on site then transported to the laboratory. Assaying was conducted at the SGS laboratory in Lima, a well known independent commercial laboratory using certified and approved methodology (http://www.sgs.com//sitemap.htm).

The samples were processed according to the metal sought. Gold was extracted via fire assay Au_FAA515, and in case of high grade, double-checked with Au_FAG505. Copper and silver were assayed by atomic absorption (Ag_AA12CP; Cu_AA12CP).

Duplicates and standards were not used at this stage.

All samples taken by the Issuer were collected by its employees. No drilling or other form of large scale sampling campaign was performed, thus no sample splitting or preparation was performed on site. All samples were sealed and shipped directly to the ALS Chemex (“ALS”) laboratory in Arequipa, Peru, for sample preparation. Pulps from these samples were shipped to the ALS laboratory in Callao, Lima, Peru or to the ALS laboratory in Vancouver for analyses.

On average, the Issuer introduced one standard and one blank with every sequence of 20 samples, inclusive.


http://www.sgs.com//sitemap.htm

Analytical packages used by ALS Chemex included: ME-ICP61, ME-ICP41, AU-AA23, AU-SCR24, AU-26D, AU-GRA22, AU-GRA21, CU-AA46 and CU-AA62. A brief description of ALS Chemex's analytical procedures is provided on their assay certificates:

◦ AU-GRA21 - Au 30 g, fire assay, gravimetric finish

◦ AU-GRA22 - Au 50 g, fire assay, gravimetric finish

◦ AU-AA26 - ore grade Au, 50 g, fire assay, atomic absorption finish

◦ CU-AA46 - ore grade Cu, aqua regia digestion, atomic absorption finish

◦ CU-AA62 - ore grade Cu, four acid digestion, atomic absorption finish

◦ ME-1CP41 - 35 element ICP – AES, aqua regia digestion

◦ ME-ICP61a - 35 element ICP – AES, high grade, four acid digestion

◦ AU-SCR24 - Au metallic screen, double minus 50 g, fire assay finish

◦ AU-AA26 - ore grade Au, 50 g, fire assay, atomic absorption finish

◦ “D” = duplicate

For a complete description of the analytical and preparation procedures, the reader is invited to view ALS's website: http://www.alsglobal.com

ALS is an ISO 9001:2000 accredited laboratory, and a number of analytical facilities have received ISO 17025 accreditations for specific laboratory procedures. As part of their ISO 17025 accreditation, ALS Laboratories participate in a number of international proficiency tests, such as those managed by CANMET and Geostats. Both of these agencies circulate samples for analysis twice a year and evaluate the performance of participating laboratories.

The Issuer introduced 3 different standards, representing multi-element ICP, anomalous Au-Cu-Mo-S, high grade Cu-Au and high grade Au-Ag and one blank sample. ALS ran a duplicate check on approximately every 8th sample and introduced up to 10 different standards and 2 blanks. The frequency of their internal standard/blank usage is not stated as the results of these determinations are shown on a separate spreadsheet layer from the Issuer's sample results. For example, however, in a suite of 101 samples, which includes 4 of the Issuer's standards and 3 blanks, ALS shows 18 internal standard and 15 internal blank determinations.

The sample collection, preparation, transportation (security) and analytical techniques used appear to be satisfactory.

For this limited suite of samples, the author's samples were also sent to the ALS Chemex preparation lab in Arequipa and analyzed in Lima. The samples were determined using ME-ICP41, Au-AA23 and Au-GRA21 packages. The lab performed 18 standard tests using 5 different standards and 14 blank determinations using 4 different blanks. No external standards or blanks were introduced to this suite of samples.


http://www.alsglobal.com/

14.0 Data Verification

The author has reviewed all the documents, plans and sections prepared by BISA and Altynor that the Issuer had available. The work done by the Issuer, including sampling and mapping, corroborates the findings made both by BISA and Altynor; however, there are some differences in opinion regarding the interpretation and origin of the “metamorphic” rocks. The Issuer had access to further research data made public by INGEMMET subsequent to Altynor's involvement in the project.

Two days were spent by the author examining surface geology, surface and underground workings and reviewing maps and sections prepared by the Issuer.

In addition, 13 check samples were collected: 7 from underground along the Ximena vein system, 4 from the Santa Maria porphyry target, 1 from the Union Veta showing, 1 from the Fiorella vein and 1 from La Lomada “stockwork” zone.

Table 7 shows a comparison between 5 contiguous samples taken by the Issuer from the Ximena 2-3 vein and 3 contiguous samples taken by the author over virtually the same interval. Fig. 21 shows the locations of both these sample suites.

Table 7. Comparison of J. Nebocat and Mawson Resources Samples, Ximena 2-3 Vein

Mawson Sample Width (m) g/t Au W X Au Nebocat Sample Width (m) g/t Au W X Au218314 0.5 17.35 8.675 73903 0.4 11.25 4.5218315 0.7 7.1 4.97 73904 1 3.16 3.16218316 0.5 5.02 2.51 73905 1.3 6.59 8.567218317 0.55 1.75 0.9625218318 0.6 0.13 0.078

2.85 6.03 2.7 6.01AVERAGE 2.12 2.23

As was described previously, the footwall sample is chalcopyrite and pyrite rich, followed by dominantly quartz vein and then disseminated sulphides in the hanging wall. There is an extremely good comparison between these two sets of samples, particularly since they are not exact width replications.

Two contiguous samples were taken from each of two sites in the Ximena 4 underground workings. Samples 73899 and 73901 were taken from the quartz vein which contains limonite and specular hematite, and samples 73900 and 73902 were taken from the respective footwall portions of the vein which are sheared and chloritic meta-intrusive rocks. Table 8 shows the results of the samples taken from Ximena 4 vein area, comparing samples taken by the author with those taken by BISA; the Issuer had not resampled Ximena 4 vein at the time of the author's visit.

Table 8. Comparison of BISA Samples with J. Nebocat Samples, Ximena 4 Vein

BISA Sample Width (m) g/t Au Location** Nebocat Sample Width (m) g/t Au W X Au86512 0.5 8.7 ceiling 73899 0.5 1.995 0.997586513 0.35 6.4 floor 73900 0.65 0.171 0.11115

AVERAGE 1.15 0.96 1.10865

86514? * 0.5 5.8 center 73901* 0.65 14.6 9.4973902* 0.7 0.319 0.2233

AVERAGE 1.35 7.20 9.7133


* the location of samples 73901 and 73902 are approximately in the area of BISA sample 86514.

** BISA's descriptions of the samples (translated) are “ceiling”, “floor” and “center”. “Ceiling” is the hanging wallside and “floor” is the footwall side of the vein.

The Au values from BISA's samples 86512 & 85513 are somewhat higher than the author's sample 73899which was taken from the principal vein. Sample 73899 was taken in the vicinity of sample 88512 and isnot a direct repetition of it, unlike the samples taken from Ximena 2-3. What is clear that samples takenfrom within the vein tend to return values of Au in the X to XX g/t

Sample 73906 was taken from a hand-dug trench from the top of the hill near the centre of the SantaMaria zone. An 8-metre chip sample ran 566 ppm Cu and 0.01 ppm Au. The rock is a strongly phyllic andargillic altered meta-intrusive of apparent felsic origin.

Samples 73907 & 73908 were taken from altered and pyritic intrusive along the creek that roughly bisectsSanta Maria zone, running from north to south. They ran 349 and 558 ppm Cu and 6 ppm and 72 ppm Moover 2 m and 4 m, respectively.

At Vetas Union zone, sample 73909 returned 76 ppm Cu and 44 ppm Mo across 2.5 m. Altynor hadinterpreted this zone to be the junction of Ximena and Fiorella veins, but neither the author nor the Issuerbelieve this to be the case. There is a little evidence of quartz veining, and it appears to be large shearzone that has been weathered and oxidized; hematite and limonite are common in addition to argillicalteration. The shear zone trends 120/60 NE and might be a leakage, or distal phenomenon from thefaulted offset chargeability anomaly west of Santa Maria zone.

A grab sample (73910) was taken of oxidized quartz vein material from a dump on the Fiorella vein. Ityielded 6.34 g/t Au and 735 ppm Cu.

The zone at La Lomada was tested with one sample. A 20 m wide chip sample of highly weatheredgranodiorite ran 0.013 g/t Au and 30 ppm Cu. This sample was taken between two parallel veins systemsseparated by about 40 m. There is no evidence of any “stockwork” style of mineralization at La Lomadaas was suggested by Altynor.

The digital data, and hard copy data derived therefrom, appears to be original and authentic. Also, theobservations made by the author on site, and the results of samples taken by same, corroborate what hasbeen presented and observed in the field. The reader is cautioned that any digital data is subject tomodification by anyone who has access to it or the motivation to do so. However, as stated previously, theobservations made by, and samples collected by, the author support was is documented in digital andwritten form and what was observed on site.

15.0 Adjacent Properties

The Zafranal porphyry deposit, owned by AQM Copper Inc., through its wholly owned Peruviansubsiduary Minera AQM Copper Peru, SAC, and 50:50 joint venture partner Teck Resources, islocated about 15 km due west of Alto Quemado.

Zafranal is becoming a significant copper-gold porphyry deposit with mineralization identified over a2,800 m strike length, up to 600 m width and up to 500 m thickness, of which the supergene blanketis between 50 m - 150 m thick. The mineralization remains open to the southeast and northwest aswell as at depth in certain areas.


http://www.aqmcopper.com/s/Home.asp

AQM announced a NI 43-101 Compliant Resource Estimate on February 28, 2011. Measured andindicated resources are reported as 301 Mt at 0.48% Cu and 0.08 g/t Au, with an additional inferredresource of 51 Mt at 0.32% Cu and 0.06 g/t Au. http://www.aqmcopper.com/s/Home.asp

Recent interpretations suggest that the porphyry was emplaced as a lenticular body within an east-west trending tectono-morphic fault that splays off the Incapuquio-Cincha-Lluta fault system. TheZafranal porphyry system is located within a “jog” of this east-west transpressive fault splay, andfaults internal to the porphyry, which trend about 1350AZ, indicate a dextral movement along thismajor structure. It has been suggested by the Issuer that the Santa Maria zone porphyry target mayhave been similarly emplaced along this same east-west structural corridor that has imparted themetamormorphic fabric on the igneous rocks at Alto Quemado.

The author has not been able to verify the claims made on AQM's website. The reader is advised thatany descriptions of geology, mineralization, resources and/or reserves on the Zafranal property haveno direct correlation with any geology, mineralization, resources and/or reserves found, or yet to befound, on the Alto Quemado property.

16.0 Mineral Processing and Metallurgical Testing

The Issuer has performed no metallurgical test work on material from the Alto Quemado project.

Altynor, previously, submitted two samples from the 80 m depth level of the Ximena 3 vein, belowthe oxide zone. These two samples assayed 97.4 g/t Au, 15.2% Cu and 98.8 g/t Au, 13.9% Cu.

The testing was done by SGS Mineral Services and included:

a) Gravity Concentration of sample in Knelson

b) Flotation rougher of the tailings from Knelson

c) Cyanidation of the flotation tailings

SGS concluded the following:

• Gravity concentration for two samples recovered 35.3% and 41% of gold, which indicates that it isnot a very favorable method for gold recovery, although the enrichment of its head grades in theconcentrate could justify it.

• Flotation process should be centered exclusively on the recovery of the high copper content intailings from the gravitational concentrate to reduce cyanide consumption in the cyanidation process.For this reason it is recommended to study the effect of grinding on the rougher flotation and thedefinition of the formula and most suitable does of reagents.

• Copper recovery is closely related to the recovery of silver, indicating that it could be possible toobtain a high grade copper concentrate with an important content of silver.

• Flotation does not have a major effect on the recovery and grade of gold.

• Cyanidation is the more suitable process for the gold recovery of this type of ore, obtainingrecoveries of 91.7% and 93.6% of gold contained in the flotation tailings; however cyanide


consumption in tests was too high due to high concentrations of copper; more testing is required toimprove the flow sheet.

Altynor’s consulting metallurgist made the following observations and recommendations:

• Recovery of gold by gravity concentration 35.3% and 41%; by flotation 39% and50% andcyanidation 91.7% and 93.6%, indicates an overall recovery of 95.18% and 96.16%.

• Increased consumption of cyanide is probably due to high content of chalcosite.

• Recovery of silver by gravity 26.7% and 25.4%; flotation 55.9% and 64.3%, cyanidation 39%and 36%, indicates an overall recovery of 68.86% and 67%.

• Recovery of copper by gravity 10.1% and 9.6%; flotation 65.5% and 72.6%, cyanidation 16%and 30%, indicates an overall recovery of 58.55% and 69.16%

• Overall recoveries of all metals are encouraging, however more systematic analytical work isrequired to improve our confidence and to arrive at the best possible flow sheet.

• It is recommended to collect representative samples of all 3 types of ore (oxide, mixed enrichedoxide/sulphide ore and primary sulphide ore) and to then conduct a comprehensive analysis oftheir properties.

Altynor further stated they did not receive the assays of these two samples prior to submission toSGS for testing. Since they yielded very high grades in Au and Cu, they were not considered to berepresentative of the entire vein system, but they decided to go ahead with the tests just the same.

17.0 Mineral Resource and Mineral Reserve Estimates

At this time, there exist no known mineral resources or reserves on the Alto Quemado property.

18.0 Interpretation and Conclusions

The Alto Quemado property is located within a prism, “pull-apart” structure, in the form of Reidelshears located at the confluence of two important metallogenic structural systems: the Cincha-Lluta/Incapuquio (NW-SE) and Clavelinas-Iquipi (E-W) faults.

On the property there exist two types of mineralization: mesothermal, high grade Au-Cu veins, andthe expression of a near-surface, buried porphyry Cu-Mo+/-(Au) deposit.

The veins were first discovered about 10 years ago and have been exploited by artisanal (informal)miners since that time. Both targets have not been drilled.

The veins exhibit signs of surface leaching; sub-surface grades in both Au and Cu increasesignificantly when compared with the surficial assay results.

The Issuer has estimated a global, in-situ potential target resource of 327,376 tonnes containing180,739 gold-equivalent ounces of Au in the Ximena and La Banda veins. The author suggests thatthis is a reasonable conceptual target that could average from 10 g/t to 15 g/t Au and from 1.5% to 4%Cu over an average thickness of 1 m. This would equate to a minimum of 300,000 tonnes at the averagegrade cited above, or an in-situ potential of 200,000 gold-equivalent ounces. This estimated tonnage


could likely be doubled to 600,000 tonnes, or an in-situ gold-equivalent potential resource of 400,000ounces.

The porphyry target has a strong phyllic alteration halo over an area about 800 m E-W by 450 m N-S. Chalcocite-derived hematite indicates secondary leaching of supergene mineralization, andsurficial rocks samples yield anomalous values in Cu between 250 ppm and 800 ppm. This areacoincides with a high chargeability IP and a magnetic low anomaly.

The host rock is a highly deformed intrusive, resembling and previously incorrectly described as ametamorphic rock. The cataclastic and mylonitic textures are the result of dynamic metamorphism,the cause of which is not yet fully understood. The government survey had previously assigned aProterozoic age to these rocks, but recent interpretations and new age dates from undeformedintrusions south of the project area, indicated that these deformed rocks can be no younger than 136-137 Ma.

19.0 Recommendations

Expand the geophysical surveys east and west of the Santa Maria porphyry zone, and conductgeophysical surveys on the newly-acquired claims north of and adjacent to the claims that are thesubject of this report.

The monzodiorite dykes found west of the Santa Maria zone should be extensively sampled to testtheir potential for gold mineralization.

A minimum 1,850 meter diamond drilling program should be done with 7 holes (850 m) testingXimena, La Banda and Fiorella vein systems and no fewer than 5 holes (1,000 m) testing portions ofthe Santa Maria porphyry target area. Pending success in either of these areas, the drill program canbe expanded accordingly.

20.0 Budget (US$)

Direct drilling costs (1850 meters @ $200/meter) $370,000Mobilization $ 5,000Water transport for drilling $ 12,000Road and site construction $ 22,000Geology, mapping, sampling $ 40,000Analyses $ 35,000Camping and accommodations $ 22,000Travel expenses $ 6,000Metallurgical and petrographic studies $ 18,000Vehicle service and fuel $ 21,000Environmental studies, reclamation, etc. $ 25,000Camp security $ 30,000Mineral tenure acquisitions and maintenance $ 76,000Office supplies and administration costs $ 10,000Sub-total: $ 693,000

Contingencies (10%) $ 69,300

TOTAL: $ 762,300


21.0 References

Benes, V., Berezansky, A. Lopatina, S., Kozhevnikov, S., Polach, I. & Rusanov, N., 2008, Technical Report Altynor Gold Corporation Alto Quemado and Achasiri Properties Peru.

Carlotto, V., Rodríguez, R., Acosta, H., Cárdenas J., Jaillard, E., 2009, Alto estructural Totos-Paras (Ayacucho): Límite paleogeográfico en la evolución mesozoica de ls cuencas Pucará (Triásico superior-Jurásico) y Arequipa (Jurásico-Cretácico). Volumen Especial No. 7, p 1-45.

Carlotto, V., Acosta, H., Mamani, M., Cerpa, L., Rodriguez R., Jaimes, F., Navarro, P., Cueva, E., Chacaltana, C., 2010, Los dominios geotectónicos del territorio peruano. XV Congreso Peruano de Geología, Resúmenes extendidos. Soc. Geol. Peru. Pub. Esp. No. 9, p 47-50.

Chávez, W., 2010, Estudio microscópico de muestras de roca y mineral proyecto Alto Quemado. Reporte preliminar interno-Mawson.

Ligarda, R., Giraldo, L., Castañeda, T., 2011, Proyecto Alto Quemado, Informe Tecnico, Mawson Resources Ltd.

Mamani, M., Tassara, A., Wörner, G., 2008, Composition and structural control of crustal domains in the central Andes. Geochemistry Geophysics Geosystems G3. An electronic Journal of the earth sciences. Volume 9, Number 3. QO3006.

Mamani, M., Rivera, F., 2011, Sistema de fallas Iquipí-Clavelinas: Zona e transición cortical e implicancias para el emplazamiento de depósitos minerales. Presentación Power Point. VII Congreso Internacional de Exploraciones – Proexplo 2011.

McInnes, D., 2010, Geophysical report from Alto Quemado Project-Peru. Mawson Internal report.

Osorio, E., Noe, J., 2003, Informe de Evaluación Geológica y Geoquímica Proyecto Alto Quemado-Arequipa. Reporte interno preparado para B.I.S.A.

Pineault, R., Fernández, G., 2004, Reporte de Procesamiento Geofísico Proyecto Alto Quemado Departamento de Arequipa, Perú. Preparado por Vald’or Geofísica, para Ximesa S.R.L.

Rivera, F., Leon, J., Cano, O., Huaman, M., 2010, Controles de mineralización en el pórfido de cobre Zafranal, en el sur del Peru. XV Peruano de Geología, Resúmenes extendidos. Soc. Geol. Peru., Pub. Esp. No. 9, p 611-614.

Schildgen, T., Ehlers, T., Whipp, D., Van Soest, M., Whipple, K. & Hodges, K., 2009, Journal of Geophysical Research. Vol. 114, FO4014.

http://www.alsglobal.com

http://www.aqmcopper.com/s/Home.asphttp: // www.goldminerpulse.com

http://www.mawsonresources.com/s/Home.asphttp://www.sgs.com//sitemap.htm

John Nebocat, P.Eng.May 15, 2011Gibsons, B.C. Canada


http://www.sgs.com//sitemap.htm

http://www.goldminerpulse.comhttp://www.mawsonresources.com/s/Home.asp




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APPENDIX I

Mawson Resources Analytical Database


SampleIDAQ1AQ2AQ3AQ4AQ5AQ6AQ7AQ8AQ9

AQ10AQ11AQ12AQ13AQ14AQ15AQ16AQ17AQ18AQ19AQ20AQ21

217801217802217803217804217805217806217807217808217809217810217811217812217813217814217815217816217817217818217819217820217821217822217823217824217825217826217827217828217829217830217831217832217833217834217835217836217837217838217839217840217841217842217843217844217845217846217847217848217849

Prospect Easting Northing SampleType SampleSubTypeSampleWeight_KgMeshSize Au_ppm_mapinfo Ag_ppm Al_% As_ppm B_ppm Ba_ppm Be_ppm Bi_ppm Ca_% Cd_ppm Co_ppm Cr_ppm Cu_ppm Fe_% Ga_ppmXIM 810,262.4 8,223,147.3 ROCKCHIP OUTCROP 0.80 0.060 -1.00 3.69 -50 150 -10 -20 0.27 -10 80 10 7,010 2.69 -50XIM 810,262.4 8,223,147.3 ROCKCHIP OUTCROP 0.74 0.060 -1.00 5.21 -50 70 -10 -20 0.33 -10 80 360 9,310 6.05 -50XIM 810,262.4 8,223,147.3 ROCKCHIP OUTCROP 1.75 0.240 1.00 5.01 -50 110 -10 -20 0.15 -10 20 90 4,030 6.66 -50XIM 810,262.4 8,223,147.3 ROCKCHIP OUTCROP 1.05 0.070 -1.00 5.59 -50 220 -10 -20 0.25 -10 50 -10 5,910 5.15 -50XIM 810,262.4 8,223,147.3 ROCKCHIP ADIT 2.56 0.930 10.00 0.1 -50 -50 -10 -20 -0.05 -10 -10 -10 110 19.35 -50XIM 810,262.4 8,223,147.3 ROCKCHIP ADIT 1.19 695.000 32.00 0.33 -50 -50 -10 -20 -0.05 -10 -10 10 1,150 19.2 -50XIM 810,262.4 8,223,147.3 ROCKCHIP ADIT 3.90 57.300 8.00 1.58 -50 100 -10 20 0.21 -10 80 20 11,700 16.8 -50XIM 810,466.4 8,223,050.3 ROCKCHIP ADIT 2.46 33.100 28.00 0.1 -50 -50 -10 -20 0.18 -10 10 -10 181,000 28.9 -50XIM 810,466.4 8,223,050.3 ROCKCHIP ADIT 4.05 11.850 16.00 0.45 -50 -50 -10 -20 -0.05 -10 20 -10 204,000 14.95 -50XIM 810,466.4 8,223,050.3 ROCKCHIP ADIT 1.94 6.110 12.00 0.89 -50 110 -10 20 -0.05 -10 70 -10 85,500 15.25 -50XIM 810,625.4 8,222,952.3 ROCKCHIP OUTCROP 2.85 0.540 2.00 3.18 -50 240 -10 -20 0.13 -10 20 40 1,750 6.46 -50XIM 810,625.4 8,222,952.3 ROCKCHIP OUTCROP 0.40 0.410 4.00 1.67 -50 120 -10 -20 0.11 -10 10 20 1,260 7.17 -50LAB 810,866.4 8,222,261.3 ROCKCHIP OUTCROP 1.49 3.430 5.00 0.64 -50 170 -10 -20 -0.05 -10 30 10 2,940 6.93 -50STA 811,232.4 8,223,370.3 ROCKCHIP OUTCROP 1.76 0.010 1.00 3.8 -50 640 -10 -20 0.1 -10 -10 30 420 3.76 -50STA 811,234.4 8,223,302.3 ROCKCHIP OUTCROP 1.17 0.010 -1.00 3.5 -50 1530 -10 -20 0.05 -10 -10 20 200 3.03 -50STA 811,387.4 8,223,386.3 ROCKCHIP OUTCROP 1.07 0.020 -1.00 6.44 -50 420 -10 -20 0.5 -10 10 -10 600 5.78 -50STA 811,423.4 8,223,109.3 ROCKCHIP OUTCROP 0.83 1.440 5.00 1.35 -50 180 -10 -20 -0.05 -10 -10 -10 40 0.75 -50STA 811,397.4 8,223,013.3 ROCKCHIP OUTCROP 0.35 -0.010 -1.00 4.9 -50 470 -10 -20 3.96 -10 10 30 100 4.24 -50LAB 811,831.4 8,222,407.3 ROCKCHIP ADIT 2.73 1.620 5.00 1.29 -50 610 -10 -20 -0.05 -10 30 -10 30,700 10.2 -50LAB 811,831.4 8,222,407.3 ROCKCHIP ADIT 4.44 23.900 9.00 2.53 -50 70 -10 30 0.54 -10 70 -10 51,900 9.9 -50LAB 811,831.4 8,222,407.3 ROCKCHIP ADIT 3.77 38.700 13.00 1.45 -50 -50 -10 60 0.99 -10 70 -10 79,300 11.95 -50FIO 810,899.5 8,222,852.9 ROCKCHIP CHANNEL 2.03 1.10 0.757 -0.20 0.2 3 -10 60 -0.5 63 0.03 -0.5 5 5 228 6.11 -10FIO 810,898.9 8,222,851.0 ROCKCHIP CHANNEL 2.61 1.20 0.146 -0.20 1.9 -2 -10 40 -0.5 2 0.08 -0.5 8 1 197 2.57 -10XIM 810,605.8 8,222,976.7 ROCKCHIP CHANNEL 2.98 0.80 0.063 0.30 1.8 -2 -10 80 -0.5 -2 0.12 -0.5 10 13 1,415 5.13 10XIM 810,609.4 8,222,976.2 ROCKCHIP CHANNEL 2.60 0.90 0.418 0.90 0.2 -2 -10 2020 -0.5 3 0.03 -0.5 9 4 314 2.18 -10 QC 1.02 -0.005 -0.20 0.31 -2 -10 60 -0.5 -2 0.09 -0.5 2 1 7 0.68 -10XIM 810,608.3 8,222,978.3 ROCKCHIP CHANNEL 2.87 1.30 0.978 0.60 0.3 -2 -10 260 -0.5 2 0.03 -0.5 17 5 468 2.52 -10XIM 810,610.0 8,222,978.0 ROCKCHIP CHANNEL 2.44 0.90 0.077 0.30 0.6 4 -10 110 -0.5 -2 0.10 -0.5 6 23 892 5.90 10XIM 810,612.3 8,222,977.1 ROCKCHIP CHANNEL 1.89 0.90 0.263 2.50 0.2 5 -10 70 -0.5 2 0.03 -0.5 7 6 1,095 6.58 -10XIM 810,615.7 8,222,975.8 ROCKCHIP CHANNEL 1.84 0.50 0.565 2.50 1.1 2 -10 140 -0.5 3 0.13 -0.5 5 -1 1,335 6.32 10XIM 810,616.1 8,222,976.2 ROCKCHIP CHANNEL 2.61 1.00 0.295 1.20 4.2 -2 -10 60 -0.5 2 0.22 -0.5 14 53 1,740 10.15 10XIM 810,616.1 8,222,980.3 ROCKCHIP CHANNEL 2.55 1.20 0.008 -0.20 3.4 -2 -10 50 -0.5 -2 0.60 -0.5 19 64 1,010 9.58 20XIM 810,625.0 8,223,001.0 ROCKCHIP CHANNEL 1.79 0.80 0.031 -0.20 1.8 -2 -10 100 -0.5 39 0.09 -0.5 3 2 310 6.44 10XIM 810,453.2 8,223,056.5 ROCKCHIP CHANNEL 2.20 0.80 0.085 -0.20 1.0 -2 -10 40 -0.5 2 0.11 -0.5 8 4 963 2.92 -10XIM 810,452.5 8,223,054.6 ROCKCHIP CHANNEL 2.14 1.00 0.162 0.90 1.0 -2 -10 50 -0.5 8 0.11 -0.5 22 1 1,530 4.62 10XIM 810,453.5 8,223,054.6 ROCKCHIP CHANNEL 2.20 0.40 4.540 1.10 0.3 5 -10 20 -0.5 12 0.04 -0.5 10 2 1,885 8.01 -10XIM 810,455.8 8,223,054.1 ROCKCHIP CHANNEL 2.64 0.65 0.143 0.80 0.6 5 -10 10 -0.5 12 0.05 -0.5 6 -1 3,030 6.76 -10XIM 810,457.6 8,223,052.0 ROCKCHIP CHANNEL 2.01 0.60 2.320 0.70 1.5 9 -10 30 -0.5 3 0.07 -0.5 22 -1 4,170 7.24 -10XIM 810,457.0 8,223,051.7 ROCKCHIP CHANNEL 2.51 1.00 0.071 -0.20 1.5 5 -10 30 -0.5 -2 0.14 -0.5 13 49 2,060 3.20 10XIM 810,466.5 8,223,044.9 ROCKCHIP CHANNEL 2.31 1.20 0.633 1.30 0.4 87 -10 130 -0.5 15 0.04 -0.5 24 6 2,570 5.91 10 QC 0.06 2.920 4.80 1.17 6 -10 20 -0.5 16 1.28 -0.5 13 7 15,300 7.52 10XIM 810,466.0 8,223,044.2 ROCKCHIP CHANNEL 2.49 0.40 0.484 0.20 1.7 26 -10 40 -0.5 2 0.16 -0.5 5 4 2,570 3.63 10FIO 810,300.0 8,223,236.0 ROCKCHIP CHANNEL 2.96 0.80 0.337 -0.20 0.6 7 -10 100 -0.5 8 0.06 -0.5 1 28 558 5.72 10FIO 810,299.0 8,223,236.0 ROCKCHIP CHANNEL 1.86 0.60 0.211 -0.20 1.7 9 -10 70 -0.5 3 0.11 -0.5 5 58 792 3.98 10XIM 810,190.0 8,223,148.0 ROCKCHIP CHANNEL 2.41 0.50 0.041 -0.20 2.8 2 -10 60 0.6 -2 0.85 -0.5 20 417 811 4.36 10XIM 810,190.0 8,223,148.5 ROCKCHIP CHANNEL 2.35 0.50 1.095 0.30 2.5 3 -10 60 -0.5 2 0.41 -0.5 39 63 2,230 5.26 10XIM 810,134.4 8,223,224.7 ROCKCHIP CHANNEL 2.76 0.75 0.032 0.70 0.2 -2 -10 60 -0.5 7 0.04 -0.5 4 27 28 3.89 -10XIM 810,136.4 8,223,224.6 ROCKCHIP CHANNEL 1.76 0.65 0.124 0.90 0.4 6 -10 120 -0.5 7 0.06 -0.5 19 9 158 9.72 -10 QC 0.92 -0.005 -0.20 0.36 -2 -10 70 -0.5 -2 0.1 -0.5 2 2 6 0.8 -10XIM 810,134.9 8,223,226.0 ROCKCHIP CHANNEL 2.66 0.60 0.079 1.70 0.8 9 -10 120 -0.5 12 0.06 -0.5 19 5 177 16.50 10XIM 810,147.5 8,223,202.0 ROCKCHIP CHANNEL 2.15 0.65 -0.050 -0.20 1.7 2 -10 150 -0.5 -2 0.37 -0.5 4 3 36 2.67 -10XIM 810,148.5 8,223,202.0 ROCKCHIP CHANNEL 2.46 1.05 -0.050 -0.20 0.4 4 -10 230 -0.5 7 0.11 -0.5 4 -1 87 12.35 10XIM 810,149.0 8,223,202.5 ROCKCHIP CHANNEL 1.75 0.60 -0.050 -0.20 2.5 -2 -10 150 -0.5 -2 0.20 -0.5 4 2 337 9.87 10XIM 810,088.0 8,223,244.0 ROCKCHIP CHANNEL 2.61 1.10 0.060 -0.20 0.6 3 -10 90 -0.5 9 0.10 -0.5 -1 153 210 20.90 10FIO 810,169.0 8,223,457.0 ROCKCHIP CHANNEL 2.76 0.50 0.360 1.60 3.6 4 -10 30 -0.5 13 0.52 -0.5 6 233 1,050 10.70 20FIO 810,169.5 8,223,457.5 ROCKCHIP CHANNEL 2.85 0.50 2.870 0.40 2.9 8 -10 50 0.7 16 0.36 -0.5 13 82 1,890 9.41 10FIO 810,170.0 8,222,458.0 ROCKCHIP CHANNEL 3.46 0.40 0.290 -0.20 3.2 5 -10 30 0.6 2 0.72 -0.5 11 89 869 5.84 10FIO 810,155.0 8,223,467.0 ROCKCHIP CHANNEL 2.48 0.65 -0.050 -0.20 1.2 3 -10 250 -0.5 2 0.26 -0.5 1 59 175 6.06 10FIO 810,155.0 8,223,469.5 ROCKCHIP CHANNEL 3.12 0.50 -0.050 0.60 0.6 14 10 70 0.5 10 0.08 -0.5 6 790 1,190 33.70 10FIO 810,155.5 8,223,469.0 ROCKCHIP CHANNEL 2.72 0.50 0.070 0.20 4.9 2 10 70 -0.5 4 0.32 -0.5 8 643 1,170 7.49 10FIO 810,257.0 8,223,366.0 ROCKCHIP CHANNEL 2.62 0.30 2.470 -0.20 0.9 19 -10 170 1.1 11 0.19 -0.5 21 27 427 26.50 10FIO 810,256.5 8,223,366.0 ROCKCHIP CHANNEL 2.33 0.55 0.180 -0.20 1.8 6 -10 330 0.7 2 0.27 -0.5 14 10 489 15.30 10FIO 810,188.0 8,223,352.0 ROCKCHIP CHANNEL 3.05 0.40 -0.050 0.30 0.5 46 -10 210 1.1 10 0.08 -0.5 3 5 199 12.95 10FIO 810,188.0 8,223,351.5 ROCKCHIP CHANNEL 2.88 0.45 -0.050 -0.20 1.1 2 -10 40 -0.5 -2 0.19 -0.5 1 6 81 2.45 -10XIM 809,933.5 8,223,322.5 ROCKCHIP CHANNEL 2.13 0.40 -0.050 -0.20 2.0 -2 -10 90 -0.5 2 0.17 -0.5 9 7 27 3.00 10XIM 809,933.0 8,223,322.0 ROCKCHIP CHANNEL 2.56 0.25 -0.050 -0.20 1.0 5 -10 160 0.5 17 0.10 -0.5 7 19 122 33.20 20XIM 809,934.0 8,223,320.5 ROCKCHIP CHANNEL 2.96 0.85 -0.050 -0.20 0.6 3 -10 160 -0.5 5 0.07 -0.5 2 -1 66 13.50 10 QC 0.06 0.440 0.80 1.91 13 10 160 0.5 3 1.4 -0.5 12 42 3,450 4.71 10XIM 809,935.5 8,223,319.0 ROCKCHIP CHANNEL 2.96 1.10 0.070 -0.20 0.6 3 -10 50 -0.5 2 0.06 -0.5 1 1 93 7.07 10XIM 809,899.5 8,223,377.0 ROCKCHIP CHANNEL 3.81 1.10 0.110 -0.20 0.8 2 -10 100 -0.5 6 0.11 -0.5 15 42 19 9.40 10

SampleIDAQ1AQ2AQ3AQ4AQ5AQ6AQ7AQ8AQ9

AQ10AQ11AQ12AQ13AQ14AQ15AQ16AQ17AQ18AQ19AQ20AQ21

217801217802217803217804217805217806217807217808217809217810217811217812217813217814217815217816217817217818217819217820217821217822217823217824217825217826217827217828217829217830217831217832217833217834217835217836217837217838217839217840217841217842217843217844217845217846217847217848217849

Hg_ppm K_% La_ppm Mg_% Mn_ppm Mo_ppm Na_% Ni_ppm P_ppm Pb_ppm S_% Sb_ppm Sc_ppm Sr_ppm Th_ppm Ti_% Tl_ppm U_ppm V_ppm W_ppm Zn_ppm Au_ppm Au_ppm_Grav Cu_AA460.5 -50 0.69 1010 -10 4.16 10 580 -20 -0.1 -50 10 90 -50 0.29 -50 -50 120 -50 40 0.0600.1 -50 2.35 1340 -10 1.66 70 690 -20 -0.1 -50 20 50 -50 0.2 -50 -50 90 -50 70 0.0600.5 -50 1.52 770 -10 1.26 10 350 -20 -0.1 -50 10 50 -50 0.16 -50 -50 100 -50 40 0.2401.5 -50 1.61 660 10 2.16 10 410 -20 -0.1 -50 10 70 -50 0.29 -50 -50 140 -50 40 0.070

-0.1 -50 -0.05 70 -10 -0.05 -10 50 -20 0.1 -50 -10 10 -50 -0.05 -50 -50 100 80 -20 0.9300.1 -50 -0.05 60 -10 0.14 -10 1230 -20 0.7 -50 -10 40 -50 -0.05 -50 -50 60 -50 -20 >100 695.0000.1 -50 0.21 940 -10 0.08 -10 1090 -20 0.1 -50 -10 40 -50 -0.05 -50 -50 50 -50 40 57.300

-0.1 -50 -0.05 70 -10 -0.05 -10 -50 -20 25.9 -50 -10 -10 -50 -0.05 -50 -50 -10 -50 20 33.100 18.1-0.1 -50 0.17 140 -10 -0.05 -10 -50 -20 11.8 -50 -10 10 -50 -0.05 -50 -50 10 -50 600 11.850 20.4-0.1 -50 0.08 80 -10 -0.05 30 -50 -20 12.6 -50 -10 10 -50 -0.05 -50 -50 30 -50 -20 6.1100.8 -50 0.78 830 -10 0.38 -10 480 -20 0.1 -50 10 30 -50 0.18 -50 -50 70 -50 20 0.5400.4 -50 0.29 420 -10 -0.05 -10 570 -20 0.1 -50 10 30 -50 0.17 -50 -50 70 -50 -20 0.4100.3 -50 -0.05 100 10 -0.05 -10 120 -20 0.3 -50 -10 10 -50 -0.05 -50 -50 60 -50 -20 3.4301.4 -50 0.21 90 20 1.44 -10 190 -20 -0.1 -50 -10 80 -50 0.1 -50 -50 90 -50 -20 0.0102.2 -50 0.23 90 10 0.56 -10 180 -20 -0.1 -50 -10 50 -50 0.08 -50 -50 40 -50 -20 0.0101.5 -50 0.6 250 40 2.33 -10 500 -20 -0.1 -50 10 130 -50 0.19 -50 -50 90 -50 30 0.0200.8 -50 0.08 80 -10 0.4 -10 -50 -20 0.1 -50 -10 10 -50 -0.05 -50 -50 10 -50 -20 1.4401.1 -50 0.77 740 -10 2.43 -10 630 -20 -0.1 -50 10 390 -50 0.29 -50 -50 110 -50 20 -0.0100.2 -50 0.26 110 60 -0.05 -10 420 -20 1.9 -50 -10 60 -50 0.06 -50 -50 50 -50 -20 1.6200.4 -50 0.5 140 10 0.65 -10 170 -20 7.7 -50 -10 20 -50 0.06 -50 -50 40 -50 -20 23.9000.2 -50 0.29 110 20 0.37 -10 110 -20 10.1 -50 -10 20 -50 -0.05 -50 -50 40 -50 -20 38.700

-1 0.05 -10 0.05 52 8 0.01 4 150 7 0.06 -2 1 8 -20 -0.01 -10 -10 19 -10 3 0.757-1 0.11 20 0.12 26 1 0.02 2 430 -2 0.04 -2 4 197 -20 -0.01 -10 -10 34 -10 -2 0.146-1 0.12 20 0.85 426 1 0.01 13 240 3 0.01 -2 3 18 -20 -0.01 -10 -10 35 -10 25 0.063-1 0.06 -10 0.04 451 1 -0.01 3 130 2 0.11 -2 1 48 -20 -0.01 -10 -10 11 -10 3 0.418-1 0.12 10 0.11 283 -1 0.17 2 80 4 0.01 -2 1 11 -20 0.03 -10 -10 6 -10 23 -0.005-1 0.08 -10 0.04 796 2 -0.01 5 210 -2 0.05 -2 1 8 -20 -0.01 -10 -10 10 -10 5 0.978-1 0.19 10 0.10 262 3 -0.01 5 450 2 0.09 -2 3 20 -20 0.01 -10 -10 32 -10 5 0.077-1 0.08 -10 0.04 460 4 -0.01 5 520 2 0.16 -2 1 9 -20 0.01 -10 -10 32 -10 6 0.263-1 0.34 10 0.38 490 2 0.01 3 460 2 0.33 -2 2 21 -20 -0.01 -10 -10 38 -10 11 0.565-1 0.22 10 2.48 858 -1 0.01 35 1030 3 0.02 -2 9 11 -20 0.01 -10 -10 113 -10 97 0.295-1 0.06 10 2.45 669 -1 0.03 46 2060 4 0.01 -2 11 25 -20 0.14 -10 -10 158 -10 33 0.008-1 0.11 10 0.88 164 4 0.06 1 500 -2 0.21 -2 8 38 -20 0.12 -10 -10 61 -10 13 0.031-1 0.08 -10 0.39 191 1 -0.01 9 180 -2 0.02 -2 2 8 -20 0.01 -10 -10 22 -10 9 0.085-1 0.05 -10 0.38 301 2 -0.01 8 300 -2 0.03 -2 2 9 -20 0.01 -10 -10 35 -10 10 0.162-1 0.04 -10 0.06 121 4 -0.01 5 600 4 0.04 -2 1 4 -20 0.01 -10 -10 27 -10 3 4.540-1 0.03 -10 0.22 111 6 0.01 5 430 4 0.04 -2 1 8 -20 -0.01 -10 -10 25 -10 6 0.143-1 0.05 -10 0.55 560 2 -0.01 10 340 -2 0.02 -2 3 8 -20 -0.01 -10 -10 36 -10 21 2.320-1 0.06 -10 0.62 328 1 0.03 13 140 -2 0.01 -2 2 14 -20 -0.01 -10 -10 24 -10 13 0.071-1 0.04 -10 0.05 672 5 0.03 5 520 2 0.03 2 2 7 -20 -0.01 -10 -10 34 -10 2 0.633-1 0.14 10 1.05 328 3 0.06 17 740 23 1.54 -2 5 67 -20 0.08 -10 -10 95 -10 98 2.920 1.530-1 0.10 -10 0.36 119 1 0.12 12 230 -2 0.03 -2 5 17 -20 -0.01 -10 -10 45 -10 10 0.484-1 0.18 20 0.07 33 4 0.06 2 190 9 0.24 -2 3 34 -20 0.01 -10 -10 44 -10 2 0.337-1 0.09 20 0.13 87 1 0.02 2 340 4 0.07 -2 7 66 20 0.03 -10 -10 83 -10 5 0.211-1 0.12 -10 2.64 735 -1 0.04 130 1550 2 0.01 -2 8 29 -20 0.17 -10 -10 68 -10 45 0.041-1 0.09 10 1.58 627 -1 0.05 36 850 4 0.01 -2 5 39 -20 0.03 -10 -10 52 -10 46 1.095-1 0.07 10 0.02 34 4 0.09 2 260 13 0.37 -2 1 29 -20 0.01 -10 -10 23 -10 4 0.032-1 0.11 10 0.04 53 35 0.13 6 990 12 0.66 -2 5 105 -20 0.02 -10 -10 48 -10 28 0.124-1 0.14 10 0.11 309 -1 0.19 1 80 2 0.02 -2 1 13 -20 0.03 -10 -10 6 -10 23 -0.005-1 0.18 10 0.05 10 11 0.12 3 1390 31 0.50 -2 9 111 -20 0.02 -10 -10 84 -10 45 0.079-1 0.10 10 0.28 77 -1 0.06 2 440 3 0.21 -2 9 90 -20 0.14 -10 -10 83 -10 12 -0.050-1 0.33 -10 0.03 38 5 0.16 -1 680 11 1.11 -2 3 71 -20 0.05 -10 -10 55 -10 5 -0.050-1 0.30 10 0.45 77 2 0.06 1 630 8 0.25 3 11 130 -20 0.10 -10 -10 164 -10 36 -0.050-1 0.08 10 0.06 13 27 0.06 3 360 27 0.16 -2 5 52 -20 0.04 -10 -10 159 -10 16 0.060-1 0.07 20 1.50 269 5 0.03 26 970 589 0.12 -2 20 180 -20 0.17 -10 -10 196 -10 98 0.360-1 0.14 10 1.48 275 4 0.03 34 1320 95 0.09 -2 11 118 -20 0.12 -10 -10 133 -10 139 2.870-1 0.09 10 2.04 448 1 0.04 54 1140 6 0.01 -2 11 57 -20 0.15 -10 -10 131 -10 193 0.290-1 0.26 20 0.47 74 1 0.22 8 650 25 1.01 -2 8 256 -20 0.14 -10 -10 72 -10 21 -0.0501 0.09 10 0.10 19 33 0.11 30 1740 184 0.53 -2 7 120 -20 0.06 -10 -10 287 -10 84 -0.050

-1 0.11 10 2.38 348 2 0.08 133 690 23 0.13 -2 21 148 -20 0.29 -10 -10 168 -10 81 0.0701 0.45 40 0.13 65 15 0.44 23 4230 22 1.86 -2 12 359 -20 0.03 -10 -10 196 -10 15 2.470

-1 0.28 20 0.54 194 3 0.09 13 1450 7 0.49 -2 12 188 -20 0.06 -10 -10 196 -10 30 0.180-1 0.23 50 0.04 34 10 0.12 2 1350 51 0.66 -2 8 205 -20 0.03 -10 -10 49 -10 24 -0.050-1 0.04 30 0.30 56 -1 0.03 4 410 2 0.03 -2 12 49 -20 0.13 -10 -10 35 -10 9 -0.050-1 0.09 10 0.51 80 2 0.04 4 390 2 0.09 -2 7 88 -20 0.05 -10 -10 63 -10 17 -0.0501 0.38 20 0.05 -5 23 0.43 4 2100 20 1.75 -2 19 177 -20 0.03 -10 -10 239 -10 18 -0.050

-1 0.21 10 0.03 14 3 0.07 2 320 5 0.39 -2 4 32 -20 0.03 -10 -10 59 -10 5 -0.0501 0.56 20 1.32 386 204 0.16 18 990 12 0.48 -2 6 86 -20 0.2 -10 -10 106 -10 61 0.440

-1 0.12 -10 0.04 15 3 0.04 2 160 -2 0.05 -2 3 14 -20 0.01 -10 -10 89 -10 9 0.070-1 0.11 10 0.09 43 4 0.12 6 740 4 0.47 -2 5 106 -20 0.06 -10 -10 92 -10 15 0.110

SampleID217850217851217852217853217854217855217856217857217858217859217860217861217862217863217864217865217866217867217868217869217870217871217872217873217874217875217876217877217878217879217880217881217882217883217884217885217886217887217888217889217890217891217892217893217894217895217896217897217898217899217900217911217912217913217914217915217916217917217918217919217920217921217922217923217924217925217926217927217928217929

Prospect Easting Northing SampleType SampleSubTypeSampleWeight_KgMeshSize Au_ppm_mapinfo Ag_ppm Al_% As_ppm B_ppm Ba_ppm Be_ppm Bi_ppm Ca_% Cd_ppm Co_ppm Cr_ppm Cu_ppm Fe_% Ga_ppmXIM 809,899.0 8,223,376.0 ROCKCHIP CHANNEL 2.50 0.30 0.130 0.20 0.5 14 -10 130 -0.5 40 0.08 -0.5 66 12 70 24.10 10XIM 809,899.0 8,223,375.5 ROCKCHIP CHANNEL 2.23 0.70 -0.050 -0.20 0.4 2 -10 150 -0.5 5 0.06 -0.5 23 8 20 6.28 10XIM 809,899.0 8,223,375.0 ROCKCHIP CHANNEL 4.38 0.80 -0.050 -0.20 0.6 2 -10 170 -0.5 3 0.06 -0.5 10 21 30 7.12 10XIM 809,899.5 8,223,373.0 ROCKCHIP CHANNEL 2.88 0.35 0.110 -0.20 0.7 6 -10 110 -0.5 19 0.11 -0.5 13 78 49 26.60 30XIM 809,899.5 8,223,372.6 ROCKCHIP CHANNEL 2.49 0.45 -0.050 -0.20 0.6 3 -10 80 -0.5 2 0.06 -0.5 19 12 22 6.49 -10XIM 809,899.5 8,223,372.0 ROCKCHIP CHANNEL 2.99 1.15 0.060 -0.20 0.5 4 -10 60 -0.5 8 0.05 -0.5 12 10 12 6.75 -10FIO 810,580.0 8,223,137.5 ROCKCHIP CHANNEL 2.07 0.80 0.130 -0.20 0.3 -2 -10 110 -0.5 3 0.02 -0.5 1 4 8 5.02 -10XIM 810,252.0 8,223,143.5 ROCKCHIP CHANNEL 2.85 0.40 -0.050 0.40 1.3 7 -10 80 -0.5 2 0.09 -0.5 38 26 2,180 4.34 10XIM 810,252.5 8,223,144.0 ROCKCHIP CHANNEL 2.00 0.35 0.330 0.80 2.4 17 -10 40 -0.5 12 0.19 -0.5 16 78 7,560 7.80 10XIM 810,253.0 8,223,144.5 ROCKCHIP CHANNEL 2.41 0.40 0.290 0.20 3.4 8 -10 50 -0.5 8 0.25 -0.5 57 210 6,430 7.89 10XIM 810,025.0 8,223,260.0 ROCKCHIP CHANNEL 2.86 1.00 0.160 0.40 1.0 12 -10 110 -0.5 30 0.11 -0.5 39 36 96 17.40 10XIM 810,026.0 8,223,261.0 ROCKCHIP CHANNEL 2.41 0.70 0.270 0.40 0.6 14 10 140 -0.5 17 0.18 -0.5 25 42 144 32.40 10FIO 810,047.0 8,223,694.5 ROCKCHIP CHANNEL 2.85 0.70 -0.050 -0.20 1.0 -2 -10 50 -0.5 -2 0.32 -0.5 5 3 9 2.16 -10 QC 1.18 -0.050 -0.20 0.36 3 -10 70 -0.5 -2 0.11 -0.5 2 2 5 0.85 -10FIO 810,048.0 8,223,695.0 ROCKCHIP CHANNEL 3.27 0.90 -0.050 -0.20 1.7 3 -10 70 -0.5 -2 0.42 -0.5 9 4 7 2.59 10FIO 810,039.0 8,223,693.5 ROCKCHIP CHANNEL 3.01 0.90 -0.050 -0.20 1.0 2 -10 20 -0.5 -2 0.23 -0.5 5 4 1 1.74 -10FIO 810,039.0 8,223,693.0 ROCKCHIP CHANNEL 3.43 0.60 -0.050 -0.20 2.1 2 -10 30 -0.5 -2 0.19 -0.5 11 64 2 3.06 10FIO 810,037.0 8,223,692.0 ROCKCHIP CHANNEL 3.31 1.00 -0.050 -0.20 1.6 2 -10 20 -0.5 -2 0.33 -0.5 4 16 2 2.44 10FIO 810,036.5 8,223,691.0 ROCKCHIP CHANNEL 2.94 1.50 -0.050 -0.20 0.7 3 -10 20 -0.5 -2 0.20 -0.5 2 3 1 1.35 -10FIO 810,036.5 8,223,689.0 ROCKCHIP CHANNEL 2.69 0.60 0.160 -0.20 1.6 4 -10 20 -0.5 -2 0.96 -0.5 2 2 1 2.49 10FIO 810,036.5 8,223,688.5 ROCKCHIP CHANNEL 3.03 0.65 -0.050 -0.20 5.3 4 -10 20 -0.5 -2 3.08 -0.5 13 42 -1 6.52 20XIM 809,867.0 8,223,367.5 ROCKCHIP CHANNEL 3.42 0.70 -0.050 -0.20 4.0 4 -10 130 -0.5 3 0.46 -0.5 8 3 185 5.34 10XIM 809,868.0 8,223,368.0 ROCKCHIP CHANNEL 2.79 0.70 0.160 1.10 2.7 2 -10 100 -0.5 10 0.25 -0.5 -1 26 323 8.23 10XIM 809,869.0 8,223,368.0 ROCKCHIP CHANNEL 2.39 0.75 0.070 -0.20 2.2 2 -10 90 -0.5 7 0.25 -0.5 1 17 514 9.76 10 QC 1.31 -0.050 -0.20 0.41 2 -10 70 -0.5 -2 0.12 -0.5 2 2 6 0.86 -10XIM 809,871.0 8,223,367.0 ROCKCHIP CHANNEL 2.76 0.85 0.130 -0.20 1.7 4 -10 170 -0.5 33 0.19 -0.5 2 23 336 14.55 10XIM 809,872.0 8,223,370.0 ROCKCHIP CHANNEL 2.58 1.20 -0.050 -0.20 2.0 4 -10 100 -0.5 4 0.19 -0.5 2 2 35 4.42 10LAB 811,498.0 8,222,472.0 ROCKCHIP CHANNEL 3.47 0.70 -0.050 -0.20 1.9 -2 -10 60 -0.5 2 0.17 -0.5 10 -1 1,880 3.21 -10LAB 811,498.0 8,222,471.0 ROCKCHIP CHANNEL 3.58 0.90 0.070 0.40 1.9 6 -10 50 -0.5 3 0.10 -0.5 43 -1 1,020 4.23 10LAB 811,498.0 8,222,470.3 ROCKCHIP CHANNEL 2.58 0.55 -0.050 0.30 0.6 28 -10 60 -0.5 8 0.04 -0.5 199 -1 1,520 5.26 10LAB 811,493.0 8,222,469.0 ROCKCHIP CHANNEL 3.82 1.00 -0.050 -0.20 0.6 2 -10 30 -0.5 -2 0.01 -0.5 9 10 199 1.57 -10LAB 811,493.0 8,222,468.0 ROCKCHIP CHANNEL 2.81 0.70 -0.050 -0.20 1.0 2 -10 30 -0.5 -2 0.07 -0.5 6 2 239 1.84 -10LAB 811,492.7 8,222,467.0 ROCKCHIP CHANNEL 2.65 0.75 -0.050 -0.20 0.7 -2 -10 20 -0.5 -2 0.08 -0.5 4 3 176 1.31 -10LAB 811,427.0 8,222,481.5 ROCKCHIP CHANNEL 2.97 0.60 -0.050 -0.20 2.0 -2 -10 50 -0.5 -2 0.20 -0.5 8 -1 21 3.71 10LAB 811,427.0 8,222,482.5 ROCKCHIP CHANNEL 4.55 0.90 -0.050 -0.20 1.3 4 -10 30 -0.5 -2 0.06 -0.5 8 4 164 2.81 -10LAB 811,426.5 8,222,484.0 ROCKCHIP CHANNEL 5.13 1.90 -0.050 -0.20 0.7 -2 -10 20 -0.5 -2 0.02 -0.5 4 8 52 1.77 -10LAB 811,358.0 8,222,507.0 ROCKCHIP CHANNEL 3.43 0.90 -0.050 -0.20 1.7 3 -10 50 -0.5 -2 0.14 -0.5 12 -1 21 3.59 -10LAB 811,359.0 8,222,508.0 ROCKCHIP CHANNEL 3.55 0.90 -0.050 -0.20 1.2 -2 -10 40 -0.5 -2 0.06 -0.5 5 7 11 2.57 -10 QC 0.07 -0.050 -0.20 0.02 2 -10 10 -0.5 -2 -0.01 -0.5 1 23 8 0.58 -10LAB 811,359.0 8,222,509.3 ROCKCHIP CHANNEL 2.90 1.65 -0.050 -0.20 1.1 -2 -10 50 -0.5 -2 0.06 -0.5 6 4 21 3.14 -10LAB 811,887.0 8,222,402.5 ROCKCHIP CHANNEL 3.59 0.80 2.450 0.30 2.4 6 -10 20 -0.5 5 0.13 -0.5 24 -1 5,650 6.81 10LAB 811,888.0 8,222,401.5 ROCKCHIP CHANNEL 4.14 0.50 5.780 2.90 1.3 19 -10 30 -0.5 48 0.06 -0.5 9 -1 11,950 10.95 10LAB 811,886.0 8,222,401.3 ROCKCHIP CHANNEL 3.32 0.60 2.260 2.20 0.8 31 -10 40 -0.5 4 0.05 -0.5 40 -1 39,300 7.64 -10LAB 811,884.0 8,222,402.0 ROCKCHIP CHANNEL 3.24 1.35 -0.050 0.90 1.0 20 -10 40 -0.5 6 0.07 -0.5 57 -1 11,300 4.93 -10LAB 811,884.0 8,222,401.0 ROCKCHIP CHANNEL 3.38 0.55 2.790 1.90 0.6 13 -10 60 -0.5 10 0.04 -0.5 35 -1 14,100 5.27 -10LAB 811,884.0 8,222,400.5 ROCKCHIP CHANNEL 3.12 0.25 11.000 8.80 0.6 23 -10 230 -0.5 10 0.03 -0.5 90 -1 33,100 12.00 -10LAB 811,882.0 8,222,399.5 ROCKCHIP CHANNEL 2.69 1.35 0.570 0.20 2.3 6 -10 20 -0.5 21 0.04 -0.5 88 -1 15,450 5.67 10LAB 811,882.0 8,222,398.5 ROCKCHIP CHANNEL 5.29 1.70 -0.050 0.20 2.5 3 -10 20 -0.5 -2 0.10 -0.5 20 53 926 4.85 10LAB 811,881.0 8,222,397.7 ROCKCHIP CHANNEL 3.39 1.10 -0.050 -0.20 2.7 4 -10 20 -0.5 -2 0.12 -0.5 17 32 988 4.91 10LAB 811,880.0 8,222,497.0 ROCKCHIP CHANNEL 2.57 0.60 -0.050 -0.20 2.6 9 -10 10 -0.5 2 0.07 -0.5 27 95 675 5.51 10 QC 0.06 -0.050 -0.20 0.03 -2 -10 10 -0.5 -2 -0.01 -0.5 2 25 17 0.6 -10REG 812,058.0 8,223,657.0 ROCKCHIP FLOAT 2.18 -0.005 -0.20 0.1 -2 -10 20 -0.5 -2 0.01 -0.5 2 9 7 0.93 -10REG 812,110.0 8,223,728.0 ROCKCHIP CHANNEL 1.56 0.30 -0.005 -0.20 0.0 -2 -10 -10 -0.5 -2 0.02 -0.5 2 10 7 0.78 -10REG 810,754.0 8,223,587.0 ROCKCHIP FLOAT 1.90 -0.005 -0.20 0.0 5 -10 20 -0.5 -2 0.02 -0.5 9 9 61 3.78 -10REG 810,680.0 8,223,667.0 ROCKCHIP CHIPS 1.47 2.00 -0.005 -0.20 0.6 -2 -10 20 -0.5 3 0.21 -0.5 12 -1 35 17.70 20REG 810,524.0 8,223,667.0 ROCKCHIP FLOAT 1.79 -0.005 -0.20 0.0 7 -10 20 -0.5 -2 0.02 -0.5 4 10 39 3.50 -10REG 810,604.0 8,222,089.0 ROCKCHIP CHANNEL 1.65 1.20 0.005 -0.20 1.0 -2 -10 90 -0.5 -2 0.27 -0.5 16 16 32 3.48 -10LAU 811,255.0 8,222,651.3 ROCKCHIP CHANNEL 1.39 1.30 0.015 0.30 0.3 -2 -10 30 -0.5 4 0.06 -0.5 9 1 35 3.84 -10LAU 811,254.1 8,222,650.6 ROCKCHIP CHANNEL 1.26 1.50 0.027 2.00 0.3 -2 -10 70 -0.5 25 0.16 -0.5 7 -1 141 12.85 -10LAU 811,268.5 8,222,640.1 ROCKCHIP CHANNEL 1.18 0.40 0.026 -0.20 0.5 2 -10 20 -0.5 7 0.04 -0.5 1 -1 394 8.94 -10LAU 811,269.8 8,222,645.2 ROCKCHIP CHANNEL 1.82 1.05 0.013 -0.20 0.4 -2 -10 20 -0.5 10 0.04 -0.5 2 -1 118 4.70 -10LAU 811,268.1 8,222,643.3 ROCKCHIP CHANNEL 1.34 0.60 0.025 -0.20 0.4 -2 -10 20 -0.5 7 0.05 -0.5 2 1 56 3.11 -10LAU 811,270.8 8,222,642.6 ROCKCHIP CHANNEL 2.40 0.90 0.013 -0.20 0.3 -2 -10 10 -0.5 8 0.02 -0.5 2 1 81 3.79 -10LAU 811,270.4 8,222,643.4 ROCKCHIP CHANNEL 0.95 0.45 0.056 0.30 0.2 -2 -10 20 -0.5 9 0.04 -0.5 14 2 67 3.00 -10LAU 811,270.6 8,222,644.2 ROCKCHIP CHANNEL 1.08 0.75 0.090 0.20 0.3 2 -10 50 -0.5 23 0.12 -0.5 5 1 43 5.83 -10LAU 811,271.0 8,222,645.0 ROCKCHIP CHANNEL 2.15 1.00 0.010 -0.20 0.4 -2 -10 40 -0.5 3 0.19 -0.5 2 1 50 2.59 -10LAU 811,270.4 8,222,645.7 ROCKCHIP CHANNEL 1.85 1.50 0.009 -0.20 0.7 -2 -10 20 -0.5 3 0.06 -0.5 3 1 49 1.76 -10LAU 811,279.1 8,222,644.9 ROCKCHIP CHANNEL 1.12 0.90 0.009 -0.20 1.4 -2 -10 40 -0.5 -2 0.13 -0.5 10 -1 43 3.80 -10

QC 0.06 0.346 1.00 1.96 12 -10 160 0.5 3 1.37 -0.5 13 42 3,500 4.76 10LAU 811,248.8 8,222,642.7 ROCKCHIP CHANNEL 1.84 1.40 0.032 -0.20 0.5 -2 -10 20 -0.5 11 0.06 -0.5 17 -1 22 4.33 -10

SampleID217850217851217852217853217854217855217856217857217858217859217860217861217862217863217864217865217866217867217868217869217870217871217872217873217874217875217876217877217878217879217880217881217882217883217884217885217886217887217888217889217890217891217892217893217894217895217896217897217898217899217900217911217912217913217914217915217916217917217918217919217920217921217922217923217924217925217926217927217928217929

Hg_ppm K_% La_ppm Mg_% Mn_ppm Mo_ppm Na_% Ni_ppm P_ppm Pb_ppm S_% Sb_ppm Sc_ppm Sr_ppm Th_ppm Ti_% Tl_ppm U_ppm V_ppm W_ppm Zn_ppm Au_ppm Au_ppm_Grav Cu_AA461 0.27 30 0.04 32 10 0.47 10 1960 11 1.78 -2 4 221 -20 0.03 -10 -10 79 -10 15 0.130

-1 0.16 10 0.02 27 2 0.13 4 320 5 1.07 -2 1 69 -20 0.02 -10 -10 20 -10 3 -0.050-1 0.10 10 0.03 26 2 0.06 6 360 4 0.22 -2 2 35 -20 0.02 -10 -10 42 -10 6 -0.0501 0.12 10 0.05 17 6 0.15 4 1240 8 0.66 -2 6 72 -20 0.05 -10 -10 144 -10 8 0.110

-1 0.12 10 0.03 34 1 0.07 5 630 -2 0.26 -2 4 54 -20 0.02 -10 -10 48 -10 8 -0.050-1 0.11 10 0.03 31 2 0.06 4 510 -2 0.18 -2 3 32 -20 0.02 -10 -10 41 -10 8 0.060-1 0.21 -10 0.02 28 13 0.01 2 300 10 0.13 -2 1 48 -20 -0.01 -10 -10 9 -10 17 0.130-1 0.01 -10 0.89 250 1 0.01 19 320 -2 0.05 -2 2 13 -20 0.01 -10 -10 39 -10 32 -0.050-1 0.01 20 1.09 337 1 0.02 22 1130 4 0.02 -2 7 73 -20 -0.01 -10 -10 79 -10 40 0.3301 0.01 10 2.43 445 1 0.03 69 620 3 0.02 -2 12 26 -20 0.01 -10 -10 96 -10 64 0.290

-1 0.13 10 0.11 37 12 0.22 18 840 13 0.72 -2 12 67 -20 0.03 -10 -10 210 -10 24 0.160-1 0.20 30 0.11 52 20 0.36 19 2480 29 1.35 -2 3 156 -20 0.02 -10 -10 174 -10 67 0.270-1 0.10 50 0.74 255 -1 0.05 5 1050 2 0.01 -2 3 13 -20 0.01 -10 -10 18 -10 20 -0.050-1 0.16 10 0.11 328 -1 0.17 2 90 2 0.02 -2 1 14 -20 0.03 -10 -10 6 -10 32 -0.050-1 0.08 50 1.22 764 1 0.04 12 920 2 0.01 -2 4 23 -20 0.01 -10 -10 33 -10 23 -0.050-1 0.04 70 0.81 260 -1 0.06 5 860 2 0.01 -2 3 6 20 -0.01 -10 -10 19 -10 16 -0.050-1 0.05 10 2.14 430 -1 0.03 44 510 -2 0.01 -2 5 7 -20 -0.01 -10 -10 42 -10 36 -0.050-1 0.06 40 1.43 315 -1 0.03 8 550 -2 -0.01 -2 2 11 -20 -0.01 -10 -10 23 -10 28 -0.050-1 0.02 50 0.55 184 -1 0.06 2 390 -2 -0.01 -2 2 5 -20 -0.01 -10 -10 8 -10 16 -0.050-1 0.05 40 1.17 297 1 0.05 2 410 2 -0.01 -2 3 28 20 -0.01 -10 -10 28 -10 29 0.160-1 0.06 10 5.90 865 1 0.01 31 920 3 -0.01 -2 24 34 -20 0.01 -10 -10 265 -10 96 -0.050-1 0.27 -10 1.67 389 2 0.01 9 530 5 -0.01 -2 13 36 -20 0.15 -10 -10 170 -10 80 -0.0501 0.20 -10 1.57 237 7 -0.01 10 390 30 0.04 -2 10 36 -20 0.10 -10 -10 124 -10 62 0.160

-1 0.15 -10 1.24 258 3 0.01 7 340 39 0.04 -2 13 32 -20 0.08 -10 -10 179 -10 53 0.070-1 0.15 10 0.13 332 -1 0.16 1 100 2 0.01 -2 1 15 -20 0.03 -10 -10 8 -10 28 -0.0501 0.26 10 0.67 102 34 0.04 9 730 16 0.37 -2 11 67 -20 0.09 -10 -10 243 -10 32 0.130

-1 0.16 10 1.29 232 5 0.05 4 420 3 0.10 -2 8 39 -20 0.12 -10 -10 96 -10 26 -0.050-1 0.15 -10 0.84 223 1 0.01 1 360 -2 -0.01 -2 2 12 -20 -0.01 -10 -10 27 -10 25 -0.050-1 0.10 -10 0.96 305 3 -0.01 1 300 3 0.01 -2 3 6 -20 -0.01 -10 -10 37 -10 33 0.070-1 0.03 -10 0.27 528 8 -0.01 5 310 4 0.01 -2 2 5 -20 -0.01 -10 -10 68 10 15 -0.050-1 0.03 -10 0.28 88 1 -0.01 1 110 -2 0.01 -2 -1 3 -20 -0.01 -10 -10 9 -10 11 -0.050-1 0.11 -10 0.29 170 -1 0.01 2 180 -2 -0.01 -2 1 6 -20 -0.01 -10 -10 11 -10 11 -0.050-1 0.04 -10 0.29 114 -1 0.01 1 100 -2 -0.01 -2 1 7 -20 -0.01 -10 -10 11 -10 7 -0.050-1 0.06 10 1.13 326 1 0.01 -1 370 -2 -0.01 -2 3 16 -20 -0.01 -10 -10 40 -10 22 -0.050-1 0.10 -10 0.76 217 1 -0.01 -1 200 2 -0.01 -2 2 6 -20 -0.01 -10 -10 26 -10 19 -0.050-1 0.07 -10 0.35 133 1 -0.01 1 320 -2 0.01 -2 1 3 -20 -0.01 -10 -10 15 -10 16 -0.050-1 0.30 10 0.63 316 1 0.01 2 680 -2 -0.01 -2 2 11 -20 -0.01 -10 -10 21 -10 18 -0.050-1 0.19 -10 0.53 252 -1 -0.01 1 380 -2 -0.01 -2 1 4 -20 -0.01 -10 -10 12 -10 20 -0.050-1 -0.01 -10 -0.01 77 5 -0.01 4 10 -2 -0.01 -2 -1 -1 -20 -0.01 -10 -10 1 -10 9 -0.050-1 0.13 -10 0.45 248 1 -0.01 1 340 -2 0.01 -2 1 7 -20 -0.01 -10 -10 22 -10 23 -0.050-1 0.09 -10 1.31 389 4 0.02 2 460 -2 -0.01 -2 2 6 -20 -0.01 -10 -10 49 -10 24 2.450-1 0.09 -10 0.68 165 45 0.07 3 670 10 0.33 -2 2 19 -20 -0.01 -10 -10 144 -10 16 5.780 1.1951 0.01 -10 0.48 172 17 -0.01 2 560 -2 0.10 -2 2 6 -20 -0.01 -10 -10 79 -10 16 2.260 3.930

-1 0.02 -10 0.51 364 8 -0.01 4 740 -2 0.07 -2 2 5 -20 -0.01 -10 -10 80 -10 17 -0.050 1.1301 0.01 -10 0.31 110 11 -0.01 4 590 -2 0.09 -2 1 6 -20 -0.01 -10 -10 81 -10 12 2.790 1.4101 0.01 -10 0.35 206 33 -0.01 3 620 3 0.49 -2 2 5 -20 -0.01 -10 -10 101 -10 10 11.000 3.310

-1 0.03 -10 1.47 658 5 -0.01 8 400 -2 0.02 -2 3 5 -20 -0.01 -10 -10 51 -10 26 0.570 1.545-1 0.05 10 1.50 248 2 0.03 22 510 -2 -0.01 -2 4 3 -20 -0.01 -10 -10 50 -10 28 -0.050-1 0.04 10 1.82 333 1 0.02 12 520 2 -0.01 -2 5 3 -20 -0.01 -10 -10 56 -10 30 -0.050-1 0.02 10 1.81 397 2 0.01 13 360 -2 -0.01 -2 8 2 -20 -0.01 -10 -10 61 -10 32 -0.050-1 -0.01 -10 0.01 78 5 -0.01 5 10 -2 -0.01 -2 -1 -1 -20 -0.01 -10 -10 2 -10 9 -0.050-1 0.03 -10 0.06 89 1 0.01 3 50 -2 0.03 -2 -1 7 -20 -0.01 -10 -10 4 -10 3 -0.005-1 0.01 -10 0.03 82 1 0.01 2 10 -2 -0.01 -2 -1 2 -20 -0.01 -10 -10 1 -10 2 -0.005-1 -0.01 -10 0.02 107 2 -0.01 11 120 2 0.02 -2 -1 5 -20 -0.01 -10 -10 15 -10 4 -0.005-1 0.03 10 0.36 297 -1 0.02 24 40 3 0.01 -2 4 14 -20 0.16 -10 -10 680 -10 44 -0.005-1 0.01 -10 0.02 94 1 0.01 10 170 -2 0.04 -2 -1 8 -20 -0.01 -10 -10 52 -10 2 -0.005-1 0.24 10 0.33 674 5 0.01 21 1140 42 0.02 -2 7 12 -20 -0.01 -10 -10 39 -10 31 0.005-1 0.09 -10 0.02 47 14 0.06 1 410 -2 0.09 -2 -1 19 -20 -0.01 -10 -10 15 -10 3 0.015-1 0.12 -10 0.07 97 23 0.07 -1 750 4 0.27 -2 -1 31 -20 -0.01 -10 -10 7 -10 2 0.027-1 0.09 10 0.02 24 5 0.04 -1 500 3 0.09 -2 1 73 -20 -0.01 -10 -10 48 -10 -2 0.026-1 0.10 10 0.02 25 16 0.03 -1 140 -2 0.03 -2 1 8 -20 -0.01 -10 -10 9 -10 -2 0.013-1 0.08 10 0.02 31 10 0.04 -1 270 -2 0.03 -2 -1 44 -20 -0.01 -10 -10 10 -10 -2 0.025-1 0.09 10 0.02 25 6 0.05 -1 80 2 0.04 -2 -1 5 -20 -0.01 -10 -10 9 -10 -2 0.013-1 0.04 -10 0.02 35 20 0.05 1 150 2 0.53 -2 -1 7 -20 -0.01 -10 -10 3 -10 -2 0.056-1 0.17 -10 0.05 94 29 0.03 5 760 4 0.24 -2 -1 16 -20 0.01 -10 -10 12 -10 7 0.090-1 0.10 10 0.17 51 14 0.05 2 460 2 0.03 -2 1 21 -20 -0.01 -10 -10 10 -10 2 0.010-1 0.08 10 0.06 46 5 0.03 1 110 -2 0.02 -2 1 12 -20 -0.01 -10 -10 10 -10 -2 0.009-1 0.14 20 0.35 78 15 0.04 -1 450 2 0.02 -2 2 19 -20 -0.01 -10 -10 22 -10 7 0.009-1 0.56 20 1.29 387 217 0.17 18 1010 11 0.49 -2 6 94 -20 0.21 -10 -10 111 -10 63 0.346-1 0.20 10 0.08 188 13 0.02 2 460 -2 0.07 -2 1 9 -20 -0.01 -10 -10 5 -10 2 0.032

SampleID217930217931217932217933217934217935217936217937217938217939217940217941217942217943217944217945217946217947217948217949217950217951217952217953217954217955217956217957217958217959217960217961217962217963217964217965217966217967217968217969217970217971217972217973217974217975217976217977217978217979217980217981217982217983217984217985217986217987217988217989217990217991217992217993217994217995217996217997217998217999

Prospect Easting Northing SampleType SampleSubTypeSampleWeight_KgMeshSize Au_ppm_mapinfo Ag_ppm Al_% As_ppm B_ppm Ba_ppm Be_ppm Bi_ppm Ca_% Cd_ppm Co_ppm Cr_ppm Cu_ppm Fe_% Ga_ppmLAU 811,248.0 8,222,642.0 ROCKCHIP CHANNEL 1.96 0.90 0.014 -0.20 0.4 -2 -10 20 -0.5 4 0.05 -0.5 11 1 10 3.03 -10LAU 811,247.1 8,222,641.3 ROCKCHIP CHANNEL 1.92 1.40 0.023 -0.20 1.7 -2 -10 20 -0.5 4 0.20 -0.5 15 -1 26 5.70 -10LAU 811,246.3 8,222,640.7 ROCKCHIP CHANNEL 2.58 0.60 0.089 -0.20 0.7 -2 -10 20 -0.5 36 0.08 -0.5 45 -1 139 11.05 -10LAU 811,245.4 8,222,640.0 ROCKCHIP CHANNEL 3.00 1.60 0.022 0.20 0.4 -2 -10 20 -0.5 5 0.03 -0.5 75 1 21 3.25 -10LAU 811,243.9 8,222,639.0 ROCKCHIP CHANNEL 2.40 1.95 0.031 0.20 0.6 2 -10 40 -0.5 7 0.06 -0.5 15 -1 24 7.93 -10LAU 811,242.9 8,222,638.2 ROCKCHIP CHANNEL 1.81 0.90 -0.005 -0.20 1.6 -2 -10 30 -0.5 -2 0.07 -0.5 4 1 12 1.49 -10FIO 810,654.5 8,223,099.2 ROCKCHIP CHANNEL 2.01 1.20 0.553 -0.20 0.6 2 -10 100 -0.5 13 0.09 -0.5 2 59 241 13.65 10FIO 810,653.5 8,223,098.0 ROCKCHIP CHANNEL 2.38 1.45 0.817 -0.20 0.6 4 -10 100 -0.5 26 0.09 -0.5 -1 57 315 14.30 10FIO 810,653.0 8,223,097.0 ROCKCHIP CHANNEL 1.30 0.90 0.055 -0.20 0.7 -2 -10 50 -0.5 -2 0.06 -0.5 2 13 56 1.49 -10FIO 810,892.2 8,222,882.7 ROCKCHIP CHANNEL 1.50 0.90 0.245 0.40 2.0 9 -10 300 -0.5 5 0.24 -0.5 2 -1 1,610 6.87 10FIO 810,891.4 8,222,883.5 ROCKCHIP CHANNEL 1.67 0.70 1.045 0.50 0.4 25 -10 360 -0.5 180 0.05 -0.5 3 -1 2,230 15.10 -10 QC 0.06 -0.005 -0.20 0.02 -2 -10 10 -0.5 2 -0.01 -0.5 2 22 10 0.57 -10FIO 810,889.6 8,222,884.2 ROCKCHIP CHANNEL 1.52 0.70 0.354 0.30 1.6 38 -10 140 0.5 23 0.15 -0.5 9 45 4,220 13.30 10FIO 810,674.2 8,223,124.1 ROCKCHIP CHANNEL 2.07 0.40 0.069 0.30 3.4 2 -10 160 0.6 4 0.42 -0.5 32 299 3,170 6.39 10FIO 810,672.5 8,223,126.2 ROCKCHIP CHANNEL 2.56 1.30 2.440 1.60 0.7 2 -10 90 -0.5 84 0.05 -0.5 1 48 791 7.27 -10FIO 810,672.0 8,223,126.0 ROCKCHIP CHANNEL 2.28 0.90 0.122 -0.20 1.3 -2 -10 110 -0.5 10 0.11 -0.5 -1 177 900 9.69 10FIO 810,626.5 8,223,107.8 ROCKCHIP CHANNEL 1.79 0.50 0.144 -0.20 0.9 -2 -10 40 -0.5 10 0.08 -0.5 -1 283 550 10.75 20FIO 810,624.7 8,223,108.4 ROCKCHIP CHANNEL 2.91 1.35 0.666 0.20 0.4 -2 -10 130 -0.5 21 0.06 -0.5 1 15 134 6.59 10FIO 810,626.8 8,223,110.0 ROCKCHIP CHANNEL 1.98 0.90 0.744 -0.20 0.3 -2 -10 190 -0.5 11 0.03 -0.5 1 6 72 4.52 -10FIO 810,626.7 8,223,112.5 ROCKCHIP CHANNEL 2.73 1.55 1.270 0.20 0.3 3 -10 90 -0.5 41 0.11 -0.5 -1 21 445 12.20 10 QC 1.04 0.007 -0.20 0.31 -2 -10 60 -0.5 -2 0.09 -0.5 2 2 5 0.72 -10FIO 810,575.5 8,223,153.0 ROCKCHIP CHANNEL 2.39 0.60 0.159 -0.20 2.2 4 -10 90 -0.5 5 0.14 -0.5 6 586 107 13.70 10FIO 810,577.0 8,223,150.0 ROCKCHIP CHANNEL 2.60 0.45 2.240 0.50 0.4 3 -10 130 -0.5 10 0.02 -0.5 1 4 24 7.12 -10FIO 810,576.4 8,223,153.0 ROCKCHIP CHANNEL 1.76 0.50 0.765 -0.20 0.4 -2 -10 130 -0.5 9 0.04 -0.5 1 9 28 6.45 10XIM 810,312.8 8,223,113.8 ROCKCHIP CHANNEL 2.67 1.30 0.236 -0.20 2.3 2 -10 60 -0.5 4 0.19 -0.5 21 -1 5,080 5.07 10XIM 810,311.5 8,223,113.6 ROCKCHIP CHANNEL 2.52 1.30 0.043 -0.20 2.8 -2 -10 70 -0.5 -2 0.22 -0.5 36 -1 3,310 5.17 10XIM 810,310.6 8,223,113.5 ROCKCHIP CHANNEL 2.90 0.50 0.015 -0.20 2.4 2 -10 50 -0.5 -2 0.17 -0.5 25 -1 3,770 4.62 10XIM 810,310.4 8,223,116.2 ROCKCHIP CHANNEL 3.07 1.00 2.410 0.90 1.5 14 -10 40 -0.5 14 0.06 -0.5 27 144 6,890 8.20 10XIM 810,309.0 8,223,113.0 ROCKCHIP CHANNEL 2.34 0.60 0.562 -0.20 3.2 -2 -10 20 -0.5 10 0.16 -0.5 66 364 11,700 5.84 10XIM 810,308.6 8,223,112.8 ROCKCHIP CHANNEL 1.90 0.45 0.039 -0.20 2.5 5 -10 150 -0.5 14 0.30 -0.5 71 156 8,550 5.21 10XIM 810,307.8 8,223,112.2 ROCKCHIP CHANNEL 2.43 1.50 0.017 -0.20 2.0 -2 -10 100 -0.5 3 0.35 -0.5 18 -1 1,690 3.51 10LAU 811,159.6 8,222,650.4 ROCKCHIP CHANNEL 1.77 0.50 0.013 -0.20 1.2 2 -10 60 -0.5 2 0.15 -0.5 53 1 143 1.83 -10LAU 811,159.5 8,222,649.9 ROCKCHIP CHANNEL 2.09 0.40 0.125 0.30 0.5 12 -10 50 -0.5 62 0.07 -0.5 28 -1 164 11.20 10LAU 811,159.3 8,222,649.3 ROCKCHIP CHANNEL 3.01 0.70 0.229 -0.20 1.4 3 -10 70 -0.5 7 0.16 -0.5 50 -1 34 4.37 -10LAU 811,158.7 8,222,642.8 ROCKCHIP CHANNEL 1.55 0.05 0.269 0.40 1.0 3 -10 130 -0.5 19 0.10 -0.5 53 -1 60 13.40 10LAU 811,150.3 8,222,640.1 ROCKCHIP CHANNEL 1.90 0.30 -0.005 -0.20 0.4 3 -10 130 -0.5 -2 0.06 -0.5 11 2 95 1.72 -10FIO 811,028.0 8,222,811.0 ROCKCHIP CHANNEL 1.95 1.00 0.010 -0.20 1.8 -2 -10 50 -0.5 -2 0.21 -0.5 10 2 29 3.53 10FIO 811,027.0 8,222,810.0 ROCKCHIP CHANNEL 1.93 0.70 0.335 -0.20 0.5 3 -10 30 -0.5 466 0.05 -0.5 5 -1 163 11.40 10FIO 811,026.0 8,222,809.0 ROCKCHIP CHANNEL 1.73 0.80 0.005 -0.20 1.0 -2 -10 30 -0.5 2 0.14 -0.5 11 2 39 2.17 -10FIO 811,020.0 8,222,805.0 ROCKCHIP CHANNEL 1.35 0.05 9.770 0.20 0.6 -2 -10 20 -0.5 45 0.05 -0.5 5 -1 364 11.25 10FIO 811,011.2 8,222,794.3 ROCKCHIP CHANNEL 1.78 0.20 0.288 -0.20 0.6 -2 -10 20 -0.5 296 0.06 -0.5 4 -1 795 11.90 10FIO 810,986.3 8,222,875.4 ROCKCHIP CHANNEL 2.13 1.20 3.150 0.50 1.5 3 -10 10 -0.5 9 0.18 -0.5 8 -1 6,100 3.80 -10FIO 810,984.6 8,222,877.0 ROCKCHIP CHANNEL 2.72 1.00 0.015 -0.20 0.5 -2 -10 10 -0.5 -2 0.04 -0.5 5 2 283 1.10 -10FIO 810,984.6 8,222,873.8 ROCKCHIP CHANNEL 1.80 1.00 0.028 -0.20 1.3 -2 -10 20 -0.5 -2 0.11 -0.5 6 4 416 2.45 10FIO 810,947.8 8,222,860.0 ROCKCHIP CHANNEL 2.75 1.00 11.350 1.80 1.2 -2 -10 20 -0.5 6 0.10 -0.5 2 -1 10,850 4.72 -10FIO 810,893.0 8,222,881.0 ROCKCHIP CHANNEL 2.46 1.00 0.019 -0.20 2.4 -2 -10 70 -0.5 -2 0.17 -0.5 11 3 5,080 4.05 10 QC 0.06 0.331 1.00 1.9 11 -10 150 0.5 3 1.34 -0.5 12 41 3,450 4.69 10FIO 810,893.0 8,222,882.0 ROCKCHIP CHANNEL 2.03 0.50 0.044 0.20 1.8 -2 -10 50 -0.5 26 0.08 -0.5 2 6 5,240 5.53 10FIO 810,893.0 8,222,883.0 ROCKCHIP CHANNEL 1.40 1.00 0.064 0.20 3.0 3 -10 90 0.6 64 0.28 -0.5 16 29 4,700 6.10 10REG 805,996.0 8,224,549.0 ROCKCHIP CHANNEL 2.48 0.15 -0.050 1.20 0.1 2 10 70 -0.5 -2 0.03 -0.5 6 6 8,700 1.20 -10REG 806,411.0 8,224,257.0 ROCKCHIP CHANNEL 2.42 0.50 -0.050 0.30 1.2 -2 -10 40 -0.5 -2 0.05 -0.5 8 5 397 2.70 -10LOM 811,048.0 8,221,971.0 ROCKCHIP CHANNEL 2.77 0.60 20.500 1.00 0.3 16 10 60 -0.5 6 0.06 -0.5 9 1 772 10.20 -10LAB 811,539.0 8,222,439.5 ROCKCHIP CHANNEL 3.11 1.10 -0.050 -0.20 1.1 3 -10 50 -0.5 3 0.11 -0.5 63 1 1,080 3.85 10LAB 811,538.0 8,222,440.0 ROCKCHIP CHANNEL 2.75 0.65 -0.050 -0.20 0.3 -2 -10 70 -0.5 2 0.02 -0.5 24 24 125 1.10 -10LAB 811,539.0 8,222,441.5 ROCKCHIP CHANNEL 2.79 1.10 -0.050 0.20 2.3 -2 -10 280 -0.5 -2 0.33 -0.5 25 -1 615 4.65 10LAB 811,538.0 8,222,444.5 ROCKCHIP CHANNEL 2.58 1.00 -0.050 0.20 0.8 -2 -10 40 -0.5 -2 0.02 -0.5 7 8 287 2.30 -10LAB 811,540.0 8,222,443.5 ROCKCHIP CHANNEL 1.98 0.60 -0.050 -0.20 0.4 -2 -10 30 -0.5 -2 0.03 -0.5 16 5 387 1.84 -10LAB 811,541.0 8,222,444.0 ROCKCHIP CHANNEL 1.64 0.90 0.070 0.20 1.0 -2 -10 40 -0.5 -2 0.08 -0.5 31 6 294 2.51 -10LAB 811,541.5 8,222,445.0 ROCKCHIP CHANNEL 1.63 0.60 -0.050 -0.20 0.6 -2 -10 30 -0.5 -2 0.06 -0.5 11 6 158 1.57 -10LAB 811,542.0 8,222,446.0 ROCKCHIP CHANNEL 2.03 0.70 -0.050 -0.20 0.4 2 -10 20 -0.5 -2 0.05 -0.5 9 11 91 1.17 -10LAB 811,506.5 8,222,464.0 ROCKCHIP CHANNEL 2.70 0.95 -0.050 -0.20 1.5 -2 -10 30 -0.5 -2 0.16 -0.5 14 4 838 3.16 10LAB 811,507.0 8,222,465.0 ROCKCHIP CHANNEL 3.44 1.05 -0.050 0.20 0.8 4 -10 10 -0.5 2 0.02 -0.5 100 8 830 5.50 10 QC 0.06 2.900 5.00 1.21 5 -10 20 -0.5 7 1.4 -0.5 16 19 15,550 7.9 10LAB 811,507.0 8,222,466.0 ROCKCHIP CHANNEL 2.79 0.50 -0.050 -0.20 0.4 2 -10 10 -0.5 -2 0.05 -0.5 51 9 462 2.71 -10LAB 811,511.5 8,222,463.5 ROCKCHIP CHANNEL 3.55 0.60 0.070 0.50 0.9 8 -10 150 -0.5 -2 0.03 -0.5 59 4 4,520 4.44 -10LAB 811,512.0 8,222,464.0 ROCKCHIP CHANNEL 3.50 0.50 -0.050 -0.20 0.9 14 -10 30 -0.5 2 0.03 -0.5 146 6 1,330 5.73 -10LAB 811,512.0 8,222,465.0 ROCKCHIP CHANNEL 2.70 1.25 -0.050 -0.20 0.6 10 -10 20 -0.5 -2 0.03 -0.5 67 9 573 4.18 -10LAB 811,512.5 8,222,466.0 ROCKCHIP CHANNEL 2.56 0.80 -0.050 -0.20 0.5 -2 -10 30 -0.5 -2 0.05 -0.5 13 6 182 1.70 -10LAB 811,513.0 8,222,466.5 ROCKCHIP CHANNEL 3.43 1.30 -0.050 -0.20 2.0 -2 -10 40 -0.5 -2 0.14 -0.5 13 2 474 3.57 10LAB 811,513.5 8,222,467.5 ROCKCHIP CHANNEL 3.05 0.80 -0.050 -0.20 2.6 -2 -10 30 -0.5 2 0.19 -0.5 16 1 715 4.30 10

SampleID217930217931217932217933217934217935217936217937217938217939217940217941217942217943217944217945217946217947217948217949217950217951217952217953217954217955217956217957217958217959217960217961217962217963217964217965217966217967217968217969217970217971217972217973217974217975217976217977217978217979217980217981217982217983217984217985217986217987217988217989217990217991217992217993217994217995217996217997217998217999

Hg_ppm K_% La_ppm Mg_% Mn_ppm Mo_ppm Na_% Ni_ppm P_ppm Pb_ppm S_% Sb_ppm Sc_ppm Sr_ppm Th_ppm Ti_% Tl_ppm U_ppm V_ppm W_ppm Zn_ppm Au_ppm Au_ppm_Grav Cu_AA46-1 0.17 20 0.04 100 7 0.02 1 290 -2 0.02 -2 -1 6 -20 -0.01 -10 -10 4 -10 2 0.014-1 0.20 20 0.57 216 2 0.01 1 340 -2 0.02 -2 2 20 -20 -0.01 -10 -10 17 -10 14 0.023-1 0.13 10 0.10 373 13 -0.01 1 440 2 0.04 -2 1 10 -20 -0.01 -10 -10 14 -10 7 0.089-1 0.14 -10 0.05 1150 17 -0.01 2 110 -2 0.03 -2 1 9 -20 -0.01 -10 -10 3 -10 6 0.022-1 0.17 30 0.04 85 25 0.03 -1 290 3 0.13 -2 1 46 -20 -0.01 -10 -10 23 -10 2 0.031-1 0.13 30 0.06 29 2 0.01 2 120 -2 0.04 -2 2 41 -20 -0.01 -10 -10 15 -10 -2 -0.005-1 0.09 10 0.06 44 53 0.17 10 1510 40 0.56 -2 11 190 -20 0.07 -10 -10 130 -10 29 0.553-1 0.17 -10 0.06 33 19 0.02 8 850 17 0.19 -2 6 29 -20 0.01 -10 -10 119 -10 6 0.817-1 0.09 10 0.06 31 1 0.05 3 100 5 0.06 -2 2 32 -20 0.01 -10 -10 17 -10 3 0.055-1 0.08 20 0.84 156 2 0.05 3 610 5 0.06 -2 6 63 -20 0.05 -10 -10 91 -10 225 0.245-1 0.19 -10 0.05 33 37 0.01 6 1530 18 0.15 -2 1 22 -20 -0.01 -10 -10 99 -10 95 1.045-1 -0.01 -10 0.01 72 5 -0.01 4 10 -2 0.01 -2 -1 -1 -20 -0.01 -10 -10 1 -10 8 -0.005-1 0.20 10 0.64 197 9 0.01 19 1340 9 0.06 -2 8 18 20 -0.01 -10 -10 209 -10 55 0.354-1 0.04 20 2.12 1030 1 0.02 89 570 6 0.01 -2 14 37 -20 0.12 -10 -10 110 -10 101 0.069-1 0.17 10 0.11 51 15 0.02 5 330 19 0.12 -2 5 24 -20 0.03 -10 -10 66 -10 6 2.440-1 0.24 20 0.29 34 1 0.02 3 280 6 0.05 -2 7 65 -20 0.04 -10 -10 112 -10 6 0.122-1 0.09 10 0.11 20 12 0.06 5 540 12 0.15 -2 8 52 -20 0.04 -10 -10 140 -10 23 0.144-1 0.22 10 0.04 55 17 0.06 2 500 14 0.29 -2 2 45 -20 0.02 -10 -10 30 -10 4 0.666-1 0.23 -10 0.03 38 2 0.03 2 560 3 0.27 -2 1 23 -20 0.01 -10 -10 13 -10 2 0.744-1 0.12 -10 0.05 73 47 0.01 5 890 10 0.09 -2 2 22 -20 0.02 -10 -10 59 -10 8 1.270-1 0.13 10 0.11 284 -1 0.15 1 80 -2 0.01 -2 1 12 -20 0.03 -10 -10 6 -10 24 0.007-1 0.21 20 0.36 36 2 0.02 22 1240 7 0.13 -2 13 223 -20 0.06 -10 -10 152 -10 94 0.159-1 0.29 -10 0.04 26 12 0.04 1 250 18 0.38 -2 1 32 -20 -0.01 -10 -10 23 -10 7 2.240-1 0.34 -10 0.04 36 10 0.08 2 230 18 0.44 -2 1 46 -20 -0.01 -10 -10 26 -10 39 0.765-1 0.13 10 1.60 429 -1 0.02 15 430 3 0.02 -2 6 24 -20 0.04 -10 -10 75 -10 43 0.236-1 0.20 10 1.98 620 -1 0.02 14 410 2 0.01 -2 6 19 -20 0.02 -10 -10 82 -10 53 0.043-1 0.20 10 1.78 495 -1 0.03 10 410 2 0.01 -2 6 19 -20 0.01 -10 -10 77 -10 38 0.015-1 0.05 -10 0.78 348 2 -0.01 24 590 5 0.05 -2 4 13 -20 -0.01 -10 -10 61 -10 37 2.410-1 0.01 10 2.74 1175 -1 0.02 72 510 2 0.01 -2 15 9 -20 -0.01 -10 -10 82 -10 80 0.562 1.170-1 0.09 30 1.69 2040 2 0.02 40 730 2 0.01 -2 9 22 -20 -0.01 -10 -10 84 -10 72 0.039-1 0.15 10 1.28 579 1 0.04 8 560 2 0.01 -2 6 27 -20 -0.01 -10 -10 75 -10 43 0.017-1 0.07 20 0.38 378 1 0.03 2 160 2 0.01 -2 2 15 -20 -0.01 -10 -10 26 -10 14 0.013-1 0.11 10 0.06 37 26 0.06 1 480 10 0.20 -2 1 34 -20 -0.01 -10 -10 85 -10 3 0.125-1 0.09 10 0.59 266 7 0.04 2 290 3 0.02 -2 2 17 -20 -0.01 -10 -10 38 -10 17 0.229-1 0.12 10 0.26 86 9 0.01 3 480 -2 0.06 -2 1 12 -20 -0.01 -10 -10 43 -10 10 0.269-1 0.11 10 0.04 360 1 -0.01 2 140 -2 0.02 -2 1 9 -20 -0.01 -10 -10 16 -10 10 -0.005-1 0.12 40 0.58 122 1 0.03 4 300 -2 0.01 -2 4 32 -20 -0.01 -10 -10 30 -10 13 0.010-1 0.09 30 0.04 31 8 0.08 1 360 5 0.18 -2 1 21 -20 -0.01 -10 -10 50 -10 3 0.335-1 0.04 20 0.41 109 1 0.05 5 140 2 0.01 -2 2 12 -20 -0.01 -10 -10 14 -10 9 0.005-1 0.05 10 0.11 39 7 0.03 1 570 4 0.13 -2 3 41 -20 0.01 -10 -10 88 -10 4 9.770-1 0.07 10 0.10 33 6 0.02 2 560 3 0.06 -2 2 13 -20 -0.01 -10 -10 92 -10 3 0.288-1 0.05 20 1.07 342 1 0.03 5 590 2 0.01 -2 4 5 -20 0.04 -10 -10 32 -10 26 3.150-1 0.05 20 0.26 159 1 0.04 1 50 2 -0.01 -2 -1 5 -20 -0.01 -10 -10 5 -10 6 0.015-1 0.09 20 0.82 302 -1 0.04 2 260 2 0.01 -2 2 7 -20 -0.01 -10 -10 23 -10 19 0.028-1 0.12 30 0.67 211 1 0.04 5 630 2 0.01 -2 2 4 -20 -0.01 -10 -10 21 -10 12 >10.0 11.350 1.085-1 0.23 10 1.70 566 1 0.02 6 620 2 0.01 -2 4 13 -20 -0.01 -10 -10 53 -10 53 0.019-1 0.54 20 1.26 380 213 0.16 18 1000 10 0.48 2 6 89 -20 0.2 -10 -10 108 -10 63 0.331-1 0.11 10 1.01 184 1 0.01 11 600 2 0.02 -2 2 26 -20 -0.01 -10 -10 42 -10 21 0.044-1 0.16 20 2.25 690 2 0.02 19 860 4 0.01 -2 6 16 -20 -0.01 -10 -10 74 -10 57 0.0641 0.05 -10 0.04 282 3 0.01 1 60 2 0.01 -2 -1 5 -20 -0.01 -10 10 31 -10 6 -0.050

-1 0.05 -10 0.79 457 -1 0.02 2 130 3 -0.01 -2 1 9 -20 -0.01 -10 -10 34 60 47 -0.050-1 0.13 -10 0.04 48 15 0.01 -1 360 -2 0.04 -2 1 44 -20 -0.01 -10 -10 75 -10 4 20.500-1 0.07 10 0.48 226 2 0.04 1 360 -2 -0.01 -2 2 8 -20 -0.01 -10 -10 42 -10 14 -0.050-1 0.06 -10 0.13 117 1 -0.01 1 60 -2 -0.01 -2 -1 5 -20 -0.01 -10 -10 7 -10 7 -0.050-1 0.13 10 1.01 365 -1 0.03 2 390 -2 -0.01 -2 2 27 -20 -0.01 -10 -10 31 -10 30 -0.050-1 0.05 -10 0.38 144 2 -0.01 12 150 -2 -0.01 -2 1 3 -20 -0.01 -10 -10 13 -10 16 -0.050-1 0.04 -10 0.17 263 2 -0.01 1 40 -2 -0.01 2 1 4 -20 -0.01 -10 -10 9 -10 16 -0.050-1 0.04 -10 0.46 150 2 0.01 1 170 -2 -0.01 -2 1 6 -20 -0.01 -10 -10 17 -10 16 0.070-1 0.02 -10 0.28 114 -1 0.01 1 110 -2 -0.01 -2 1 5 -20 -0.01 -10 -10 12 -10 7 -0.050-1 0.03 -10 0.12 104 1 0.01 1 80 -2 -0.01 -2 1 4 -20 -0.01 -10 -10 11 -10 6 -0.050-1 0.03 -10 0.97 335 -1 0.01 2 170 3 -0.01 -2 2 15 -20 -0.01 -10 -10 25 -10 17 -0.050-1 -0.01 -10 0.56 221 2 -0.01 4 90 -2 0.01 -2 1 2 -20 -0.01 -10 -10 48 10 14 -0.050-1 0.15 10 1.06 357 3 0.06 21 820 25 1.6 2 5 77 -20 0.09 -10 -10 106 -10 111 2.900 1.555-1 0.01 -10 0.19 157 2 -0.01 1 50 -2 0.01 -2 1 5 -20 -0.01 -10 -10 15 -10 7 -0.050-1 0.02 -10 0.55 187 3 -0.01 3 180 -2 0.08 -2 2 5 -20 -0.01 -10 -10 52 -10 11 0.070-1 0.03 -10 0.56 210 6 -0.01 4 280 -2 0.03 -2 2 5 -20 -0.01 -10 -10 75 -10 11 -0.050-1 0.05 -10 0.32 158 3 -0.01 2 210 -2 -0.01 -2 1 4 -20 -0.01 -10 -10 48 -10 9 -0.050-1 0.04 -10 0.22 155 1 -0.01 1 100 -2 -0.01 -2 1 6 -20 -0.01 -10 -10 14 -10 12 -0.050-1 0.16 10 1.25 312 1 0.02 1 470 -2 -0.01 -2 3 7 -20 -0.01 -10 -10 35 -10 24 -0.050-1 0.13 10 1.60 447 -1 0.03 2 630 -2 -0.01 -2 5 9 -20 -0.01 -10 -10 65 -10 30 -0.050

SampleID218000218105218106218107218201218202218203218204218205218206218207218208218209218210218211218212218213218214218215218216218217218218218219218220218221218222218223218224218225218226218227218228218229218230218231218232218233218234218235218236218237218238218239218240218241218242218243218244218245218246218247218248218249218250218251218252218253218254218255218256218257218258218259218260218261218262218263218264218265218266

Prospect Easting Northing SampleType SampleSubTypeSampleWeight_KgMeshSize Au_ppm_mapinfo Ag_ppm Al_% As_ppm B_ppm Ba_ppm Be_ppm Bi_ppm Ca_% Cd_ppm Co_ppm Cr_ppm Cu_ppm Fe_% Ga_ppmREG 807,692.0 8,221,989.0 ROCKCHIP CHANNEL 1.86 0.20 0.100 0.40 0.1 -2 -10 10 -0.5 -2 0.01 -0.5 1 10 27 0.60 -10REG 814,477.0 8,222,998.0 ROCKCHIP CHIPS 1.66 2.00 -0.005 -0.20 1.1 -2 -10 30 -0.5 -2 0.24 -0.5 7 17 8 1.85 10REG 814,500.0 8,222,880.0 ROCKCHIP DUMP 2.34 0.20 8.830 4.80 0.43 11 -10 100 -0.5 32 0.05 -0.5 139 10 1,280 10.6 -10REG 813,052.0 8,223,039.0 ROCKCHIP FLOAT 1.84 0.40 0.030 -0.20 0.49 6 -10 100 -0.5 5 0.09 -0.5 113 60 47 13.2 10XIM 809,878.0 8,223,092.0 ROCKCHIP CHANNEL 1.34 0.1 0.180 0.50 0.13 7 10 40 -0.5 17 0.04 -0.5 12 28 269 7.31 -10LOM 810,976.0 8,222,209.0 ROCKCHIP CHANNEL 2.99 0.35 2.550 0.30 0.52 20 10 70 -0.5 4 0.08 -0.5 42 -1 1,065 7.68 -10LOM 810,976.5 8,222,209.0 ROCKCHIP CHANNEL 3.46 0.3 0.100 0.20 1.59 8 -10 40 -0.5 2 0.34 -0.5 21 -1 553 4.54 10LOM 810,956.0 8,222,218.0 ROCKCHIP CHANNEL 2.85 0.30 29.500 1.80 0.46 10 10 30 -0.5 7 0.06 -0.5 6 -1 2,330 8.48 -10LOM 810,872.0 8,222,219.0 ROCKCHIP CHANNEL 3.08 1.50 -0.050 -0.20 1.25 6 10 60 -0.5 -2 0.52 -0.5 96 -1 41 4.85 -10LOM 810,873.5 8,222,220.5 ROCKCHIP CHANNEL 3.34 1.50 -0.050 -0.20 1.06 2 -10 80 -0.5 -2 0.66 -0.5 111 1 55 3.39 -10LOM 810,874.0 8,222,230.0 ROCKCHIP CHANNEL 3.45 0.20 0.250 0.50 0.58 8 -10 70 -0.5 2 0.08 -0.5 67 -1 77 12.8 10LOM 810,895.5 8,222,247.0 ROCKCHIP CHANNEL 3.45 0.55 2.950 1.10 1.86 13 10 60 -0.5 7 0.36 -0.5 63 -1 4,660 8.19 -10LOM 810,896.0 8,222,247.0 ROCKCHIP CHANNEL 2.33 0.40 1.250 1.60 0.71 9 10 60 -0.5 2 0.1 -0.5 26 -1 3,740 5.62 -10LOM 810,896.0 8,222,247.5 ROCKCHIP CHANNEL 2.92 0.35 0.070 0.30 1.04 -2 -10 60 -0.5 3 0.34 -0.5 13 -1 4,760 1.87 -10LOM 810,896.5 8,222,248.0 ROCKCHIP CHANNEL 2.47 0.30 0.210 0.80 0.84 4 -10 70 -0.5 3 0.2 -0.5 41 -1 4,420 5.13 -10LOM 810,897.0 8,222,248.5 ROCKCHIP CHANNEL 3.02 0.40 -0.050 -0.20 1.65 -2 -10 70 -0.5 -2 0.68 -0.5 23 -1 1,360 2.57 -10LOM 810,891.0 8,222,304.0 ROCKCHIP CHANNEL 2.44 0.30 1.250 0.90 0.57 2 -10 60 -0.5 2 0.13 -0.5 10 -1 5,900 4.4 -10

QC 1.35 -0.050 -0.20 0.34 -2 -10 70 -0.5 -2 0.11 -0.5 2 2 29 0.77 -10LOM 810,821.0 8,222,324.0 ROCKCHIP CHANNEL 2.31 0.30 -0.050 -0.20 0.32 -2 -10 90 -0.5 -2 0.04 -0.5 4 2 14 4.5 -10LOM 810,821.5 8,222,325.0 ROCKCHIP CHANNEL 2.27 1.25 -0.050 0.20 0.44 5 10 90 -0.5 2 0.07 -0.5 8 -1 25 10 -10LOM 810,848.0 8,222,246.0 ROCKCHIP CHANNEL 2.41 0.40 0.140 -0.20 1.51 2 -10 60 -0.5 -2 0.18 -0.5 35 -1 1,665 3.45 -10LOM 810,848.0 8,222,277.0 ROCKCHIP CHANNEL 2.53 0.25 0.790 1.00 0.3 5 -10 100 -0.5 2 0.03 -0.5 23 3 1,630 5.13 -10LOM 810,849.0 8,222,277.0 ROCKCHIP CHANNEL 3.40 0.40 -0.050 -0.20 1.21 -2 -10 120 -0.5 -2 0.29 -0.5 17 -1 2,330 2.98 -10LOM 810,836.0 8,222,294.0 ROCKCHIP CHANNEL 4.15 0.40 0.360 0.70 1.32 20 10 180 -0.5 7 0.15 -0.5 286 -1 2,370 9.46 -10LOM 810,836.0 8,222,293.5 ROCKCHIP CHANNEL 3.67 0.60 3.080 1.10 1.04 10 -10 190 -0.5 4 0.22 -0.5 127 -1 2,540 9.9 -10LOM 810,823.0 8,222,290.0 ROCKCHIP CHANNEL 3.21 0.15 2.400 0.70 0.96 -2 -10 80 -0.5 -2 0.43 -0.5 15 -1 2,450 2.75 -10LOM 810,791.0 8,222,272.0 ROCKCHIP CHANNEL 2.79 0.40 -0.050 -0.20 1.89 -2 -10 40 -0.5 -2 0.68 -0.5 22 -1 464 2.65 -10LOM 810,791.0 8,222,272.5 ROCKCHIP CHANNEL 2.49 0.26 0.760 0.30 0.23 3 -10 120 -0.5 -2 0.1 -0.5 38 4 1,705 3.84 -10LOM 810,791.5 8,222,273.0 ROCKCHIP CHANNEL 3.41 0.45 -0.050 -0.20 1.4 -2 -10 70 -0.5 -2 0.73 -0.5 10 -1 1,055 1.73 -10LOM 810,999.0 8,221,953.5 ROCKCHIP CHANNEL 3.53 0.45 0.730 -0.20 0.48 -2 -10 30 -0.5 3 0.07 -0.5 7 4 412 0.95 -10LOM 811,076.5 8,221,946.0 ROCKCHIP CHANNEL 3.96 0.30 0.850 0.50 0.4 6 10 230 -0.5 2 0.08 -0.5 17 -1 10,150 9.11 -10LOM 811,077.0 8,221,947.0 ROCKCHIP CHANNEL 3.15 0.45 0.070 -0.20 0.7 -2 -10 70 -0.5 -2 0.42 -0.5 19 1 621 1.17 -10LOM 811,047.0 8,221,973.5 ROCKCHIP CHANNEL 2.49 0.35 12.650 1.10 1.43 37 20 650 0.9 11 0.21 -0.5 296 -1 3,800 10.25 -10 QC 0.09 0.400 1.00 1.88 12 10 160 0.5 2 1.41 -0.5 13 44 3,530 4.56 10LOM 811,047.0 8,221,973.0 ROCKCHIP CHANNEL 2.52 0.33 9.410 0.50 0.36 9 10 50 -0.5 4 0.06 -0.5 20 1 849 6.61 -10LOM 810,992.0 8,221,958.0 ROCKCHIP CHANNEL 3.13 0.20 5.590 0.70 1.88 4 10 20 -0.5 17 0.44 -0.5 16 -1 11,050 5.24 -10LOM 810,992.3 8,221,957.5 ROCKCHIP CHANNEL 2.80 0.45 0.140 -0.20 1.54 -2 -10 50 -0.5 -2 0.71 -0.5 14 6 1,530 2.25 -10LOM 810,900.5 8,222,074.0 ROCKCHIP CHANNEL 3.86 0.75 -0.050 -0.20 0.64 -2 -10 80 -0.5 -2 0.12 -0.5 20 2 714 2 -10LOM 810,886.0 8,222,078.0 ROCKCHIP CHANNEL 3.12 1.00 0.460 0.30 1.41 2 -10 110 -0.5 2 0.29 -0.5 28 3 1,795 2.87 -10LOM 810,886.0 8,222,077.0 ROCKCHIP CHANNEL 2.25 0.50 0.140 -0.20 1.27 -2 -10 60 -0.5 -2 0.41 -0.5 20 2 450 2.15 -10LOM 810,884.0 8,222,093.0 ROCKCHIP CHANNEL 3.39 0.65 10.900 3.20 0.53 2 -10 80 -0.5 3 0.11 -0.5 14 -1 5,140 2.22 -10LOM 810,732.0 8,222,317.0 ROCKCHIP CHANNEL 2.72 0.30 12.100 1.10 0.63 -2 -10 110 -0.5 -2 0.12 -0.5 9 -1 6,530 3.55 -10LOM 810,705.5 8,222,356.0 ROCKCHIP CHANNEL 3.08 0.30 0.280 -0.20 0.93 -2 -10 40 -0.5 -2 0.23 -0.5 7 -1 2,290 2.15 -10LOM 810,705.0 8,222,356.0 ROCKCHIP CHANNEL 3.48 0.30 0.400 0.30 0.37 -2 -10 40 -0.5 -2 0.05 -0.5 12 1 1,755 4.15 -10LOM 810,704.0 8,222,355.0 ROCKCHIP CHANNEL 2.76 0.45 0.160 -0.20 1.06 -2 -10 60 -0.5 -2 0.43 -0.5 11 -1 2,910 3.44 -10LOM 810,754.0 8,222,349.0 ROCKCHIP CHANNEL 1.52 0.15 0.670 0.20 0.23 4 -10 180 -0.5 -2 0.03 -0.5 46 5 1,295 6.45 -10 QC 1.26 -0.050 -0.20 0.29 -2 -10 60 -0.5 -2 0.09 -0.5 2 2 13 0.61 -10LOM 810,754.5 8,222,349.0 ROCKCHIP CHANNEL 2.39 0.55 -0.050 -0.20 1.49 -2 -10 40 -0.5 -2 0.74 -0.5 9 1 365 1.93 -10XIM 809,178.0 8,223,428.0 ROCKCHIP CHANNEL 2.91 0.50 0.070 -0.20 0.91 -2 -10 110 -0.5 -2 0.16 -0.5 22 30 731 2.48 -10XIM 809,178.0 8,223,429.0 ROCKCHIP CHANNEL 3.03 1.10 1.590 1.40 0.26 3 -10 50 -0.5 36 0.03 -0.5 1 6 698 5.99 -10XIM 809,178.5 8,223,430.0 ROCKCHIP CHANNEL 2.58 0.70 0.830 -0.20 0.62 -2 -10 50 -0.5 12 0.05 -0.5 4 3 576 2.15 -10FIO 809,493.5 8,223,859.0 ROCKCHIP CHANNEL 2.53 0.50 0.170 -0.20 1.06 2 -10 90 -0.5 -2 0.27 -0.5 50 1 102 2.64 -10FIO 809,494.0 8,223,859.0 ROCKCHIP CHANNEL 2.92 0.18 6.420 0.70 0.21 11 10 140 -0.5 5 0.03 -0.5 86 4 590 8.91 -10FIO 809,494.5 8,223,859.5 ROCKCHIP CHANNEL 2.61 0.50 -0.050 -0.20 2.01 -2 -10 80 -0.5 -2 0.41 -0.5 24 4 85 4.12 10FIO 809,474.0 8,223,905.0 ROCKCHIP CHANNEL 2.76 1.10 1.700 0.70 2.66 10 -10 100 -0.5 3 0.23 -0.5 3 12 615 8.25 10XIM 810,090.0 8,223,095.0 ROCKCHIP CHANNEL 3.88 1.35 0.110 1.00 4.34 -2 -10 130 -0.5 -2 0.4 -0.5 32 376 657 11.25 10XIM 809,615.0 8,223,299.0 ROCKCHIP CHANNEL 3.28 0.70 2.040 0.40 1.7 6 10 30 -0.5 7 0.18 -0.5 53 27 1,490 11.15 10XIM 809,615.0 8,223,298.0 ROCKCHIP CHANNEL 2.89 0.60 1.570 0.70 1.97 4 10 30 0.5 16 0.15 -0.5 119 11 5,000 18.9 10XIM 809,570.0 8,223,312.0 ROCKCHIP CHANNEL 3.05 0.80 0.630 0.50 1.92 3 10 40 -0.5 6 0.13 -0.5 66 60 2,970 12.05 10XIM 809,570.0 8,223,313.0 ROCKCHIP CHANNEL 3.20 0.70 5.390 1.20 0.58 7 10 20 -0.5 41 0.1 -0.5 96 -1 18,650 9.92 -10XIM 809,525.0 8,223,328.5 ROCKCHIP CHANNEL 2.86 0.80 2.200 0.60 0.48 7 10 60 0.5 25 0.13 -0.5 8 13 658 12.7 -10XIM 809,524.0 8,223,328.0 ROCKCHIP CHANNEL 3.33 1.00 0.410 -0.20 1.03 -2 -10 50 -0.5 2 0.16 -0.5 7 15 1,555 5.15 -10XIM 809,523.5 8,223,326.5 ROCKCHIP CHANNEL 4.04 1.60 0.430 0.30 1.02 2 -10 60 -0.5 11 0.16 -0.5 9 10 1,330 6.08 -10LAB 811,812.0 8,222,427.5 ROCKCHIP CHANNEL 2.98 0.65 0.070 0.30 1.83 -2 -10 10 -0.5 -2 0.13 -0.5 14 3 2,800 3.3 10LAB 811,812.0 8,222,428.5 ROCKCHIP CHANNEL 3.98 0.90 0.630 2.20 0.66 7 -10 30 -0.5 10 0.02 -0.5 22 -1 16,350 9.18 -10 QC 0.09 -0.050 -0.20 0.01 -2 10 10 -0.5 -2 -0.01 -0.5 2 24 22 0.55 -10LAB 811,812.0 8,222,429.3 ROCKCHIP CHANNEL 2.89 0.60 0.380 2.00 2.29 8 -10 170 -0.5 16 0.15 -0.5 27 18 11,250 6.38 10LAB 811,767.0 8,222,410.5 ROCKCHIP CHANNEL 2.53 0.80 0.070 0.20 2.15 2 -10 20 -0.5 -2 0.07 -0.5 14 -1 2,840 5.47 10LAB 811,767.0 8,222,411.2 ROCKCHIP CHANNEL 2.06 0.45 0.070 -0.20 0.8 4 -10 60 -0.5 -2 0.06 -0.5 8 3 1,020 2.72 -10LAB 811,766.5 8,222,412.0 ROCKCHIP CHANNEL 2.67 0.90 0.170 0.40 0.58 26 -10 60 -0.5 6 0.05 -0.5 16 2 2,250 6.59 -10

SampleID218000218105218106218107218201218202218203218204218205218206218207218208218209218210218211218212218213218214218215218216218217218218218219218220218221218222218223218224218225218226218227218228218229218230218231218232218233218234218235218236218237218238218239218240218241218242218243218244218245218246218247218248218249218250218251218252218253218254218255218256218257218258218259218260218261218262218263218264218265218266

Hg_ppm K_% La_ppm Mg_% Mn_ppm Mo_ppm Na_% Ni_ppm P_ppm Pb_ppm S_% Sb_ppm Sc_ppm Sr_ppm Th_ppm Ti_% Tl_ppm U_ppm V_ppm W_ppm Zn_ppm Au_ppm Au_ppm_Grav Cu_AA46-1 0.04 -10 0.03 100 -1 -0.01 -1 20 2 -0.01 -2 -1 3 -20 -0.01 -10 -10 4 -10 6 0.100-1 0.06 10 0.81 272 -1 0.06 10 470 -2 0.01 -2 2 9 -20 0.08 -10 -10 27 -10 21 -0.0051 0.07 -10 0.1 180 13 0.01 15 590 6 0.14 -2 1 15 -20 0.01 -10 -10 41 -10 8 8.830

-1 0.03 10 0.04 161 4 -0.01 16 1350 4 0.05 -2 2 11 -20 0.01 -10 -10 62 -10 16 0.030-1 0.06 10 0.03 55 1 0.03 5 300 30 0.13 -2 1 13 -20 0.01 -10 -10 132 -10 4 0.18-1 0.1 -10 0.11 47 68 0.02 -1 410 8 0.11 2 1 26 -20 -0.01 -10 -10 143 -10 3 2.55-1 0.17 -10 0.46 105 11 0.04 -1 480 3 0.06 -2 6 48 -20 0.06 -10 -10 129 -10 6 0.1-1 0.09 -10 0.05 54 123 0.01 -1 360 4 0.03 -2 2 11 -20 0.01 -10 -10 79 -10 -2 29.5-1 0.05 -10 0.52 265 3 0.03 2 220 -2 0.01 -2 2 39 -20 0.03 -10 -10 51 -10 6 -0.05-1 0.08 -10 0.31 185 2 0.03 2 300 -2 0.03 -2 1 41 -20 0.05 -10 -10 42 -10 6 -0.05-1 0.13 -10 0.06 44 40 0.03 -1 600 -2 0.16 5 2 39 -20 0.01 -10 -10 118 -10 4 0.251 0.13 10 0.4 224 30 0.03 -1 470 43 0.02 -2 6 40 -20 0.01 -10 -10 98 -10 10 2.95

-1 0.24 -10 0.17 132 27 0.02 -1 410 20 0.04 -2 1 25 -20 -0.01 -10 -10 84 -10 6 1.25-1 0.25 -10 0.22 106 1 0.02 1 520 -2 0.01 -2 1 20 -20 0.03 -10 -10 29 -10 5 0.07-1 0.2 -10 0.23 143 3 0.01 -1 380 -2 0.01 2 1 13 -20 0.01 -10 -10 59 -10 6 0.21-1 0.19 -10 0.89 332 1 0.02 1 640 -2 0.01 -2 2 35 -20 0.09 -10 -10 52 -10 12 -0.051 0.07 -10 0.04 51 1 0.01 -1 150 -2 0.03 -2 1 35 -20 0.01 -10 -10 42 -10 4 1.25

-1 0.15 10 0.11 327 -1 0.18 1 90 -2 0.01 -2 1 15 -20 0.03 -10 -10 7 -10 29 -0.05-1 0.13 -10 0.03 24 7 0.13 -1 210 3 0.32 -2 1 65 -20 0.01 -10 -10 35 -10 -2 -0.05-1 0.15 -10 0.05 19 17 0.11 -1 340 3 0.28 -2 2 73 -20 0.01 -10 -10 77 -10 6 -0.05-1 0.25 -10 0.8 524 1 0.02 1 550 -2 0.01 -2 2 8 -20 0.02 -10 -10 42 -10 19 0.14-1 0.17 -10 0.06 64 6 0.01 1 270 2 0.3 -2 1 23 -20 -0.01 -10 -10 42 -10 2 0.79-1 0.28 10 0.45 177 1 0.02 -1 450 -2 0.01 -2 2 51 -20 0.03 -10 -10 48 -10 11 -0.05-1 0.32 10 0.25 955 24 0.02 2 570 9 0.02 -2 3 18 -20 -0.01 -10 -10 153 -10 9 0.361 0.23 10 0.24 801 38 0.01 -1 500 -2 0.01 -2 3 17 -20 -0.01 -10 -10 114 -10 7 3.08

-1 0.31 -10 0.22 359 2 0.01 1 520 31 0.01 3 2 19 -20 0.03 -10 -10 45 -10 21 2.4-1 0.14 -10 1.34 309 -1 0.04 2 540 -2 0.01 -2 2 40 -20 0.08 -10 -10 49 -10 15 -0.05-1 0.04 -10 0.03 53 1 0.01 1 160 -2 0.23 -2 1 14 -20 0.01 -10 -10 35 -10 4 0.76-1 0.2 10 0.55 153 -1 0.02 1 470 -2 0.01 -2 3 37 -20 0.11 -10 -10 49 -10 7 -0.05-1 0.07 10 0.3 406 -1 0.03 1 100 9 0.01 -2 1 6 -20 -0.01 -10 -10 17 -10 6 0.731 0.12 -10 0.07 61 13 0.01 1 140 -2 0.05 -2 2 16 -20 0.01 -10 -10 89 50 3 0.85 1.015

-1 0.32 -10 0.12 97 2 0.01 1 520 -2 0.01 -2 1 24 -20 0.02 -10 -10 16 -10 3 0.07-1 0.11 10 0.34 10650 30 0.03 7 200 2 0.05 3 7 102 -20 0.01 -10 -10 117 -10 10 12.65-1 0.55 20 1.22 411 244 0.17 17 1080 8 0.5 -2 6 98 -20 0.21 -10 -10 115 -10 61 0.4-1 0.16 -10 0.05 83 12 0.02 1 280 -2 0.12 2 1 31 -20 -0.01 -10 -10 91 -10 -2 9.411 0.15 -10 1.36 375 2 0.03 -1 420 -2 -0.01 -2 2 28 -20 0.03 -10 -10 63 -10 16 5.59 1.105

-1 0.2 -10 1.01 162 1 0.02 1 560 -2 -0.01 -2 2 41 -20 0.08 -10 -10 56 -10 10 0.14-1 0.17 10 0.21 709 1 0.02 2 420 10 -0.01 -2 3 9 -20 -0.01 -10 -10 32 -10 13 -0.05-1 0.14 -10 0.98 384 2 0.01 1 360 4 0.02 2 2 24 -20 0.03 -10 -10 38 -10 19 0.46-1 0.2 -10 0.7 229 1 0.01 2 480 -2 0.01 -2 2 27 -20 0.05 -10 -10 31 -10 11 0.14-1 0.13 -10 0.23 314 5 0.01 -1 220 -2 0.02 -2 1 11 -20 -0.01 -10 -10 37 -10 11 10.9-1 0.25 -10 0.19 162 3 0.01 1 350 -2 0.01 -2 1 9 -20 -0.01 -10 -10 35 -10 11 12.1-1 0.2 -10 0.27 144 1 0.01 1 360 -2 -0.01 -2 1 20 -20 0.03 -10 -10 30 -10 6 0.28-1 0.19 -10 0.04 58 5 0.01 1 390 -2 0.02 -2 1 21 -20 0.01 -10 -10 25 -10 3 0.4-1 0.19 -10 0.43 271 1 0.02 1 530 -2 -0.01 -2 1 18 -20 0.04 -10 -10 31 -10 7 0.161 0.04 -10 0.05 51 1 0.02 2 300 -2 0.11 -2 1 11 -20 0.01 -10 -10 59 -10 2 0.67

-1 0.14 10 0.1 282 -1 0.19 1 90 -2 0.01 -2 1 12 -20 0.03 -10 -10 6 -10 27 -0.05-1 0.15 -10 0.85 250 -1 0.03 1 600 -2 -0.01 -2 2 40 -20 0.11 -10 -10 50 -10 11 -0.05-1 0.24 30 0.36 658 -1 0.03 19 320 -2 -0.01 -2 2 15 -20 -0.01 -10 -10 25 -10 41 0.07-1 0.18 -10 0.03 37 3 0.01 -1 80 2 0.02 -2 -1 18 -20 -0.01 -10 -10 47 -10 3 1.59-1 0.2 10 0.12 108 1 0.02 4 100 -2 -0.01 -2 1 14 -20 -0.01 -10 -10 15 -10 21 0.83-1 0.28 10 0.49 357 -1 0.01 7 490 3 -0.01 -2 2 12 -20 0.06 -10 -10 39 -10 14 0.17-1 0.07 -10 0.04 200 7 0.01 7 270 67 0.67 -2 1 8 -20 -0.01 -10 -10 100 -10 2 6.42-1 0.24 -10 1.26 600 -1 0.02 8 580 -2 -0.01 -2 3 26 -20 0.09 -10 -10 79 -10 25 -0.05-1 0.27 10 1.01 520 1 0.01 6 680 -2 0.03 2 4 30 -20 0.08 -10 -10 47 -10 60 1.71 0.02 -10 3.76 1075 1 0.01 96 740 -2 0.1 -2 11 20 -20 0.12 -10 -10 109 -10 101 0.11

-1 0.13 10 0.64 530 5 0.01 25 660 5 0.01 3 4 26 -20 0.04 -10 -10 76 -10 87 2.041 0.14 10 0.83 908 12 0.01 39 730 2 0.01 -2 5 26 -20 0.06 -10 -10 110 -10 96 1.57

-1 0.2 10 0.77 691 5 0.01 35 760 -2 0.01 -2 4 6 -20 0.03 -10 -10 87 -10 111 0.63-1 0.12 10 0.25 243 7 0.01 30 470 4 0.03 -2 1 10 -20 0.01 -10 -10 91 -10 32 5.39 1.8651 0.16 10 0.12 253 11 0.01 6 610 -2 0.02 2 2 54 -20 0.06 -10 -10 84 -10 20 2.2

-1 0.16 50 0.36 325 1 0.01 12 600 -2 -0.01 -2 3 56 -20 0.03 -10 -10 42 -10 49 0.41-1 0.12 20 0.34 445 2 0.01 10 490 -2 0.01 -2 3 43 -20 0.01 -10 -10 39 -10 43 0.43-1 0.09 -10 1.04 223 1 0.03 4 530 -2 -0.01 -2 4 4 -20 -0.01 -10 -10 48 -10 16 0.071 0.03 -10 0.34 98 5 0.01 2 320 -2 3.57 -2 1 3 -20 -0.01 -10 -10 37 -10 6 0.63 1.635

-1 0.01 -10 -0.01 74 5 -0.01 3 10 -2 -0.01 -2 -1 1 -20 -0.01 -10 -10 1 -10 9 -0.051 0.04 10 0.95 192 2 0.01 15 810 3 0.09 -2 4 20 -20 -0.01 -10 -10 78 -10 27 0.38 1.125

-1 0.07 10 1.22 139 1 0.01 4 330 -2 -0.01 -2 4 7 -20 -0.01 -10 -10 67 -10 33 0.07-1 0.03 -10 0.31 88 3 0.01 3 230 -2 0.02 2 1 11 -20 -0.01 -10 -10 35 -10 8 0.07-1 0.03 -10 0.22 66 13 0.01 -1 350 3 0.04 -2 1 8 -20 -0.01 -10 -10 50 -10 4 0.17

SampleID218267218268218269218270218271218272218273218274218275218276218277218278218282218283218284218285218286218287218288218289218290218291218292218293218294218295218296218297218298218299218300218301218302218303218304218305218306218307218308218309218310218311218312218313218314218315218316218317218318218319218320218321218322218323218324218325218401218402218403218404218405218406218407218408218409218410218411218412218413218414

Prospect Easting Northing SampleType SampleSubTypeSampleWeight_KgMeshSize Au_ppm_mapinfo Ag_ppm Al_% As_ppm B_ppm Ba_ppm Be_ppm Bi_ppm Ca_% Cd_ppm Co_ppm Cr_ppm Cu_ppm Fe_% Ga_ppmLAB 811,766.0 8,222,413.0 ROCKCHIP CHANNEL 2.78 0.80 -0.050 -0.20 2.4 2 -10 30 -0.5 2 0.19 -0.5 11 1 721 4.32 10LAB 811,745.0 8,222,405.0 ROCKCHIP CHANNEL 1.49 0.60 -0.050 -0.20 1.11 8 -10 30 -0.5 -2 0.09 -0.5 27 -1 680 4.03 -10LAB 811,744.7 8,222,406.0 ROCKCHIP CHANNEL 3.95 1.10 0.140 1.00 0.55 12 -10 70 -0.5 3 0.02 -0.5 12 3 1,280 4.19 -10LAB 811,744.0 8,222,406.5 ROCKCHIP CHANNEL 3.01 1.00 -0.050 -0.20 2.71 2 -10 30 -0.5 2 0.16 -0.5 25 1 548 5.34 10LAB 811,823.0 8,222,426.0 ROCKCHIP CHANNEL 2.46 0.90 0.190 0.60 1.62 12 10 20 -0.5 15 0.04 -0.5 45 1 17,300 7.19 10LAB 811,822.5 8,222,425.0 ROCKCHIP CHANNEL 3.55 0.50 0.400 0.70 1.32 30 -10 20 -0.5 6 0.04 -0.5 49 9 1,600 7.33 -10LAB 811,822.0 8,222,424.0 ROCKCHIP CHANNEL 2.71 1.30 0.070 -0.20 1.91 3 -10 10 -0.5 3 0.08 -0.5 14 21 1,040 3.74 10LAB 811,822.0 8,222,423.0 ROCKCHIP CHANNEL 2.99 1.20 0.070 -0.20 1.65 14 -10 20 -0.5 2 0.13 -0.5 13 16 1,250 3.45 10LAB 811,745.0 8,222,406.0 ROCKCHIP CHANNEL 3.11 1.30 0.100 1.30 0.22 16 -10 130 -0.5 3 0.04 -0.5 5 3 938 3.6 -10LAB 811,698.0 8,222,389.0 ROCKCHIP CHANNEL 2.77 1.55 0.440 1.90 0.17 64 -10 150 -0.5 6 0.03 -0.5 6 3 1,010 5.68 -10LAB 811,697.5 8,222,390.0 ROCKCHIP CHANNEL 3.37 0.80 -0.050 0.20 1.3 6 -10 20 -0.5 3 0.05 -0.5 10 -1 2,150 3.23 -10REG 810,737.0 8,224,618.0 ROCKCHIP CHANNEL 3.48 0.50 0.411 0.40 0.44 122 -10 140 -0.5 5 0.04 -0.5 77 10 70 10.25 -10LAB 811,312.0 8,222,528.0 ROCKCHIP CHANNEL 3.60 1.10 -0.050 -0.20 0.73 4 -10 40 -0.5 2 0.11 -0.5 6 3 38 1.84 -10LAB 811,313.0 8,222,530.0 ROCKCHIP CHANNEL 3.87 1.90 -0.050 -0.20 0.8 2 -10 40 -0.5 2 0.06 -0.5 26 3 104 2.43 -10LOM 811,138.5 8,222,255.0 ROCKCHIP CHANNEL 3.10 0.18 3.170 -0.20 0.41 4 -10 150 -0.5 3 0.09 -0.5 19 2 1,810 2.66 -10

QC 0.09 2.990 4.70 1.16 7 -10 20 -0.5 23 1.3 -0.5 14 7 15,000 7.28 10LOM 811,129.0 8,222,309.0 ROCKCHIP CHANNEL 2.81 0.45 -0.050 -0.20 3.22 -2 -10 30 -0.5 2 0.13 -0.5 15 -1 544 5.19 10LOM 811,128.5 8,222,308.0 ROCKCHIP CHANNEL 3.96 0.50 0.670 -0.20 1.35 9 -10 30 -0.5 10 0.3 -0.5 18 -1 7,330 4.29 -10LOM 811,128.0 8,222,307.5 ROCKCHIP CHANNEL 2.71 0.60 -0.050 -0.20 2.01 3 -10 20 -0.5 -2 0.38 -0.5 14 -1 2,240 2.95 -10LOM 811,099.0 8,222,328.0 ROCKCHIP CHANNEL 2.76 0.26 8.120 5.00 1.27 9 10 140 -0.5 22 0.11 -0.5 3 -1 27,600 5.9 -10LOM 811,098.0 8,222,327.5 ROCKCHIP CHANNEL 2.03 0.80 -0.050 -0.20 1.56 3 -10 40 -0.5 2 0.29 -0.5 9 2 121 2.31 -10LOM 811,065.5 8,222,358.0 ROCKCHIP CHANNEL 2.66 0.25 7.220 0.50 0.51 4 -10 70 -0.5 6 0.14 -0.5 2 -1 11,050 2.66 -10REG 810,353.0 8,223,743.0 ROCKCHIP CHANNEL 1.67 2.00 0.140 -0.20 0.05 -2 -10 10 -0.5 -2 0.01 -0.5 2 7 87 0.74 -10REG 810,355.0 8,223,742.0 ROCKCHIP CHANNEL 2.73 2.00 -0.050 -0.20 0.04 3 -10 20 -0.5 -2 0.03 -0.5 10 12 31 2.03 -10REG 810,717.0 8,223,370.0 SOIL -80# 3.96 2.520 0.70 2.19 16 -10 110 0.6 4 0.59 -0.5 20 30 1,230 5.33 10REG 810,693.0 8,223,372.0 SOIL -80# 4.38 0.009 -0.20 1.77 8 -10 210 0.6 -2 0.31 -0.5 16 34 55 3.32 10REG 810,701.0 8,223,346.0 SOIL -80# 3.02 0.049 -0.20 2.17 13 -10 200 0.6 2 0.52 -0.5 18 29 78 4.48 10REG 810,727.0 8,223,349.0 SOIL -80# 4.48 0.007 -0.20 2.13 8 -10 190 0.6 2 0.51 -0.5 16 44 80 3.72 10REG 810,732.0 8,223,326.0 SOIL -80# 3.45 0.006 -0.20 1.54 6 -10 150 -0.5 -2 0.41 -0.5 19 38 48 3.48 10XIM 809,317.0 8,223,410.0 ROCKCHIP CHANNEL 3.98 0.55 1.330 1.80 0.42 18 10 70 -0.5 135 0.06 -0.5 36 7 893 17.2 10XIM 809,318.0 8,223,410.0 ROCKCHIP CHANNEL 3.96 0.80 0.070 -0.20 0.72 3 -10 70 -0.5 4 0.12 -0.5 8 17 899 5.51 -10XIM Ximnena 1 ROCKCHIP UNDERGROUND 3.71 0.60 13.900 9.1 0.77 -2 -10 30 -0.5 6 0.03 -0.5 22 12 1650 12.05 10XIM Ximnena 1 ROCKCHIP UNDERGROUND 2.94 0.30 12.250 5 1.23 -2 -10 40 -0.5 -2 0.08 -0.5 53 7 27700 14.5 10XIM Ximnena 1 ROCKCHIP UNDERGROUND 4.16 0.20 1.410 8.1 2.05 3 -10 -10 -0.5 13 0.05 -0.5 306 -1 60600 24.8 20XIM Ximnena 1 ROCKCHIP UNDERGROUND 5.53 0.40 0.590 5.1 2.61 -2 -10 20 -0.5 28 0.19 -0.5 71 199 48400 12.05 20XIM Ximnena 1 ROCKCHIP UNDERGROUND 2.33 0.35 34.100 6.4 1.99 3 -10 70 -0.5 29 0.12 -0.5 35 28 5830 15.5 10XIM Ximnena 1 ROCKCHIP UNDERGROUND 2.75 0.20 30.500 11.2 0.7 4 -10 20 -0.5 21 0.03 -0.5 19 9 3620 17.7 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.87 1.00 2.270 4.2 0.35 3 -10 -10 -0.5 5 0.04 -0.5 28 -1 26700 10.3 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.85 0.95 4.230 8.8 0.27 3 -10 -10 -0.5 3 0.03 -0.5 36 -1 44800 15.2 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 3.19 0.20 15.500 14.1 0.21 7 -10 -10 -0.5 2 0.02 -0.5 30 -1 64100 23.7 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 5.62 0.90 13.650 10.9 0.73 -2 -10 -10 -0.5 -2 0.03 -0.5 66 -1 79400 22.1 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.32 0.40 0.330 1.2 2.31 82 10 30 -0.5 -2 0.15 -0.5 27 -1 9280 6.22 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.28 0.80 9.900 12.3 0.84 17 10 -10 -0.5 -2 0.03 -0.5 79 -1 74400 17.6 10

QC 1.38 -0.050 -0.2 0.35 -2 10 70 -0.5 -2 0.1 -0.5 2 2 230 0.84 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.72 0.48 17.350 21.8 0.37 -2 10 -10 -0.5 -2 -0.01 -0.5 -1 -1 236000 16.2 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.88 0.70 7.100 11.3 0.67 -2 10 -10 -0.5 -2 0.02 -0.5 83 -1 126500 9.54 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.36 0.50 5.020 6.7 0.95 -2 -10 -10 -0.5 13 0.02 -0.5 190 -1 69300 10.3 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.45 0.55 1.750 5.7 0.49 2 -10 -10 -0.5 8 0.02 -0.5 36 -1 62900 10.85 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.08 0.60 0.130 3.2 1.91 -2 -10 -10 -0.5 2 0.16 -0.5 52 -1 16750 7.3 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.26 1.00 5.780 10.8 0.42 -2 10 -10 -0.5 6 0.02 -0.5 65 -1 124500 10.45 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 3.46 0.20 4.810 5.4 0.24 6 -10 -10 -0.5 5 0.02 -0.5 9 -1 7850 9.89 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 4.43 0.90 10.050 6.1 0.34 -2 -10 -10 -0.5 -2 0.03 -0.5 76 -1 68300 8.57 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 3.42 0.70 4.570 8.1 0.53 -2 -10 -10 -0.5 -2 0.05 -0.5 37 -1 63600 10.4 -10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 5.15 0.90 2.780 8.9 0.6 -2 -10 -10 -0.5 19 0.06 -0.5 65 -1 47100 10.7 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 3.26 1.00 1.090 15.2 0.7 -2 -10 -10 -0.5 5 0.02 -0.5 32 -1 42400 14.4 10XIM Ximena 2 y 3 ROCKCHIP UNDERGROUND 3.82 0.75 7.440 8.2 0.67 -2 10 -10 -0.5 12 0.36 -0.5 142 -1 64300 8.98 -10STA 811,251.0 8,223,252.0 ROCKCHIP CHIPS 2.96 5.00 0.012 -0.2 0.38 -2 -10 340 -0.5 -2 0.06 -0.5 2 6 362 2.12 -10STA 811,272.0 8,223,181.0 ROCKCHIP CHIPS 1.82 5.00 0.011 -0.2 0.42 -2 -10 140 -0.5 -2 0.07 -0.5 1 10 314 3.44 10STA 811,261.0 8,223,129.0 ROCKCHIP CHIPS 2.28 5.00 0.005 -0.2 0.53 -2 -10 100 -0.5 -2 0.05 -0.5 1 7 131 2.16 -10STA 811,262.0 8,223,039.0 ROCKCHIP CHIPS 2.57 5.00 0.009 0.2 0.73 -2 -10 80 -0.5 -2 0.25 -0.5 4 19 284 5.4 10STA 811,216.0 8,223,320.0 ROCKCHIP CHIPS 2.6 5.00 0.005 -0.2 0.45 -2 -10 190 -0.5 -2 0.05 -0.5 1 4 157 1.37 -10STA 811,215.0 8,223,354.0 ROCKCHIP CHIPS 2.66 5.00 0.007 -0.2 0.42 -2 -10 240 -0.5 -2 0.04 -0.5 1 4 205 2.35 -10STA 811,228.0 8,223,407.0 ROCKCHIP CHIPS 2.94 5.00 -0.005 -0.2 0.36 -2 -10 160 -0.5 -2 0.03 -0.5 1 4 148 1.26 -10REG 810,737.0 8,223,278.0 SOIL -80# 4.57 5.00 0.007 -0.2 2.25 6 -10 240 0.8 -2 0.52 -0.5 15 42 53 3.76 10REG 810,700.0 8,223,287.0 SOIL -80# 4.54 5.00 0.005 -0.2 1.53 3 -10 170 0.5 2 0.4 -0.5 14 35 51 3.47 10REG 810,673.0 8,223,295.0 SOIL -80# 4.28 5.00 -0.005 -0.2 1.32 5 -10 180 -0.5 -2 0.43 -0.5 13 34 46 3.41 10REG 810,672.0 8,223,260.0 SOIL -80# 4.9 5.00 -0.005 -0.2 2.06 5 10 190 0.7 -2 0.43 -0.5 16 41 56 4.08 10REG 810,793.0 8,223,316.0 SOIL -80# 4.06 5.00 0.029 -0.2 1.76 6 -10 170 0.5 3 0.51 -0.5 17 41 62 3.97 10REG 810,808.0 8,223,378.0 SOIL -80# 4.41 3.00 -0.005 -0.2 1.4 3 -10 180 -0.5 -2 0.5 -0.5 12 29 45 2.77 10REG 810,780.0 8,223,335.0 SOIL -80# 4.66 5.00 -0.005 -0.2 2.18 7 -10 180 0.6 -2 0.42 -0.5 19 45 46 4.11 10

SampleID218267218268218269218270218271218272218273218274218275218276218277218278218282218283218284218285218286218287218288218289218290218291218292218293218294218295218296218297218298218299218300218301218302218303218304218305218306218307218308218309218310218311218312218313218314218315218316218317218318218319218320218321218322218323218324218325218401218402218403218404218405218406218407218408218409218410218411218412218413218414

Hg_ppm K_% La_ppm Mg_% Mn_ppm Mo_ppm Na_% Ni_ppm P_ppm Pb_ppm S_% Sb_ppm Sc_ppm Sr_ppm Th_ppm Ti_% Tl_ppm U_ppm V_ppm W_ppm Zn_ppm Au_ppm Au_ppm_Grav Cu_AA46-1 0.03 50 1.42 230 -1 0.03 5 730 -2 0.01 -2 3 9 -20 -0.01 -10 -10 41 -10 17 -0.05-1 0.12 10 0.4 141 2 0.01 -1 390 3 0.01 -2 2 9 -20 -0.01 -10 -10 38 -10 23 -0.05-1 0.04 -10 0.2 57 6 -0.01 -1 310 -2 0.03 -2 1 6 -20 -0.01 -10 -10 46 -10 5 0.14-1 0.04 10 1.69 237 -1 0.01 1 560 -2 0.01 -2 3 12 -20 -0.01 -10 -10 54 -10 26 -0.05-1 0.02 -10 0.98 286 17 -0.01 6 360 -2 0.08 -2 3 4 -20 0.01 -10 -10 64 10 16 0.19 1.73-1 0.02 -10 0.76 240 20 -0.01 1 510 -2 0.42 -2 2 1 -20 -0.01 -10 -10 50 40 12 0.4-1 0.06 10 1.05 261 1 0.01 5 440 -2 0.01 -2 3 2 -20 -0.01 -10 -10 37 -10 15 0.07-1 0.07 30 1 247 2 0.03 4 640 -2 0.04 -2 3 3 -20 -0.01 -10 -10 43 10 10 0.07-1 0.03 -10 0.03 38 4 0.01 5 280 2 0.05 -2 1 10 -20 -0.01 -10 -10 48 -10 -2 0.1-1 0.05 -10 0.02 49 62 0.01 -1 290 3 0.08 4 1 13 -20 -0.01 -10 -10 49 -10 3 0.44-1 0.03 -10 0.64 96 1 0.01 2 200 -2 0.01 -2 2 7 -20 -0.01 -10 -10 51 -10 9 -0.05-1 0.06 10 0.04 39 5 0.05 3 690 85 0.32 -2 3 42 -20 0.01 -10 -10 171 -10 16 0.411-1 0.04 -10 0.29 217 1 0.02 -1 250 -2 0.01 -2 1 5 -20 -0.01 -10 -10 21 -10 11 -0.05-1 0.08 -10 0.38 144 6 0.03 1 280 -2 0.49 -2 1 6 -20 -0.01 -10 -10 21 -10 6 -0.05-1 0.13 -10 0.14 611 2 -0.01 2 210 3 0.15 -2 1 9 -20 -0.01 -10 -10 25 -10 3 3.17-1 0.14 10 1.03 333 2 0.06 16 740 25 1.45 -2 5 66 -20 0.09 -10 -10 98 -10 99 2.99 1.5-1 0.21 10 2.68 743 -1 -0.01 -1 410 2 0.01 -2 2 5 -20 -0.01 -10 -10 40 -10 33 -0.05-1 0.13 -10 0.74 312 1 0.01 -1 410 6 0.01 -2 1 22 -20 0.01 -10 -10 76 -10 15 0.67-1 0.1 -10 1.29 511 -1 0.02 -1 470 2 0.01 -2 3 24 -20 0.06 -10 -10 39 -10 26 -0.05-1 0.11 -10 0.88 371 1 0.01 -1 370 4 0.04 -2 2 11 -20 -0.01 -10 -10 93 -10 20 8.12 2.76-1 0.19 10 0.92 285 -1 0.02 3 450 -2 0.01 -2 1 20 -20 -0.01 -10 -10 17 -10 14 -0.05-1 0.22 -10 0.13 276 7 -0.01 -1 400 -2 0.07 -2 1 7 -20 0.01 -10 -10 35 -10 2 7.22 1.105-1 0.01 -10 0.01 49 1 0.01 1 30 -2 0.02 -2 -1 2 -20 -0.01 -10 -10 6 -10 -2 0.14-1 0.01 -10 0.01 52 1 -0.01 8 60 -2 0.07 -2 -1 5 -20 -0.01 -10 -10 22 -10 -2 -0.05

33.5 0.11 20 1.13 897 2 0.03 22 930 16 0.05 -2 8 61 -20 0.06 -10 -10 102 -10 67 2.5200.09 0.3 10 0.45 685 1 0.02 17 830 9 0.03 -2 5 53 -20 0.17 -10 -10 95 -10 46 0.0090.18 0.2 30 0.82 796 1 0.02 21 920 7 0.02 -2 8 58 -20 0.11 -10 -10 113 -10 44 0.0490.17 0.28 10 0.76 856 1 0.03 30 950 7 0.03 -2 6 60 -20 0.16 -10 -10 95 -10 60 0.0070.06 0.23 10 0.62 531 1 0.02 21 910 7 0.02 -2 4 45 -20 0.13 -10 -10 93 -10 45 0.006

-1 0.06 10 0.06 177 5 0.01 3 480 3 0.06 -2 2 17 -20 0.01 -10 -10 100 -10 9 1.33-1 0.21 10 0.13 92 -1 0.01 4 440 -2 0.05 -2 2 76 -20 0.01 -10 -10 52 -10 15 0.071 0.1 -10 0.25 95 4 0.02 11 750 6 2.36 6 2 11 -20 -0.01 -10 -10 45 -10 6 13.91 0.14 10 0.4 174 4 0.02 14 740 5 4.73 5 2 10 -20 -0.01 -10 -10 33 -10 15 12.25 2.77

-1 0.01 -10 1.25 368 2 0.01 69 30 5 >10.0 7 3 4 -20 0.01 -10 -10 52 -10 38 1.41 6.061 0.09 -10 1.84 512 2 0.02 29 420 3 6 5 7 15 -20 0.02 -10 -10 90 -10 42 0.59 4.841 0.05 10 0.4 683 7 0.03 23 1670 5 0.13 3 5 47 -20 0.02 -10 -10 48 -10 21 34.11 0.08 10 0.07 39 15 0.02 7 1380 2 0.13 7 2 27 -20 0.01 -10 -10 38 -10 8 30.51 0.04 -10 0.18 67 1 0.01 20 50 3 6.8 5 1 -1 -20 -0.01 -10 -10 34 10 7 2.27 2.671 0.01 10 0.07 74 -1 0.01 16 50 2 >10.0 -2 1 -1 -20 -0.01 -10 -10 31 10 10 4.23 4.48

-1 0.02 -10 0.06 61 -1 0.01 14 20 4 >10.0 4 -1 -1 -20 -0.01 -10 -10 21 10 15 15.5 6.411 0.07 -10 0.2 103 1 0.01 34 100 3 >10.0 9 1 -1 -20 -0.01 -10 -10 15 -10 16 13.65 7.94

-1 0.32 10 1.14 419 1 0.01 17 540 2 1.82 -2 4 3 -20 -0.01 -10 -10 63 -10 41 0.331 0.04 -10 0.21 83 1 0.01 31 50 8 >10.0 7 1 -1 -20 -0.01 -10 -10 16 -10 14 9.9 7.44

-1 0.16 10 0.1 340 -1 0.21 2 90 3 0.05 -2 1 16 -20 0.03 -10 -10 7 -10 26 -0.051 0.02 -10 0.11 82 1 0.01 8 10 6 6.8 8 -1 -1 -20 -0.01 -10 -10 3 10 19 17.35 23.61 0.04 -10 0.3 153 2 0.01 13 20 4 7.4 4 1 6 -20 0.01 -10 -10 18 10 14 7.1 12.651 0.07 -10 0.37 222 2 0.01 22 30 6 >10.0 5 1 2 -20 0.01 -10 -10 19 -10 20 5.02 6.93

-1 0.03 -10 0.27 128 1 0.01 17 40 3 >10.0 4 1 -1 -20 0.01 -10 -10 17 10 12 1.75 6.291 0.08 -10 1.29 384 3 0.02 22 350 3 3.41 2 4 3 -20 0.03 -10 -10 50 -10 35 0.13 1.6751 0.04 -10 0.19 151 3 0.01 20 120 3 4.84 2 1 1 -20 0.01 -10 -10 16 10 14 5.78 12.451 0.01 -10 0.02 42 10 0.01 4 530 12 1.05 5 2 6 -20 -0.01 -10 -10 24 -10 6 4.81

-1 0.05 -10 0.11 91 2 0.01 15 60 5 8.7 5 -1 3 -20 -0.01 -10 -10 8 -10 8 10.05 6.831 -0.01 -10 0.2 122 2 0.01 12 100 5 5.22 -2 1 2 -20 0.01 -10 -10 19 10 11 4.57 6.361 0.01 -10 0.26 203 1 0.01 35 110 3 9 4 1 5 -20 0.01 -10 -10 15 10 15 2.78 4.711 0.01 -10 0.1 91 3 0.01 16 180 5 3.31 5 1 2 -20 0.01 -10 -10 20 10 9 1.09 4.241 0.03 -10 0.31 185 2 0.01 30 50 3 8.1 2 1 7 -20 0.01 -10 -10 13 -10 13 7.44 6.43

-1 0.26 10 0.05 63 80 0.07 2 220 3 0.29 -2 1 54 -20 0.01 -10 -10 9 -10 2 0.012-1 0.2 10 0.03 63 9 0.05 1 360 -2 0.21 -2 -1 63 -20 -0.01 -10 -10 10 -10 2 0.011-1 0.23 10 0.1 59 17 0.06 2 150 3 0.19 -2 1 39 -20 0.01 -10 -10 13 -10 3 0.005-1 0.28 50 0.19 113 5 0.06 14 590 5 0.35 -2 4 118 40 0.06 -10 -10 78 -10 10 0.009-1 0.18 30 0.04 27 6 0.05 2 170 4 0.09 -2 1 45 -20 0.01 -10 -10 5 -10 2 0.005-1 0.2 10 0.04 38 13 0.03 2 170 3 0.05 -2 1 25 -20 0.01 -10 -10 14 -10 2 0.007-1 0.16 10 0.03 42 34 0.04 1 100 2 0.01 -2 1 17 -20 -0.01 -10 -10 3 -10 -2 -0.005

0.03 0.49 20 0.72 851 1 0.02 25 1360 9 0.03 -2 7 80 -20 0.17 -10 -10 93 -10 580.02 0.34 10 0.43 525 1 0.01 18 1180 8 0.03 -2 3 52 -20 0.18 -10 -10 105 -10 530.02 0.38 10 0.46 454 1 0.01 18 1360 7 0.03 -2 3 51 -20 0.17 -10 -10 104 -10 560.03 0.38 10 0.53 608 1 0.01 20 1190 9 0.03 -2 5 59 -20 0.18 -10 -10 118 -10 55

0.3 0.28 10 0.69 561 1 0.02 22 1020 8 0.02 -2 5 54 -20 0.18 -10 -10 112 -10 520.03 0.28 10 0.65 472 -1 0.02 21 1010 6 0.01 -2 4 48 -20 0.16 -10 -10 79 -10 500.05 0.31 10 0.7 774 1 0.02 27 840 7 0.02 -2 6 54 -20 0.18 -10 -10 109 -10 55

SampleID218415218416218417218418218419218420218421218422218423218424218425218426218427218428218429218430218431218432218433218434218435218436218437218438218439218440218441218442218443218444218445218446218447218448218449218450218451218452218453218454218455218456218457218458218459218460218461218462218463218464218465218466218467218468218469218470218471218472218473218474218475218476218477218478218479218480218481218482218483218484

Prospect Easting Northing SampleType SampleSubTypeSampleWeight_KgMeshSize Au_ppm_mapinfo Ag_ppm Al_% As_ppm B_ppm Ba_ppm Be_ppm Bi_ppm Ca_% Cd_ppm Co_ppm Cr_ppm Cu_ppm Fe_% Ga_ppmREG 810,762.0 8,223,363.0 SOIL -80# 5.09 5.00 -0.005 -0.2 1.78 6 -10 190 0.5 -2 0.48 -0.5 13 39 45 3.29 10REG 810,727.0 8,223,332.0 ROCKCHIP CHANNEL 2.21 2.00 0.132 -0.2 0.2 6 -10 80 -0.5 9 0.05 -0.5 35 10 144 4.9 -10REG 810,703.0 8,223,336.0 ROCKCHIP CHANNEL 2.85 2.20 0.084 -0.2 0.66 22 -10 20 -0.5 6 0.07 -0.5 45 28 95 7.83 10REG 810,975.0 8,224,977.0 ROCKCHIP CHANNEL 3.3 0.50 0.075 -0.2 0.11 38 -10 220 -0.5 -2 0.02 -0.5 212 9 36 4.56 -10STA 811,217.0 8,222,754.0 ROCKCHIP CHIPS 4.00 0.013 -0.2 0.88 4 10 70 -0.5 2 0.12 -0.5 6 1 94 6.6 10STA 811,195.0 8,222,815.0 ROCKCHIP CHIPS 0.25 0.031 -0.2 0.48 3 10 60 -0.5 5 0.12 -0.5 6 27 236 11.8 10

QC 0.006 -0.2 0.01 -2 -10 10 -0.5 -2 -0.01 -0.5 1 23 8 0.55 -10STA 811,204.0 8,222,932.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.81 -2 -10 50 -0.5 -2 0.48 -0.5 7 21 102 2.33 -10STA 811,059.0 8,223,178.0 ROCKCHIP CHIPS 5.00 0.007 -0.2 1.02 -2 -10 90 -0.5 2 0.51 -0.5 7 43 69 2.01 -10STA 811,036.0 8,223,378.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 1.45 -2 -10 60 -0.5 -2 0.08 -0.5 2 44 131 3.88 -10STA 811,042.0 8,223,380.0 ROCKCHIP CHIPS 6.00 -0.005 -0.2 1.69 -2 -10 110 -0.5 -2 0.28 -0.5 3 2 101 3.23 10STA 811,056.0 8,223,394.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.45 -2 -10 80 -0.5 -2 0.04 -0.5 1 14 45 1.88 -10STA 811,105.0 8,223,399.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.38 -2 -10 170 -0.5 -2 0.04 -0.5 1 6 52 1.25 -10STA 811,114.0 8,223,295.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.42 -2 -10 170 -0.5 -2 0.04 -0.5 1 3 44 1.29 -10STA 811,098.0 8,223,250.0 ROCKCHIP CHIPS 4.00 -0.005 -0.2 0.49 -2 -10 40 -0.5 -2 0.06 -0.5 1 7 32 1.35 -10STA 811,110.0 8,223,204.0 ROCKCHIP CHIPS 3.00 -0.005 -0.2 0.51 -2 -10 60 -0.5 -2 0.07 -0.5 1 4 28 1.29 -10STA 811,146.0 8,223,141.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.64 -2 -10 110 -0.5 -2 0.23 -0.5 1 5 47 2.03 10STA 811,232.0 8,223,023.0 ROCKCHIP CHIPS 0.60 -0.005 -0.2 0.71 4 -10 120 -0.5 -2 0.06 -0.5 2 -1 128 12.35 10STA 811,315.0 8,223,127.0 ROCKCHIP CHIPS 4.00 0.008 -0.2 1.78 -2 -10 60 -0.5 -2 0.5 -0.5 4 22 257 3.11 10STA 811,187.0 8,223,191.0 ROCKCHIP CHIPS 3.00 -0.005 -0.2 0.4 -2 -10 100 -0.5 -2 0.04 -0.5 1 3 96 2.91 -10STA 811,150.0 8,223,252.0 ROCKCHIP CHIPS 4.00 -0.005 -0.2 1.07 -2 -10 60 -0.5 -2 0.17 -0.5 2 21 155 3.61 10

QC -0.005 -0.2 0.35 -2 -10 70 -0.5 -2 0.11 -0.5 2 2 4 0.77 -10STA 811,173.0 8,223,303.0 ROCKCHIP CHIPS 5.50 0.006 -0.2 0.47 -2 -10 240 -0.5 -2 0.05 -0.5 1 11 183 3.6 -10STA 811,166.0 8,223,355.0 ROCKCHIP CHIPS 4.00 0.014 -0.2 0.61 -2 -10 670 -0.5 -2 0.09 -0.5 1 7 376 5.16 -10STA 811,210.0 8,223,398.0 ROCKCHIP CHIPS 5.00 0.005 -0.2 0.39 -2 -10 170 -0.5 -2 0.02 -0.5 1 4 96 1.05 -10STA 811,292.0 8,223,390.0 ROCKCHIP CHIPS 4.00 0.029 0.2 0.77 -2 -10 50 -0.5 2 0.06 -0.5 4 37 1160 4.84 -10STA 811,344.0 8,223,340.0 ROCKCHIP CHIPS 5.00 0.010 -0.2 0.35 2 -10 150 -0.5 -2 0.05 -0.5 1 4 186 2.52 -10STA 811,301.0 8,223,306.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.57 -2 -10 250 -0.5 -2 0.09 -0.5 1 4 251 2.7 -10STA 811,292.0 8,223,350.0 ROCKCHIP CHIPS 5.00 0.019 -0.2 0.45 -2 -10 240 -0.5 -2 0.04 -0.5 1 5 379 2.97 -10STA 811,345.0 8,223,240.0 ROCKCHIP CHIPS 4.00 0.014 0.2 1.63 -2 -10 80 0.5 2 0.4 -0.5 9 129 850 6.19 10STA 811,315.0 8,223,211.0 ROCKCHIP CHIPS 4.00 0.009 -0.2 0.89 -2 -10 70 0.7 -2 0.13 -0.5 2 54 420 5.3 10STA 811,343.0 8,223,150.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.39 2 -10 430 -0.5 -2 0.08 -0.5 1 4 83 2.14 -10STA 811,290.0 8,223,046.0 ROCKCHIP CHIPS 3.00 0.101 -0.2 1.16 3 -10 70 -0.5 2 0.13 -0.5 7 41 193 6.96 -10STA 811,306.0 8,223,029.0 ROCKCHIP CHIPS 4.00 0.012 -0.2 1.22 -2 -10 50 -0.5 -2 0.42 -0.5 7 39 378 2.52 -10STA 811,654.0 8,223,039.0 ROCKCHIP CHIPS 4.00 -0.005 -0.2 1.48 2 -10 130 -0.5 -2 0.42 -0.5 10 1 238 4.14 10STA 811,673.0 8,223,081.0 ROCKCHIP CHANNEL 5.00 0.006 0.2 1.61 -2 -10 110 -0.5 -2 0.42 -0.5 9 1 474 4 10STA 811,678.0 8,223,082.0 ROCKCHIP CHANNEL 5.00 0.006 -0.2 1.66 -2 -10 90 -0.5 -2 0.5 -0.5 8 1 638 3.58 10

QC 0.335 0.7 1.91 12 10 160 0.5 -2 1.39 -0.5 13 46 3540 4.54 10STA 811,697.0 8,223,082.0 ROCKCHIP CHANNEL 5.00 0.009 -0.2 1.02 2 -10 310 -0.5 3 0.16 -0.5 4 1 813 4.99 10STA 811,775.0 8,223,110.0 ROCKCHIP CHANNEL 5.00 0.006 -0.2 0.89 -2 -10 50 -0.5 -2 0.29 -0.5 6 17 130 2.51 -10STA 811,779.0 8,223,112.0 ROCKCHIP CHANNEL 4.00 0.011 0.3 2.13 5 -10 120 1.1 -2 0.11 -0.5 23 33 1430 4.77 10STA 811,782.0 8,223,115.0 ROCKCHIP CHANNEL 5.00 0.005 0.3 3.6 10 10 110 5.5 -2 0.52 -0.5 64 65 8590 5.25 10STA 811,795.0 8,223,115.0 ROCKCHIP CHANNEL 5.00 0.008 0.3 1.86 4 -10 40 0.8 -2 0.67 -0.5 15 83 1360 5.62 10STA 811,813.0 8,223,112.0 ROCKCHIP CHANNEL 5.00 0.012 0.4 1.32 -2 -10 60 -0.5 -2 0.76 -0.5 10 57 486 3.67 10STA 811,815.0 8,223,116.0 ROCKCHIP CHANNEL 6.00 0.010 -0.2 1.44 -2 -10 130 0.5 -2 0.73 -0.5 38 53 1540 4.42 10STA 811,763.0 8,222,998.0 ROCKCHIP CHIPS 3.00 0.013 -0.2 1.17 3 -10 90 -0.5 4 0.45 -0.5 10 25 420 2.6 10STA 811,851.0 8,223,158.0 ROCKCHIP CHIPS 4.50 0.017 0.4 1.14 3 -10 70 -0.5 3 0.46 -0.5 16 6 514 6.63 10STA 811,859.0 8,223,265.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 2.02 3 -10 80 0.5 -2 0.77 -0.5 15 41 61 4.94 10STA 811,790.0 8,223,221.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 0.34 -2 -10 90 -0.5 -2 0.04 -0.5 -1 3 89 1.72 -10STA 811,717.0 8,223,204.0 ROCKCHIP CHIPS 4.00 0.018 -0.2 0.98 2 -10 110 -0.5 2 0.09 -0.5 -1 -1 927 5.47 10STA 811,760.0 8,223,144.0 ROCKCHIP CHIPS 3.00 -0.005 -0.2 0.32 -2 -10 60 -0.5 -2 0.02 -0.5 1 2 169 2.63 -10STA 811,652.0 8,223,151.0 ROCKCHIP CHIPS 4.00 0.005 -0.2 2.56 -2 -10 80 -0.5 -2 0.34 -0.5 4 1 474 2.93 10

QC -0.005 -0.2 0.38 -2 10 80 -0.5 -2 0.11 -0.5 1 1 4 0.7 -10STA 811,592.0 8,223,095.0 ROCKCHIP CHIPS 3.00 0.011 -0.2 1.7 -2 -10 50 -0.5 -2 0.46 -0.5 2 1 269 2.45 10STA 811,621.0 8,222,983.0 ROCKCHIP CHIPS 5.00 -0.005 -0.2 1.58 -2 -10 90 -0.5 -2 0.94 -0.5 7 2 41 1.97 -10STA 811,577.0 8,223,309.0 ROCKCHIP CHIPS 5.00 0.006 -0.2 1.07 3 -10 90 -0.5 -2 0.09 -0.5 1 15 858 4.3 10STA 811,662.0 8,223,254.0 ROCKCHIP CHIPS 4.00 0.007 -0.2 1.27 -2 -10 190 -0.5 -2 0.14 -0.5 -1 79 473 4.95 10STA 811,555.0 8,223,178.0 ROCKCHIP CHIPS 4.00 -0.005 -0.2 0.32 -2 -10 120 -0.5 -2 0.03 -0.5 -1 5 40 2.18 -10STA 811,539.0 8,223,242.0 ROCKCHIP CHIPS 5.00 0.026 -0.2 0.37 -2 -10 130 -0.5 2 0.05 -0.5 -1 2 314 6.1 -10STA 811,492.0 8,223,310.0 ROCKCHIP CHIPS 5.00 0.024 -0.2 0.33 -2 -10 120 -0.5 2 0.06 -0.5 -1 7 407 4.1 -10STA 811,465.0 8,223,371.0 ROCKCHIP CHIPS 5.00 0.018 -0.2 1.32 -2 -10 60 -0.5 -2 0.08 -0.5 1 89 820 3.47 10STA 811,448.0 8,223,243.0 ROCKCHIP CHIPS 3.00 0.019 -0.2 0.55 -2 -10 70 -0.5 -2 0.06 -0.5 -1 22 472 3.44 -10STA 811,488.0 8,223,190.0 ROCKCHIP CHIPS 5.00 0.005 0.2 0.44 -2 -10 90 -0.5 -2 0.03 -0.5 -1 6 180 3.89 -10STA 811,485.0 8,223,101.0 ROCKCHIP CHIPS 2.00 0.005 -0.2 1.99 -2 -10 50 -0.5 -2 0.66 -0.5 5 7 254 2.83 10STA 811,512.0 8,223,019.0 ROCKCHIP CHIPS 5.00 0.005 0.2 2.01 2 -10 50 -0.5 -2 0.4 -0.5 2 1 272 2.37 10STA 811,375.0 8,222,956.0 ROCKCHIP CHIPS 0.70 -0.005 -0.2 0.99 -2 -10 50 -0.5 -2 0.41 -0.5 8 3 353 1.02 -10STA 811,374.0 8,222,954.0 ROCKCHIP CHIPS 3.50 0.012 -0.2 1.85 -2 -10 100 -0.5 -2 0.71 -0.5 13 2 525 2.27 10STA 811,363.0 8,223,012.0 ROCKCHIP CHANNEL 5.00 0.011 -0.2 0.88 -2 -10 40 -0.5 -2 0.39 -0.5 4 27 217 1.94 -10

QC -0.005 -0.2 0.01 -2 10 10 -0.5 -2 -0.01 -0.5 -1 24 8 0.57 -10STA 811,367.0 8,223,017.0 ROCKCHIP CHANNEL 5.00 -0.005 -0.2 2.02 -2 -10 40 -0.5 -2 0.83 -0.5 9 5 389 3.12 10

SampleID218415218416218417218418218419218420218421218422218423218424218425218426218427218428218429218430218431218432218433218434218435218436218437218438218439218440218441218442218443218444218445218446218447218448218449218450218451218452218453218454218455218456218457218458218459218460218461218462218463218464218465218466218467218468218469218470218471218472218473218474218475218476218477218478218479218480218481218482218483218484

Hg_ppm K_% La_ppm Mg_% Mn_ppm Mo_ppm Na_% Ni_ppm P_ppm Pb_ppm S_% Sb_ppm Sc_ppm Sr_ppm Th_ppm Ti_% Tl_ppm U_ppm V_ppm W_ppm Zn_ppm Au_ppm Au_ppm_Grav Cu_AA460.05 0.29 10 0.68 687 -1 0.02 21 810 8 0.02 -2 5 62 -20 0.16 -10 -10 89 -10 59

-1 0.04 -10 0.03 48 1 0.02 2 440 4 0.19 -2 1 17 -20 0.01 -10 -10 33 -10 3 0.132-1 0.08 -10 0.13 61 3 0.01 13 510 6 0.06 2 3 9 -20 0.01 -10 -10 74 -10 12 0.084-1 0.01 -10 0.02 48 3 0.01 9 150 7 0.62 -2 -1 18 -20 -0.01 -10 -10 32 -10 16 0.075-1 0.11 -10 0.18 62 13 0.08 1 460 5 0.17 -2 4 49 -20 0.07 -10 -10 69 -10 3 0.013-1 0.07 -10 0.18 194 47 0.04 1 690 10 0.08 -2 1 19 -20 0.06 -10 -10 66 -10 3 0.031-1 -0.01 -10 -0.01 74 5 -0.01 3 10 2 -0.01 -2 -1 -1 -20 -0.01 -10 -10 1 -10 8 0.006-1 0.12 10 0.59 278 -1 0.05 8 710 3 0.14 -2 3 30 -20 0.11 -10 -10 40 -10 18 -0.005-1 0.19 10 0.59 199 1 0.05 14 750 3 0.16 -2 2 50 -20 0.14 -10 -10 36 -10 22 0.007-1 0.3 10 0.54 97 2 0.03 4 450 4 0.2 -2 5 33 -20 0.08 -10 -10 50 -10 37 -0.005-1 0.26 10 0.73 201 3 0.04 2 550 2 0.23 -2 5 70 -20 0.14 -10 -10 51 -10 23 -0.005-1 0.19 20 0.08 39 1 0.04 2 260 -2 0.09 -2 1 24 -20 0.05 -10 -10 11 -10 6 -0.005-1 0.16 40 0.03 37 5 0.04 -1 180 5 0.07 -2 1 28 -20 0.02 -10 -10 5 -10 5 -0.005-1 0.17 10 0.03 36 1 0.03 -1 190 2 0.05 -2 1 24 -20 0.01 -10 -10 4 -10 4 -0.005-1 0.13 10 0.09 37 1 0.05 1 300 -2 0.14 -2 2 29 -20 0.04 -10 -10 12 -10 6 -0.005-1 0.15 10 0.12 51 1 0.07 1 220 6 0.18 -2 2 46 -20 0.05 -10 -10 11 -10 5 -0.0051 0.18 830 0.1 52 5 0.08 1 1130 41 0.27 -2 1 126 1480 0.07 -10 -10 20 -10 -2 -0.005

-1 0.32 20 0.07 34 32 0.05 1 990 11 0.31 -2 3 117 -20 0.03 -10 -10 70 -10 18 -0.005-1 0.22 30 0.56 126 29 0.06 9 570 3 0.19 -2 9 134 50 0.2 -10 -10 73 -10 18 0.008-1 0.21 40 0.03 41 4 0.04 -1 170 2 0.1 -2 1 24 20 -0.01 -10 -10 7 -10 4 -0.005-1 0.18 10 0.3 67 1 0.04 2 180 4 0.09 -2 5 65 -20 0.06 -10 -10 50 -10 11 -0.005-1 0.15 10 0.11 336 -1 0.24 1 100 -2 0.02 -2 1 18 -20 0.03 -10 -10 7 -10 27 -0.005-1 0.22 20 0.04 44 32 0.05 1 430 -2 0.19 -2 2 51 -20 0.01 -10 -10 21 -10 5 0.006-1 0.22 20 0.06 55 18 0.04 3 530 3 0.15 -2 4 65 20 0.01 -10 -10 32 -10 13 0.014-1 0.18 20 0.03 39 28 0.04 -1 120 -2 0.04 -2 1 21 -20 0.01 -10 -10 4 -10 -2 0.0051 0.17 10 0.15 60 20 0.02 8 470 2 0.04 -2 7 30 -20 0.03 -10 -10 41 -10 9 0.029

-1 0.19 20 0.03 32 28 0.03 -1 250 4 0.13 -2 1 39 -20 -0.01 -10 -10 7 -10 2 0.01-1 0.29 30 0.09 40 37 0.07 2 400 8 0.32 -2 2 70 -20 0.02 -10 -10 16 -10 5 -0.005-1 0.18 30 0.04 48 41 0.04 1 230 3 0.04 -2 2 36 30 0.01 -10 -10 19 -10 2 0.019-1 0.3 10 0.61 108 12 0.05 36 420 -2 0.35 -2 9 75 -20 0.1 -10 -10 75 -10 19 0.014-1 0.22 40 0.24 55 32 0.07 8 1150 3 0.3 -2 6 137 30 0.03 -10 -10 45 -10 7 0.009-1 0.23 20 0.04 51 9 0.03 1 290 -2 0.1 -2 1 32 -20 -0.01 -10 -10 5 -10 2 -0.005-1 0.32 20 0.28 176 13 0.04 18 390 7 0.14 -2 5 39 20 0.05 -10 -10 54 -10 18 0.101-1 0.16 10 0.57 261 2 0.04 20 470 2 0.01 -2 5 34 -20 0.17 -10 -10 53 -10 24 0.012-1 0.11 -10 0.79 240 2 0.04 2 590 7 0.09 -2 4 105 -20 0.13 -10 -10 85 -10 22 -0.005-1 0.18 10 0.77 235 3 0.07 2 510 2 0.4 -2 4 168 -20 0.11 -10 -10 71 -10 14 0.006-1 0.13 -10 0.89 236 5 0.04 2 590 2 0.43 -2 3 80 -20 0.13 -10 -10 67 -10 17 0.0061 0.53 20 1.2 393 257 0.17 20 1060 9 0.5 -2 6 103 -20 0.22 -10 -10 112 -10 64 0.335

-1 0.17 10 0.66 194 6 0.04 2 620 7 0.17 -2 4 114 -20 0.06 -10 -10 54 -10 12 0.009-1 0.13 10 0.51 136 1 0.06 6 350 2 0.98 -2 2 66 -20 0.12 -10 -10 34 -10 14 0.006-1 0.11 10 1.35 257 20 0.03 36 700 10 1.59 -2 5 11 -20 0.08 -10 -10 61 -10 41 0.011-1 0.14 30 2.21 1130 5 0.03 103 1350 6 1.26 -2 8 25 -20 0.17 -10 -10 86 -10 102 0.0051 0.1 10 1.67 522 3 0.06 29 820 6 1.5 -2 6 97 -20 0.18 -10 -10 97 -10 58 0.008

-1 0.08 10 1.12 233 1 0.05 7 620 3 2.61 -2 4 61 -20 0.13 -10 -10 60 -10 29 0.012-1 0.1 10 1.07 690 30 0.07 85 940 6 1.04 -2 6 64 -20 0.19 -10 -10 88 -10 64 0.01-1 0.12 20 0.53 224 1 0.04 12 1220 2 0.01 -2 5 20 -20 0.08 -10 -10 55 -10 14 0.013-1 0.25 10 0.69 289 5 0.1 14 1340 6 2.91 -2 7 63 -20 0.18 -10 -10 101 -10 23 0.0171 0.14 10 1 779 1 0.04 25 900 3 0.01 -2 9 53 -20 0.25 -10 -10 110 -10 46 -0.005

-1 0.22 10 0.03 38 4 0.03 1 220 4 0.1 -2 1 18 -20 0.01 -10 -10 7 -10 3 -0.005-1 0.08 10 0.2 41 16 0.03 1 410 3 0.04 -2 5 124 -20 0.02 -10 -10 64 -10 8 0.018-1 0.17 20 0.02 46 4 0.03 1 270 2 0.09 -2 1 36 -20 -0.01 -10 -10 4 -10 2 -0.005-1 0.15 10 0.65 183 1 0.03 2 320 4 0.06 -2 9 274 -20 0.11 -10 -10 79 -10 32 0.005-1 0.16 10 0.1 317 -1 0.28 -1 90 2 0.02 -2 1 18 -20 0.03 -10 -10 7 -10 25 -0.005-1 0.14 -10 0.67 168 1 0.04 1 340 3 0.03 -2 6 87 -20 0.14 -10 -10 65 -10 20 0.011-1 0.1 -10 0.77 195 1 0.07 -1 550 2 0.42 -2 2 62 -20 0.13 -10 -10 54 -10 16 -0.005-1 0.17 10 0.16 42 5 0.02 2 400 4 0.03 -2 8 41 -20 0.05 -10 -10 56 -10 5 0.006-1 0.15 10 0.28 41 13 0.03 4 290 4 0.05 -2 8 61 -20 0.02 -10 -10 71 -10 12 0.007-1 0.26 20 0.02 32 4 0.13 -1 240 2 0.51 -2 1 40 -20 -0.01 -10 -10 4 -10 -2 -0.005-1 0.14 10 0.03 38 68 0.02 -1 180 2 0.05 -2 1 47 -20 -0.01 -10 -10 34 -10 -2 0.026-1 0.12 10 0.03 34 39 0.02 -1 170 3 0.05 -2 1 24 -20 0.01 -10 -10 25 -10 5 0.024-1 0.13 30 0.4 72 20 0.03 5 250 3 0.04 -2 7 53 40 0.02 -10 -10 51 -10 5 0.018-1 0.15 30 0.1 36 16 0.03 2 260 4 0.06 -2 2 43 20 0.01 -10 -10 26 -10 4 0.019-1 0.22 60 0.02 29 6 0.08 -1 250 5 0.28 -2 1 52 90 0.01 -10 -10 24 -10 -2 0.005-1 0.13 10 0.78 252 2 0.03 3 410 3 0.03 -2 7 91 -20 0.18 -10 -10 78 -10 24 0.005-1 0.09 -10 0.77 125 4 0.03 1 240 3 0.01 -2 6 55 -20 0.12 -10 -10 72 -10 23 0.005-1 0.09 -10 0.53 280 1 0.05 6 380 3 0.01 -2 3 43 -20 0.07 -10 -10 40 -10 12 -0.005-1 0.13 -10 1.1 346 5 0.06 5 640 3 0.04 -2 4 166 -20 0.14 -10 -10 73 -10 24 0.012-1 0.11 50 0.48 130 1 0.05 14 440 3 0.46 -2 3 51 30 0.13 -10 -10 39 -10 12 0.011-1 -0.01 -10 -0.01 76 5 -0.01 3 10 2 -0.01 -2 -1 1 -20 -0.01 -10 -10 1 -10 9 -0.005-1 0.17 10 1.36 304 2 0.03 8 750 3 0.07 -2 5 61 -20 0.22 -10 -10 70 -10 28 -0.005

SampleID218485218486218487218488218489218490218491218492218493218494218495218496218497218498218499218500218501218502218503218504218505218506218507218508218509218510

Prospect Easting Northing SampleType SampleSubTypeSampleWeight_KgMeshSize Au_ppm_mapinfo Ag_ppm Al_% As_ppm B_ppm Ba_ppm Be_ppm Bi_ppm Ca_% Cd_ppm Co_ppm Cr_ppm Cu_ppm Fe_% Ga_ppmSTA 811,370.0 8,223,022.0 ROCKCHIP CHANNEL 5.00 0.016 0.2 1.02 -2 -10 30 -0.5 -2 0.48 -0.5 5 46 241 2.44 10STA 811,372.0 8,223,023.0 ROCKCHIP CHANNEL 1.10 0.010 0.2 0.68 2 -10 30 -0.5 -2 0.06 -0.5 1 7 417 2.35 -10STA 811,373.0 8,223,015.0 ROCKCHIP CHANNEL 5.00 -0.005 -0.2 0.44 -2 -10 40 -0.5 -2 0.06 -0.5 1 6 63 0.8 -10STA 811,380.0 8,223,019.0 ROCKCHIP CHANNEL 5.00 0.008 -0.2 0.88 -2 -10 20 -0.5 -2 0.17 -0.5 2 22 148 1.73 -10STA 811,386.0 8,223,020.0 ROCKCHIP CHANNEL 5.00 0.008 0.2 1.2 -2 -10 30 -0.5 -2 0.58 -0.5 9 39 391 2.9 -10STA 811,389.0 8,223,024.0 ROCKCHIP CHANNEL 5.00 0.019 0.3 1.63 -2 -10 30 -0.5 -2 0.81 -0.5 9 57 296 5.1 10STA 811,390.0 8,223,028.0 ROCKCHIP CHANNEL 5.00 0.007 -0.2 0.89 -2 -10 30 -0.5 -2 0.32 -0.5 5 26 114 2.52 10STA 811,415.0 8,223,124.0 ROCKCHIP CHANNEL 2.50 0.014 -0.2 0.67 -2 -10 50 -0.5 -2 0.19 -0.5 1 6 223 4.71 10STA 811,385.0 8,223,063.0 ROCKCHIP CHIPS 3.00 0.009 -0.2 0.88 2 -10 30 -0.5 -2 0.71 -0.5 4 122 135 1.33 -10STA 811,399.0 8,223,053.0 ROCKCHIP CHIPS 5.00 0.006 -0.2 0.7 -2 -10 60 -0.5 2 0.35 -0.5 4 21 177 2.24 -10STA 811,418.0 8,223,072.0 ROCKCHIP CHIPS 6.00 0.014 0.2 2.14 3 -10 100 -0.5 2 0.46 -0.5 9 180 1270 6 10STA 811,409.0 8,223,058.0 ROCKCHIP CHIPS 5.50 0.009 -0.2 0.86 -2 -10 50 -0.5 -2 0.45 -0.5 11 4 808 1.39 -10STA 811,424.0 8,223,115.0 ROCKCHIP CHANNEL 0.30 2.590 2.2 0.31 3 -10 40 -0.5 16 0.02 -0.5 1 8 692 4.8 -10

QC 0.335 0.8 1.8 11 10 160 -0.5 -2 1.37 -0.5 13 44 3390 4.66 10STA 811,423.0 8,223,112.0 ROCKCHIP CHANNEL 4.00 0.050 -0.2 0.66 3 -10 50 -0.5 4 0.03 -0.5 5 10 660 3.63 -10STA 811,427.0 8,223,135.0 ROCKCHIP CHANNEL 5.00 0.012 -0.2 1.03 -2 -10 60 -0.5 2 0.1 -0.5 4 80 360 5.42 10STA 811,444.0 8,222,873.0 ROCKCHIP CHANNEL 0.50 0.016 -0.2 1.01 2 -10 50 -0.5 6 0.15 -0.5 17 1 281 8.02 10STA 811,447.0 8,222,875.0 ROCKCHIP CHANNEL 3.50 -0.005 -0.2 1.92 -2 -10 50 -0.5 -2 0.37 -0.5 13 2 396 3.31 10STA 811,450.0 8,222,878.0 ROCKCHIP CHANNEL 4.50 -0.005 -0.2 1.54 -2 -10 40 -0.5 -2 0.67 -0.5 6 8 492 3.44 10STA 811,427.0 8,223,138.0 ROCKCHIP CHANNEL 5.00 -0.005 -0.2 0.51 2 -10 60 -0.5 -2 0.06 -0.5 2 5 153 2.61 -10STA 811,427.0 8,223,144.0 ROCKCHIP CHANNEL 5.00 0.026 -0.2 0.92 -2 -10 60 -0.5 2 0.12 -0.5 3 29 164 3.23 -10STA 811,427.0 8,223,149.0 ROCKCHIP CHANNEL 5.00 0.021 -0.2 0.84 2 -10 70 -0.5 -2 0.06 -0.5 4 25 290 5.04 10STA 811,418.0 8,223,205.0 ROCKCHIP CHIPS 5.00 0.006 -0.2 1.86 -2 -10 80 -0.5 -2 0.64 -0.5 7 43 376 5.12 10STA 811,411.0 8,223,220.0 ROCKCHIP CHIPS 5.00 0.005 -0.2 1.04 2 -10 80 -0.5 -2 0.07 -0.5 6 32 259 3.83 -10STA 811,403.0 8,223,259.0 ROCKCHIP CHIPS 5.00 0.005 -0.2 0.73 -2 -10 80 -0.5 -2 0.08 -0.5 10 31 649 3.53 -10STA 811,392.0 8,223,419.0 ROCKCHIP CHIPS 2.00 0.022 -0.2 1.69 2 -10 50 -0.5 -2 0.37 -0.5 9 1 900 2.94 -10

SampleID218485218486218487218488218489218490218491218492218493218494218495218496218497218498218499218500218501218502218503218504218505218506218507218508218509218510

Hg_ppm K_% La_ppm Mg_% Mn_ppm Mo_ppm Na_% Ni_ppm P_ppm Pb_ppm S_% Sb_ppm Sc_ppm Sr_ppm Th_ppm Ti_% Tl_ppm U_ppm V_ppm W_ppm Zn_ppm Au_ppm Au_ppm_Grav Cu_AA46-1 0.12 60 0.68 185 1 0.06 24 630 3 0.34 -2 3 38 20 0.17 -10 -10 56 -10 18 0.016-1 0.12 10 0.13 52 6 0.02 6 600 4 0.02 -2 3 11 -20 0.04 -10 -10 17 -10 7 0.01-1 0.13 40 0.09 48 1 0.08 4 100 4 0.04 -2 -1 13 20 0.01 -10 -10 4 -10 5 -0.005-1 0.1 50 0.51 118 4 0.07 16 250 4 0.3 -2 3 19 30 0.08 -10 -10 35 -10 20 0.008-1 0.17 90 0.82 188 4 0.06 30 710 7 0.95 -2 4 24 40 0.14 -10 -10 61 -10 20 0.008-1 0.19 30 1.6 287 2 0.09 39 1750 -2 1.41 2 5 52 -20 0.3 -10 -10 129 -10 29 0.019-1 0.17 40 0.68 149 1 0.07 12 440 2 0.68 -2 3 26 -20 0.1 -10 -10 40 -10 14 0.007-1 0.13 20 0.15 71 8 0.05 2 350 4 0.11 -2 2 88 -20 0.1 -10 -10 107 -10 5 0.014-1 0.06 90 0.34 137 -1 0.05 17 170 3 0.01 -2 3 45 20 0.1 -10 -10 24 -10 13 0.009-1 0.13 10 0.38 138 2 0.06 17 390 2 0.41 -2 2 35 -20 0.09 -10 -10 26 -10 13 0.006-1 0.26 20 1.41 241 11 0.04 38 650 3 0.15 -2 11 76 -20 0.16 -10 -10 87 -10 28 0.014-1 0.09 20 0.46 202 8 0.05 7 440 2 0.21 -2 2 26 -20 0.07 -10 -10 26 -10 12 0.009-1 0.14 10 0.03 43 13 0.03 1 180 -2 0.14 -2 1 11 -20 0.01 -10 -10 16 -10 2 2.59-1 0.57 20 1.23 392 230 0.18 19 1000 10 0.46 -2 6 93 -20 0.19 -10 -10 104 -10 62 0.335-1 0.14 20 0.15 143 11 0.03 6 270 -2 0.03 -2 3 8 -20 0.02 -10 -10 16 -10 6 0.05-1 0.19 10 0.46 112 10 0.05 9 410 -2 0.49 -2 5 41 -20 0.09 -10 -10 47 -10 10 0.012-1 0.19 -10 0.51 185 20 0.08 1 510 2 0.29 -2 4 66 -20 0.1 -10 -10 86 -10 8 0.016-1 0.16 -10 1.59 376 1 0.06 4 540 -2 0.02 -2 5 26 -20 0.08 -10 -10 91 -10 28 -0.005-1 0.08 10 1.07 390 -1 0.05 3 440 -2 0.03 2 5 14 -20 0.01 -10 -10 69 -10 17 -0.005-1 0.18 10 0.14 55 2 0.06 2 280 -2 0.23 -2 1 30 -20 0.05 -10 -10 14 -10 5 -0.005-1 0.18 10 0.58 114 9 0.06 9 460 -2 0.39 -2 4 39 -20 0.08 -10 -10 39 -10 14 0.026-1 0.23 10 0.32 96 22 0.05 8 450 3 0.3 -2 3 31 -20 0.03 -10 -10 31 -10 10 0.021-1 0.27 10 1.11 266 3 0.12 17 1140 2 0.46 -2 7 86 -20 0.14 -10 -10 97 -10 25 0.006-1 0.32 10 0.55 137 13 0.04 14 270 -2 1 -2 3 25 -20 0.06 -10 -10 28 -10 10 0.005-1 0.21 20 0.36 145 23 0.04 13 300 2 0.72 -2 1 23 -20 0.03 -10 -10 14 -10 9 0.005-1 0.13 -10 1.01 286 59 0.04 2 410 -2 0.19 -2 4 61 -20 0.08 -10 -10 45 -10 28 0.022

APPENDIX II

Selected Maps and Sections Prepared by

Mawson Resources Ltd.

and Buenaventura Ingenieros. S.A.


LA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDALA BANDA

[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/[email protected]/tAu; 0.72%Cu; 86.47g/tAu-eq

5.4m

@2.

09g/

tAu;

1.6

%C

u; 4

.99g

/tAu-

eq5.

4m@

2.09

g/tA

u; 1

.6%

Cu;

4.9

9g/tA

u-eq

5.4m

@2.

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tAu;

1.6

%C

u; 4

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eq5.

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2.09

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Cu;

4.9

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5.4m

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1.6

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u; 4

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eq5.

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4.9

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5.4m

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1.6

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u; 4

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5.4m

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3.5

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3.5

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3.5

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3.5

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1.2m

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3.5

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u; 2

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1.2m

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3.5

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u; 2

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1.2m

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3.5

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u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq

1.2m

@16

.52g

/tAu;

3.5

%C

u; 2

2.88

g/tA

u-eq




XIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA IXIMENA I



0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq0.

60m

@13

.9g/

tAu;

0.1

65%

Cu;

14.

2g/tA

u-eq

0.60

m@

13.9

g/tA

u; 0

.165

%C

u; 1

4.2g

/tAu-

eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq6.

3m@

0.41

g/tA

u; 0

.1%

Cu;

0.5

9g/tA

u-eq

6.3m

@0.

41g/

tAu;

0.1

%C

u; 0

.59g

/tAu-

eq

XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3XIMENA 2 y 3

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

6.05

m@

0.75

g/tA

u; 0

.23%

Cu;

1.1

6g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq2.

83m

@5.

95g/

tAu;

9.9

3%C

u; 2

4.01

g/tA

u-eq

2.83

m@

5.95

g/tA

u; 9

.93%

Cu;

24.

01g/

tAu-

eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.4m

@9.

4g/tA

u; 0

.11%

Cu;

9.5

9g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

1.3m

@15

.99g

/tAu;

0.1

3%C

u; 1

6.23

g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

6.65

m@

0.48

g/tA

u; 0

.5%

Cu;

1.3

8g/tA

u-eq

XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4XIMENA 4

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u0.

25m

@14

4.0g

/tAu;

0.0

27%

Cu

0.25

m@

144.

0g/tA

u; 0

.027

%C

u




811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000

810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500

810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000

812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000

811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500

809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500

3200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200

3000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000

2800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800

DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008DDHAQ008

811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000811000

810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500810500

810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000810000

812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000812000

811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500811500

809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500809500

3200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200320032003200

3000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000300030003000

2800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800280028002800



DDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00WDDHAQ00W

DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ011DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005DDHAQ005


DDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00ZDDHAQ00Z


DDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00YDDHAQ00Y


LEYENDA POR TAMAÑOANCHO DE MUESTREO

>=0.4 <0.6 m

>=0.8 <1.0 m

>= 1.0 m

>=0.6 <0.8 m

<0.4 m

>=0.5 <1.0 ppm Au

>=0.1 <0.5 ppm Au

LEYENDA POR COLORLEY DE Au

>= 5 ppm Au

>=1.0 <5 ppm Au

<0.1 ppm Au

SONDAJE PROPUESTO

SONDAJE PROPUESTO OPCIONAL

[email protected]/t Au

XIMENA 1

[email protected]/t AuIncluye: [email protected]/tAu

3,000 [email protected]/t Au



XIMENA 2 y 3







XIMENA 4


100 metros



[email protected]/tAu



[email protected]/tAu3,000 msnm

LA BANDA

100 metros

SECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDASECCION LONGITUDINAL VETA XIMENA Y VETA LA BANDA

Nota: 0.5%Cu = 1 g/t Au

NO SE

FIGURE:

ALTO QUEMADO PROJECT, PERUPROPERTY GEOLOGY


DATE:

PSAD 56/18S

PROJECTION:SCALE:DRAWING BY:

TCQ-LGCSEE GRID

SECCION LONGITUDINAL VETAS: XIMENA - LA BANDA

SEE SECC

Feb 2011

09

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6.5

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6.5

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6.5

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6.5

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6.5

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6.5

°-1

6.5

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6.5

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6.5

°-1

6.5

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6.5

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6.5

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6.5

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°

-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °

-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 °-73.5 ° -72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °

-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °

-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °-73 °

-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 °-72.5 ° -70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °

-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °

-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °

-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °-70.5 °

-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °-16 °

-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °-16.5 °

-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °-17.5 °

-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °-71 °

-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °-70 °

-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °-18 °

-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °

-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 °-72 ° -71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °-71.5 °

-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °-17 °

10050

kilometers

0

TIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIATIA MARIA

CERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDECERRO VERDE

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LIMA

PERU

FIGURE:

ALTO QUEMADO PROJECT, PERUPROPERTY GEOLOGY


DATE:

PSAD 56/18S

PROJECTION:SCALE:DRAWING BY:

TCQ-LGCSEE GRID

GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)GEOLOGIA REGIONAL - INGEMMET (PROYECTO GR1)

SEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BARSEE BAR

Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011Feb 2011

04040404040404040404040404040404040404040404040404040404040404040404040404040404040404040404040404DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:DRAWING BY:LGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGCLGC

LAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOGLAT / LOG

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VETA XIMENA

VETA FIORELA

VETA LA BANDA

VETA LA LOMADA

UNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETAS


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NANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITO

EL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATO

PLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANAL



XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3

CAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTO

FALLA TORO BRAVO

FALLA VISCACHA

FALLA VENADO

FALLA ZOR

RO

AND

INO

FALLA GUANACO

FA

LLA

TO

TO

RA

YO

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8223000 mN

8221500 mN

812500 mE

8221000 mN

8222000 mN

8222500 mN

811500 mE811000 mE

811000 mE

8222

000

mN

8222

500

mN

8223

000

mN

812500 mE

811500 mE

812000 mE

812000 mE

8223

500

mN

8223500 mN

8224

000

mN

8224000 mN

810500 mE

810500 mE809000 mE

809000 mE

810000 mE

809500 mE

809500 mE

810000 mE82

2100

0 m

N82

2150

0 m

N

0 125 250

meters

vt B y ep (w)

qz ser (s) vt qz (m)

sw qz-py-ser

ser (s) live lim vt Qz "B"

qz-ser (s) live hm

vlt ep, clo (s)

sw goe-ser-hm-OxMn

vt ep+qz

cl - ep - hem (w) dis

Gngr1/2 ep-mt (m)

Gngr 1/2 cl (m)

Gneis FK gr vlts ep (w)

Gngr alcalinoGngrgr

Gngr 1/2 alt(w)

hm sup

Gngr 1/2 vt ep.

hm sup

vn qz-OxFe-OxCu

Grgr cl-mus (m)

cl-OxFe (w) ep vt (w)

ep (w)

vt ep (m)

ep manchas

ep manchas

POZO AGUA

boulder qz lechoso

Boulders Qz-OxFe

boulders Qz-hem (w) vnl ep (s)

bloques gneis asimilados Grdy

Q

Q

Q

UD

intem p

Q

Q

U

Q

Q

200361

mdy py cl-ep (m)

mdy horfels

Dy fina cl-ep

Dk cl-ep-dy (m)

mdy angulo plano corta gneis

vn qz-py-hm 10cm

CATEO

LABOR

LABOR

CATEO floats qz hem viva

intemp

CATEO nn qz

DDHAQ004DDHAQ001

DDHAQ002

DDHAQ012*

DDHAQ00X*

DDHAQ011

DDHAQ005

DDHAQ00Y*DDHAQ007

DDHAQ006

DDHAQ008

DDHAQ00W*

DDHAQ009

DDHAQ010

Dk con OxCu

Grdy/vt py-clo-ep-cpy (w)

vt qz con cl

hm en vt

dike? Grgr Fk

Gngr 1/2

clo (s)

OxFe (10cm) ep(m)

ep (w)

clo+ep (m)

clo (m)

py tz

qz-ser (s)

py-ep (w)

cl (w)

Gngrgr cl (w) vt ep (w) N 130º

vt ep (w)

vt ep (s)

vt ep (m-w)

vt ep (m)

vt ep (m)

qzdy 2m diam

boulder qz-OxFe

Gndy

tz py-mt

Gngr 1/2

vt ep (m)

ser (w)-clo(m)

bloque GnGr fresco

qz-cl(s) OxCu hm, jar(sup) +/-4m

ep (m) vt

Gngr 1/2 ep+clo (m)

200347

200354

200357

200362

200363

200364

AQ-21

AQL-08

AQL-10

AQL-11

AQL-13

vt ep (m)

dy fina

3,000

3,300

2,90

0

3,200

3,10

0

60

60

3055

30

30

55

30

25

45

30

30

35

35

30

30

80

80

70 60

60

5045

40

55

25

45

55

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20

15 15

80

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75

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80

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30

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60

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40

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72

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43

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18

30

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40

40

24

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30

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58

33

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58

60

80

60

60

45

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65

78

70

80

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23

60

35

35

80

15

65

80

85

75

70

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30

70 6080

80

70

32

80

80

45

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80

70 7585

80

85

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70

80

30

60

40

40

20

56

28

30

60

45

70

40

8075

75

60

30

23

50

35

40

35

42

20

60

70 65

45

60

5551

45

30

26

72

53

65

60

28

45

55

50

75

45

76

57

50

40

758060

30

28

55

62

45

28

33

20

40

80

70 70

7070

40

23

2520

60

35

65

75

50

35

45

38

25

50

48

65

65

60

60

60 70

60

80

60

60

80

35

78

75

85

25

20

80

80

65

85

50

60

6545

50

25

20

50

15

60

40

70

43

25

30

40

30

53

60

45

40

42

85

85

75

50

70

70

42

85

55

3533

75

5845

77

77

77

45

54

65

70

80

80

75

45

8077

40

74

65

44

70

75

80

55

70

60

60

45

50

70

78

7580

17

65

65 80

75

50

60

25

25

40

35

85

65

7222

30

7035

80

21

26

23

30

25

60

70

20

30

60

60

56

70

6070

75

80 25

7060

10

70

85 85

80

80 80

80

80

70

76

60

70

80

85

505050

60

6060

60

60

55

75

75 75

50

26

66

50

70

56

55

65

60

60 55

52

45

58

85

63

85

45

5070

85

60

80

85

43

32

75

60

70

75

70 40

40

82

58

90

85

38

60

60

60

60

60

15

70

20

20

3060

60

60

70

30

50 70

5070

60

70

60

60

80

75

55

75

50

80

38

25

60

65 70

75

60

70

60

88

75

LABOR

LABOR

Vetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas Mesotermales

45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°

FallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallas

Fallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas Interpretadas

GranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodiorita

Monzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / Dioritas

CuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonita

Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Granítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/Diorítico

MicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodiorita

60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°

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Foliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo Deformado

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Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)

TrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrinchera

CarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarretera

DenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenuncios

Sondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje Propuesto

Rb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/Estructuras

Rb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y Fracturas

Línea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de Sección

THIS PRINT AND ALL INFORMATION THEREON IS OUR PROPERTY, IS CONFIDENTIAL

Office: Perú

Scale: 1/5,000

Date: Feb 2011

Geol. by: RLC - LGC - TCQ

Rev. by: RLC

AND MUST NOT BE MADE PUBLIC OR COPIED UNLESS AUTHORIZED BY US. IT IS

SUBJECT TO RETURN ON DEMAND.

Project : ALTO QUEMADO

Projection : PSAD 56 - ZONA 18

MINERAL EXPLORATION DEPARTAMENT

LIMA - PERÚ

Drawn by: LGC - TCQ

P_File N° 001

Map N°

File Name:

GEOLOGIA LOCAL INTERPRETADA

03

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VETA XIMENA

VETA FIORELA

VETA LA BANDA

VETA LA LOMADA

UNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETASUNION VETAS


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NANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITONANDITO

EL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATOEL CHATO

PLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANALPLANTA ARTESANAL



XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3XIMENA 2 Y 3

CAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTOCAMPAMENTO

FALLA TORO BRAVO

FALLA VISCACHA

FALLA VENADO

FALLA ZOR

RO

AND

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FALLA GUANACO

FA

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TO

TO

RA

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8223000 mN

8221500 mN

812500 mE

8221000 mN

8222000 mN

8222500 mN

811500 mE811000 mE

811000 mE

8222

000

mN

8222

500

mN

8223

000

mN

812500 mE

811500 mE

812000 mE

812000 mE

8223

500

mN

8223500 mN

8224

000

mN

8224000 mN

810500 mE

810500 mE809000 mE

809000 mE

810000 mE

809500 mE

809500 mE

810000 mE82

2100

0 m

N82

2150

0 m

N

0 125 250

meters

vt B y ep (w)

qz ser (s) vt qz (m)

sw qz-py-ser

ser (s) live lim vt Qz "B"

qz-ser (s) live hm

vlt ep, clo (s)

sw goe-ser-hm-OxMn

vt ep+qz

cl - ep - hem (w) dis

Gngr1/2 ep-mt (m)

Gngr 1/2 cl (m)

Gneis FK gr vlts ep (w)

Gngr alcalinoGngrgr

Gngr 1/2 alt(w)

hm sup

Gngr 1/2 vt ep.

hm sup

vn qz-OxFe-OxCu

Grgr cl-mus (m)

cl-OxFe (w) ep vt (w)

ep (w)

vt ep (m)

ep manchas

ep manchas

POZO AGUA

boulder qz lechoso

Boulders Qz-OxFe

boulders Qz-hem (w) vnl ep (s)

bloques gneis asimilados Grdy

Q

Q

Q

UD

intem p

Q

Q

U

Q

Q

200361

mdy py cl-ep (m)

mdy horfels

Dy fina cl-ep

Dk cl-ep-dy (m)

mdy angulo plano corta gneis

vn qz-py-hm 10cm

CATEO

LABOR

LABOR

CATEO floats qz hem viva

intemp

CATEO nn qz

DDHAQ004DDHAQ001

DDHAQ002

DDHAQ012*

DDHAQ00X*

DDHAQ011

DDHAQ005

DDHAQ00Y*DDHAQ007

DDHAQ006

DDHAQ008

DDHAQ00W*

DDHAQ009

DDHAQ010

Dk con OxCu

Grdy/vt py-clo-ep-cpy (w)

vt qz con cl

hm en vt

dike? Grgr Fk

Gngr 1/2

clo (s)

OxFe (10cm) ep(m)

ep (w)

clo+ep (m)

clo (m)

py tz

qz-ser (s)

py-ep (w)

cl (w)

Gngrgr cl (w) vt ep (w) N 130º

vt ep (w)

vt ep (s)

vt ep (m-w)

vt ep (m)

vt ep (m)

qzdy 2m diam

boulder qz-OxFe

Gndy

tz py-mt

Gngr 1/2

vt ep (m)

ser (w)-clo(m)

bloque GnGr fresco

qz-cl(s) OxCu hm, jar(sup) +/-4m

ep (m) vt

Gngr 1/2 ep+clo (m)

200347

200354

200357

200362

200363

200364

AQ-21

AQL-08

AQL-10

AQL-11

AQL-13

vt ep (m)

dy fina

3,000

3,300

2,90

0

3,200

3,10

0

60

60

3055

30

30

55

30

25

45

30

30

35

35

30

30

80

80

70 60

60

5045

40

55

25

45

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20

15 15

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30

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72

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43

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18

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40

40

24

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58

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60

60

45

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65

78

70

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23

60

35

35

80

15

65

80

85

75

70

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30

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80

70

32

80

80

45

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80

85

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70

80

30

60

40

40

20

56

28

30

60

45

70

40

8075

75

60

30

23

50

35

40

35

42

20

60

70 65

45

60

5551

45

30

26

72

53

65

60

28

45

55

50

75

45

76

57

50

40

758060

30

28

55

62

45

28

33

20

40

80

70 70

7070

40

23

2520

60

35

65

75

50

35

45

38

25

50

48

65

65

60

60

60 70

60

80

60

60

80

35

78

75

85

25

20

80

80

65

85

50

60

6545

50

25

20

50

15

60

40

70

43

25

30

40

30

53

60

45

40

42

85

85

75

50

70

70

42

85

55

3533

75

5845

77

77

77

45

54

65

70

80

80

75

45

8077

40

74

65

44

70

75

80

55

70

60

60

45

50

70

78

7580

17

65

65 80

75

50

60

25

25

40

35

85

65

7222

30

7035

80

21

26

23

30

25

60

70

20

30

60

60

56

70

6070

75

80 25

7060

10

70

85 85

80

80 80

80

80

70

76

60

70

80

85

505050

60

6060

60

60

55

75

75 75

50

26

66

50

70

56

55

65

60

60 55

52

45

58

85

63

85

45

5070

85

60

80

85

43

32

75

60

70

75

70 40

40

82

58

90

85

38

60

60

60

60

60

15

70

20

20

3060

60

60

70

30

50 70

5070

60

70

60

60

80

75

55

75

50

80

38

25

60

65 70

75

60

70

60

88

75

LABOR

LABOR

Vetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas MesotermalesVetas Mesotermales

45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°45°

FallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallasFallas

Fallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas InterpretadasFallas Interpretadas

GranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodioritaGranodiorita

Monzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / DioritasMonzodiorita / Dioritas

CuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonitaCuarzomonzonita

Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Intrusivo Deformado: Granítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/DioríticoGranítico/Diorítico

MicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodioritaMicrodiorita

60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°60°

LEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDALEYENDA

Foliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo DeformadoFoliación del Intrusivo Deformado

f

f80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°80°

Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)Granodiorita del Batolito (136 Ma)

TrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrincheraTrinchera

CarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarreteraCarretera

DenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenunciosDenuncios

Sondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje PropuestoSondaje Propuesto

Rb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/EstructurasRb/Bz Vetas/Estructuras

Rb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y FracturasRb/Bz Fallas y Fracturas

Línea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de SecciónLínea de Sección

THIS PRINT AND ALL INFORMATION THEREON IS OUR PROPERTY, IS CONFIDENTIAL

Office: Perú

Scale: 1/5,000

Date: Feb 2011

Geol. by: RLC - LGC - TCQ

Rev. by: RLC

AND MUST NOT BE MADE PUBLIC OR COPIED UNLESS AUTHORIZED BY US. IT IS

SUBJECT TO RETURN ON DEMAND.

Project : ALTO QUEMADO

Projection : PSAD 56 - ZONA 18

MINERAL EXPLORATION DEPARTAMENT

LIMA - PERÚ

Drawn by: LGC - TCQ

P_File N° 001

Map N°

File Name:

GEOLOGIA LOCAL DATOS FACTUALES

02

Geo_5k_LocalF.wor

APPENDIX III

Geophysical Images



Alto Quemado Project - Arequipa Peru

IP Model Stack

50m Pole - Dipole IP data Zonge Smooth Model Inversion

resistivity model displayed in log10 ohm.m Chargeability Model contours on Resistivity Model

Author : DJM Ref : PSAD56 Zn18

Drawn : Montana GIS

Date : 3-Jul-2010 Report No :

Scale 1: 10 000 Plan No :

0 200 400 600 800

metres

Scale 1: 10 000

10100e Chargeability Model (msec)

810100 E 8222600 N

810100 E 8222800 N

810100 E 8223000 N

810100 E 8223200 N

810100 E 8223400 N

810100 E 8223600 N

810100 E 8223800 N

2800 2800

2850 2850

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3000 3000

3050 3050

3100 3100

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3300 3300

3350 3350

0.0

13.8

27.5

41.3

55.0

msec


810300 E 8222400 N

810300 E 8222600 N

810300 E 8222800 N

810300 E 8223000 N

810300 E 8223200 N

810300 E 8223400 N

810300 E 8223600 N

810300 E 8223800 N

2800 2800

2850 2850

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3000 3000

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0.0

13.8

27.5

41.3

55.0

msec


810500 E 8222400 N

810500 E 8222600 N

810500 E 8222800 N

810500 E 8223000 N

810500 E 8223200 N

810500 E 8223400 N

810500 E 8223600 N

810500 E 8223800 N

2800 2800

2850 2850

2900 2900

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3000 3000

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0.0

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41.3

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msec


810700 E 8222400 N

810700 E 8222600 N

810700 E 8222800 N

810700 E 8223000 N

810700 E 8223200 N

810700 E 8223400 N

810700 E 8223600 N

810700 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

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0.0

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27.5

41.3

55.0

msec


810900 E 8222600 N

810900 E 8222800 N

810900 E 8223000 N

810900 E 8223200 N

810900 E 8223400 N

810900 E 8223600 N

810900 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

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0.0

13.8

27.5

41.3

55.0

msec


811100 E 8222600 N

811100 E 8222800 N

811100 E 8223000 N

811100 E 8223200 N

811100 E 8223400 N

811100 E 8223600 N

811100 E 8223800 N

811100 E 8224000 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

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3300 3300

3350 3350

0.0

13.8

27.5

41.3

55.0

msec


811300 E 8222600 N

811300 E 8222800 N

811300 E 8223000 N

811300 E 8223200 N

811300 E 8223400 N

811300 E 8223600 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

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0.0

13.8

27.5

41.3

55.0

msec


811500 E 8222600 N

811500 E 8222800 N

811500 E 8223000 N

811500 E 8223200 N

811500 E 8223400 N

811500 E 8223600 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

0.0

13.8

27.5

41.3

55.0

msec


811700 E 8222600 N

811700 E 8222800 N

811700 E 8223000 N

811700 E 8223200 N

811700 E 8223400 N

811700 E 8223600 N

811700 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

0.0

13.8

27.5

41.3

55.0

msec


811900 E 8222600 N

811900 E 8222800 N

811900 E 8223000 N

811900 E 8223200 N

811900 E 8223400 N

811900 E 8223600 N

811900 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

0.0

13.8

27.5

41.3

55.0

msec

10100e Resistivity Model (ohm.m log10)

810100 E 8222600 N

810100 E 8222800 N

810100 E 8223000 N

810100 E 8223200 N

810100 E 8223400 N

810100 E 8223600 N

810100 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


810300 E 8222400 N

810300 E 8222600 N

810300 E 8222800 N

810300 E 8223000 N

810300 E 8223200 N

810300 E 8223400 N

810300 E 8223600 N

810300 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


810500 E 8222400 N

810500 E 8222600 N

810500 E 8222800 N

810500 E 8223000 N

810500 E 8223200 N

810500 E 8223400 N

810500 E 8223600 N

810500 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


810700 E 8222400 N

810700 E 8222600 N

810700 E 8222800 N

810700 E 8223000 N

810700 E 8223200 N

810700 E 8223400 N

810700 E 8223600 N

810700 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


810900 E 8222600 N

810900 E 8222800 N

810900 E 8223000 N

810900 E 8223200 N

810900 E 8223400 N

810900 E 8223600 N

810900 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


811100 E 8222600 N

811100 E 8222800 N

811100 E 8223000 N

811100 E 8223200 N

811100 E 8223400 N

811100 E 8223600 N

811100 E 8223800 N

811100 E 8224000 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


811300 E 8222600 N

811300 E 8222800 N

811300 E 8223000 N

811300 E 8223200 N

811300 E 8223400 N

811300 E 8223600 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


811500 E 8222600 N

811500 E 8222800 N

811500 E 8223000 N

811500 E 8223200 N

811500 E 8223400 N

811500 E 8223600 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


811700 E 8222600 N

811700 E 8222800 N

811700 E 8223000 N

811700 E 8223200 N

811700 E 8223400 N

811700 E 8223600 N

811700 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10


811900 E 8222600 N

811900 E 8222800 N

811900 E 8223000 N

811900 E 8223200 N

811900 E 8223400 N

811900 E 8223600 N

811900 E 8223800 N

2800 2800

2850 2850

2900 2900

2950 2950

3000 3000

3050 3050

3100 3100

3150 3150

3200 3200

3250 3250

3300 3300

3350 3350

1.7

2.1

2.5

2.8

3.2

ohm.m log10



Resistivity Model Depth Slices


resistivity model displayed in log10 ohm.m Chargeability Model contours on Resistivity Model


Drawn : Montana GIS Images: Linear Stretch



0 500 1000 1500

metres

Scale 1: 20 000

Chargeability Depthslice 0015m (msec)

810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

1.8

2.1

2.5

2.9

3.3

ohm.m (log10)



IP Model Depth Slices



Drawn : Montana GIS Images: Linear Stretch



0 500 1000 1500

metres

Scale 1: 20 000


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec


810500 E

810500 E

811000 E

811000 E

811500 E

811500 E

8222500 8222500

8223000 8223000

8223500 8223500

8224000 8224000

5.0

17.5

30.0

42.5

55.0

msec

CERTIFICATE of AUTHOR

I, John Nebocat, P. Eng. do hereby certify that:

1. I am currently employed as an independent consultant by:

PGS Pacific Geological ServicesRR#5, 1486 Islandview DriveGibsons, B.C. V0N 1V5

2. I graduated with a bachelor's degree in Geological Engineering (Honours) from theMontana College of Mineral Science and Technology in 1984. In addition, I haveobtained a Diploma in Mining Technology from the British Columbia Institute ofTechnology, Burnaby, B.C., in 1974.

3. I am a member of the Professional Engineers and Geoscientists of British Columbia.

4. I have worked as a geologist for a total of 25 years since my graduation from university.

5. I have read the definition of "qualified person" set out in National Instrument 43-101("NI 43-101") and certify that by reason of my education, affiliation with a professionalassociation (as defined in NI 43-101) and past relevant work experience, I fulfill therequirements to be a "qualified person" for the purposes of NI 43-101.

6. I am responsible for the preparation of all sections the technical report titled, Report onthe Geology and Mineralization of the Alto Quemado Gold-Copper Property NearArequipa, Peru and dated 05/15/2011 (the "Technical Report") relating to the AltoQuemado 1, Relleno 1, Soltero 1, Relleno 3, Relleno 4 and Alto Quemado 2004 properties. I visited the Alto Quemado 1 and Soltero 1 properties on October 25 andOctober 26 for two (2) days.

7. I have not had prior involvement with the properties that are the subject of the TechnicalReport.

8. I am not aware of any material fact or material change with respect to the subject matterof the Technical Report that is not reflected in the Technical Report, the omissions todisclose which makes the Technical Report misleading.

Administering the Canadian Securities Regulatory System/ Régissant le Système de réglementation canadien en valeurs mobilières

PGS PACIFIC GEOLOGICAL SERVICESJohn Nebocat, Geologist, P. Eng.

R.R.#5, 1486 Islandview Drive, Gibsons, B.C. V0N 1V5Tel/Fax: (604) 886-3499 Cellular: (604) 989-4222

e-mail: [email protected]

AdministratorsCanadian Securities

en valeurs mobilièresAutorités canadiennes

9. I am independent of the issuer applying all of the tests in section 1.4 of NationalInstrument 43-101.

10. I have read National Instrument 43-101 and Form 43-101F, and the Technical Report hasbeen prepared in compliance with that instrument and form.

11. I consent to the filing of the Technical Report with any stock exchange and otherregulatory authority and any publication by them, including electronic publications in thepublic company files on their websites accessible by the public, of the Technical Report.

Dated this 19th Day of May, 2011.

JOHN NEBOCAT, P.ENG.

Administering the Canadian Securities Regulatory System/ Régissant le Système de réglementation canadien en valeurs mobilières

ALTO-QUEMADO_43-101-REPORT.pdf

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Transcript of ALTO-QUEMADO_43-101-REPORT.pdf