Mt Edwards JORC Code (2012 Edition) Mineral Resource ... · 19-04-2018 · weighting squared...
-
Upload
trinhkhanh -
Category
Documents
-
view
215 -
download
0
Transcript of Mt Edwards JORC Code (2012 Edition) Mineral Resource ... · 19-04-2018 · weighting squared...
19 April 2018
Mt Edwards JORC Code (2012 Edition) Mineral Resource
48,200 Nickel Tonnes
HIGHLIGHTS
Previously reported nickel Mineral Resources at Mt Edwards reviewed and now
reported in accordance with the JORC Code (2012 Edition).
Mt Edwards nickel Mineral Resources estimated at 3.05 million tonnes at 1.6% Ni for
48,200t of contained nickel.
Mt Edwards nickel tenements included in recent Mt Edwards Lithium Project
acquisition.
Neometals Ltd (ASX: NMT) (“Neometals”) is pleased to announce details of the nickel Mineral
Resources at the Mt Edwards tenement holding. As announced on 15 March 2018, Neometals has
executed binding agreements to acquire a package of tenure and mineral rights including lithium
and nickel rights comprising the Mt Edwards Project.
The tenement package is located 40km south of the Mt Marion Lithium Project (Neometals 13.8%,
through Reed Industrial Minerals Pty Ltd) (refer Figure 1 and Appendix 1).
Mt Edwards Nickel Mineral Resources Table
Measured Indicated Inferred TOTAL Mineral Resources
Deposit Tonne
(Kt)
Nickel
(%)
Tonne
(Kt)
Nickel
(%)
Tonne
(Kt)
Nickel
(%)
Tonne
(Kt)
Nickel
(%)
Nickel
(t)
132N 110 3.5 10 1.8 120 3.4 4,070
Armstrong 10 2.1 280 2.3 30 4.9 320 2.6 8,180
Cooke 150 1.3 150 1.3 1,950
McEwen 1,070 1.3 1,070 1.3 13,380
McEwen
Hangingwall 1,060 1.4 1,060 1.4 14,840
Zabel 330 1.8 330 1.8 5,780
TOTAL 10 2.1% 390 2.7% 2,650 1.4% 3,050 1.6% 48,200
For
per
sona
l use
onl
y
This Mineral Resource estimate is reported in accordance with the 2012 Edition of the ‘Australasian
Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’ prepared by the Joint
Or Reserves Committee of The Australasian Institute of Mining and Metallurgy, Australian Institute of
Geoscientists and Minerals Council of Australia (JORC Code) and follows a detailed interrogation and
review of the previously reported Mineral Resource estimates under the 2004 Edition of the JORC
Code by the previous owners of these tenements.
Figure 1: Mt Edwards Project & Nickel Mineral Resource Location
The Mt Edwards Project Mineral Resource encompasses part of a series of discrete nickel deposits
located on the acquired tenements. The remaining deposits will be evaluated and reported by
Neometals in accordance with JORC Code (2012 Edition) at completion of the nickel rights assignment.
Nickel is an essential component of battery for the electric vehicle (EV) and electric static storage
markets (ESS) and will form part of Neometals’ exploration and development strategy in the Mt
Edwards‐Widgiemooltha Dome area.
A summary of geology, mineralisation, estimation methodology, drill information, drill intercepts in is
provided below and in Appendices 1 to 5 accompanying this announcement.
As announced on 15 March 2018, completion of the acquisition remains conditional upon the receipt
of any necessary Ministerial consents to the transfer of the tenements, together with the receipt or
execution of any necessary consents and deeds of assignment/assumption in respect of the rights and
obligations of third parties. Completion is anticipated to occur within 2 to 3 months.
For
per
sona
l use
onl
y
A summary of information relevant to the estimates of Mineral Resources for the relevant deposits in
the Mt Edwards Project is provided in appendices attached to this announcement.
132N deposit Mineral Resource
Geology/Geological Interpretation
The mineralisation at 132N consists of structurally modified or emplaced thin anastomosing lenses of disseminated and massive Ni sulphides hosted by talc‐chlorite‐carbonate ultramafic. Overall the Ni mineralisation strikes about 340° ‐ 345° and dips approximately 65° to the west.
Sampling Sub‐sampling
Diamond core spilt ½ and ¼. Percussion & RC split 1 metre splits using riffle splitter.
Drilling Techniques Diamond, reverse circulation & percussion.
Classification Criteria
Resource classification determined on the basis of geological continuity and confidence, the number of drill hole intersections, and average distance to samples.
Sample Analysis Method
4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques.
Estimation Methodology
Grades interpolated within grade‐based domain (nominally 1.0% Ni) with a maximum internal dilution of two metres. Grade was interpolated using a combination of inverse distance weighting squared (IDW2) using Surpac software.
Cut‐off Grades Mineral Resources quoted using a 1% Ni block cut‐off.
Mining and metallurgical methods and parameters and other material modifying factors
Modifying factors are not applied for Mineral Resources, however it is considered to have reasonable prospects for eventual economic extraction via open pit and underground methods.
Armstrong deposit Mineral Resource
Geology/Geological Interpretation
Armstrong nickel mineralisation is hosted by talc‐chlorite‐carbonate altered ultramafics and typically has a pyrrhotite + pentlandite + pyrite +/‐ chalcopyrite assemblage. The mineralisation dips about 45 degrees west and plunges to the north west at around 25 degrees.
Sampling Sub‐sampling
Diamond core spilt ½ and ¼. Percussion & RC split 1 metre splits using riffle splitter.
Drilling Techniques Diamond, reverse circulation & percussion.
Classification Criteria
Resource classification determined on the basis of geological continuity and confidence, the number of drill hole intersections, and average distance to samples.
Sample Analysis Method
4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques.
Estimation Methodology
Grades interpolated within grade‐based domain (nominally 1.0% Ni) with a maximum internal dilution of two metres. Grade was interpolated using inverse distance weighting squared (IDW2) and Surpac software.
Cut‐off Grades Mineral Resources quoted using a 1% Ni block cut‐off.
For
per
sona
l use
onl
y
Mining and metallurgical methods and parameters and other material modifying factors
Modifying factors are not applied for Mineral Resources, however it is considered to have reasonable prospects for eventual economic extraction via open pit and underground methods.
Cooke deposit Mineral Resource
Geology/Geological Interpretation
The Cooke nickel sulphide mineralisation is developed on and above a ultramafic‐ mafic contact and has a steep northerly plunging syncline structure. The syncline dips steeply east and both east and west limbs contain nickel mineralisation.
Sampling Sub‐sampling
Diamond core spilt ½ and ¼. Percussion & RC split 1 metre splits using riffle splitter.
Drilling Techniques Diamond, reverse circulation & percussion.
Classification Criteria
Resource classification determined on the basis of geological continuity and confidence, the number of drill hole intersections, and average distance to samples, and lack of QAQC data.
Sample Analysis Method
4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques.
Estimation Methodology
Grades interpolated within grade‐based domain (nominally 1.0% Ni) with a maximum internal dilution of two metres. Grade was interpolated using ordinary kriging and Micromine software.
Cut‐off Grades Mineral Resources quoted using a 1% Ni block cut‐off.
Mining and metallurgical methods and parameters and other material modifying factors
Modifying factors are not applied for Mineral Resources, however it is considered to have reasonable prospects for eventual economic extraction via open pit methods.
Zabel desposit and McEwen and McEwen Hangingwall deposits Mineral Resource
Geology/Geological Interpretation
Mineralisation at Zabel and McEwen is interpreted to be structurally modified “Kambalda Style” nickel occurrence. The mineralisation is essentially draped over the hinge of a gently north plunging tight anticlinal structure. Mineralisation is generally parallel to the basal contact of the ultramafic package so the geometry is controlled by which part of the anticline the mineralisation occurs. Mineralisation occurs as basal contact massive and stringer mineralisation as well as hanging‐wall disseminated mineralisation higher up in the ultramafic sequence.
Sampling Sub‐sampling
Diamond core spilt ½ and ¼. Percussion & RC split 1 metre splits using riffle splitter.
Drilling Techniques Diamond, reverse circulation & percussion.
For
per
sona
l use
onl
y
Classification Criteria
Resource classification determined on the basis of geological continuity and confidence, the number of drill hole intersections, and average distance to samples, and lack of QAQC data.
Sample Analysis Method
4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques.
Estimation Methodology
The Mineral Resource estimate is based on a nominal 0.5% Ni wireframe cut‐off with a maximum internal dilution of two metres. Grade was interpolated using ordinary kriging, Surpac Block Maths and direct assignment techniques using Surpac software.
Cut‐off Grades Mineral Resources quoted using a 1% Ni block cut‐off.
Mining and metallurgical methods and parameters and other material modifying factors
Modifying factors are not applied for Mineral Resources, however the deposit is considered to have reasonable prospects for eventual economic extraction via open pit methods.
ENDS
For further information, please contact:
Chris Reed
Managing Director
Neometals Ltd
T: +61 8 9322 1182
Media
Michael Weir / Cameron Gilenko
Citadel‐MAGNUS
T: +61 8 6160 4900
Competent Person’s Statement:
The information in this announcement that relates to Exploration Results and Mineral Resources is
based on, and fairly represents, information and supporting documentation compiled and prepared
by Mr Luke Marshall who is a Member of The Australasian Institute of Geoscientists. Mr Marshall is a
sole trader and independent contractor to Neometals Ltd.
Mr Marshall has sufficient experience which is relevant to the styles of mineralisation and types of
deposit under consideration and to the activity being undertaken to qualify as a Competent Person as
defined in the 2012 Edition of the JORC Code.
Mr Marshall has provided prior written consent as to the form and context in which the Exploration
Results and Mineral Resources and the supporting information are presented in this market
announcement.
For
per
sona
l use
onl
y
Appendix 1 – Details of of relevant Tenure relating to the Mt Edwards nickel Mineral Resources
Tenement ID Interest %
M15/101 100 (No gold interest)
M15/99 100 (No gold interest)
M15/653 100 (No gold interest)
M15/97 100 (No gold interest)
M15/96 100 (No gold interest)
M15/102 100 (No gold interest)
M15/100 100 (No gold interest)
M15/1271 100 (No gold interest)
For
per
sona
l use
onl
y
Appendix 2 – JORC Code (2012 Edition) Mineral Resource Estimate Summaries
132N deposit Mineral Resource
An interrogation and review of the Mineral Resource estimates for the 132N deposit previously
evaluated by Consolidated Minerals Ltd (CML) in accordance with the JORC Code (2004 Edition), has
resulted in this restatement by Neometals of the Mineral Resource estimate in accordance with JORC
Code (2012 Edition). There are minor changes to the tonnage, grade and classifications but these are
considered immaterial in the context of this report.
The 132N deposit is one of a series of nickel deposits located on the tenements acquired by
Neometals. A summary of geology, mineralisation, estimation methodology, drill information, drill
intercepts and JORC Code (2012 Edition) Table 1 is provided here and in Appendices 1 to 5. The Mineral
Resource estimate for 132N is set out in the table below:
Mineral Resources Metal Grade Contained Metal
Category Cut off Tonnage Nickel Arsenic Copper Nickel Arsenic Copper
(Ni %) (Kt) (%) (ppm) (ppm) (t) (t) (t)
Indicated 1 105 3.54 790 2721 3719 83 286
Inferred 1 11 1.77 573 1059 188 6 11
Total 1 116 3.38 770 2568 3907 89 297
The mineralisation at the 132N deposit consists of structurally modified or emplaced thin
anastomosing lenses of disseminated and massive Ni sulphides hosted by talc‐chlorite‐carbonate
ultramafic. Overall the Ni mineralisation strikes approximately 340° ‐ 345° and dips approximately 65°
to the west. The following is important background information supporting this Mineral Resource
estimate.
The Mineral Resource estimate is based on a nominal 1.0% Ni wireframe cut‐off with a maximum
internal dilution of two metres. Grade was interpolated using a combination of inverse distance
weighting squared (IDW2), Surpac Block Maths, and direct assignment techniques using Surpac
software.
Statistics and a regression between nickel and specific gravity measurements were completed. That
work was also used as the basis for specific gravity estimates in the current model. SGs were assigned
to fresh mineralised material in the block model using the formula (Ni% x 0.0725) + 2.8023).
Drill data, interpretations and models are in GDA94 coordinates.
Resource classification was determined on the basis of geological continuity and confidence, the
number of drill hole intersections, and average distance to samples, as follows:
All domains and blocks defined by a single drill hole were assigned as unclassified and not included in the Mineral Resource estimate
Areas where the nominal drill hole spacing approached 25 x 25m or better, or where geological continuity and confidence were high were classified as Indicated Mineral Resource
Resources above the base of supergene sulphide (completely weathered) were assigned as unclassified irrespective of geology or the drill hole spacing. This is due to the uncertainties relating to mineralogy and processing routes. Classifying this material as unclassified has the
For
per
sona
l use
onl
y
effect of excluding it from the Mineral Resource estimate and any further economic evaluations.
Nickel mineralisation and arsenic values were validated by northing and RL versus the domain composites from the drill hole database. The estimated mineralisation displays a very good correlation between the drill hole composites and the grade estimated from the block model. Filling of the Ni grades in the block model behaved as expected and the graphs display an averaging effect of the high and low values within the drill hole data. Arsenic may be overstated in some areas of the model.
Australian Nickel Mines NL (ANM) completed an unpublished Mineral Resource estimate for the 132N
deposit in January 2008 in compliance with the JORC Code (2004 Edition). This estimate differed from
previous models in that all oxide and sulphide resources were re‐interpreted and interpolated.
A detailed review and interrogation of the January 2008 Mineral Resource estimate was completed to
determine if any further work was required to generate an updated Mineral Resource estimate in
compliance with the JORC Code (2012 Edition). Data, interpretations and methodologies were all
found to be of a reasonable standard and it was determined that no further work was necessary to
report the Mineral Resource estimate in compliance with the JORC Code (2012 Edition), although the
classifications and reporting methods in some areas of the model were changed.
It should be noted that re‐interpretation of the wireframes and re‐estimation of the Mineral Resource
are recommended before any future economic evaluations are completed on the project.
Long section, 132N: showing mineralisation domains (looking west)
For
per
sona
l use
onl
y
Cross Section, 132N: 6518900mN showing drilling and mineralisation domains
Plan view, 132N: showing drill holes and nickel mineralisation domains
Armstrong deposit Mineral Resource
An interrogation and review of the Mineral Resource estimates for the Armstrong deposit previously
evaluated by CML’s in compliance with the JORC Code (2004 Edition) has resulted in this restatement
of the Mineral Resource estimate by Neometals in accordance with the JORC Code (2012 Edition).
There are minor changes to the tonnage, grade and classifications but these are considered immaterial
in the context of this report.
The Armstrong deposit is one of a series of nickel deposits located on the tenements acquired by
Neometals. A summary of geology, mineralisation, estimation methodology, drill information, drill
intercepts and JORC Code (2012 Edition) Table 1 is provided here and in Appendices 1 to 5. The Mineral
Resource estimate for the Armstrong deposit is set out below:
For
per
sona
l use
onl
y
Mineral Resources Metal Grade Contained Metal
Category Cut off Tonnage Nickel Arsenic Copper Nickel Arsenic Copper
(Ni %) (Kt) (%) (ppm) (ppm) (t) (t) (t)
Measured 1 7 2.11 506 1757 139 3 12
Indicated 1 279 2.32 371 1849 6465 103 515
Inferred 1 29 4.91 11644 2348 1412 335 68
Total 1 314 2.56 1406 1893 8038 441 594
The Armstrong deposit nickel mineralisation is hosted by talc‐chlorite‐carbonate altered ultramafics
and typically has a pyrrhotite + pentlandite + pyrite +/‐ chalcopyrite assemblage. The mineralisation
dips about 45 degrees west and plunges to the north west at around 25 degrees.
The Mineral Resource estimate is based on a nominal 1.0% Ni wireframe cut‐off with a maximum
internal dilution of two metres. Grade was interpolated using a combination of inverse distance
weighting squared (IDW2), Surpac Block Maths and direct assignment techniques using Surpac
software.
Bulk density was interpolated using inverse distance squared utilising 3 expanding passes. After 3
passes unfilled blocks were assigned using a regression (sg = Ni X 0.0533 + 2.7878).
Drill data, interpretations and models are in GDA94 coordinates.
Mineral Resource classification was determined on the basis of geological continuity and confidence,
the number of drill hole intersections, and average distance to samples, as follows:
All domains and blocks defined by a single drill hole were assigned as unclassified and not included in the Mineral Resource estimate.
Areas where the nominal drill hole spacing was greater than 25m x 25m or where geological continuity and confidence where low were classified as Inferred Mineral Resource.
Areas where the nominal drill hole spacing approached 25 x 25m or where geological continuity and confidence were high were classified as an Indicated Mineral Resource.
Areas that surfaced in the Armstrong open pit operation and where geological confidence was high were classified as Measured Resource.
Resources above the base of supergene sulphide (completely weathered) were assigned as unclassified irrespective of geology or the drill hole spacing. This is due to the uncertainties relating to mineralogy and processing routes. Classifying this material as unclassified has the effect of excluding it from the Mineral Resource estimate and any further economic evaluations.
Nickel mineralisation and arsenic values were validated by northing and RL versus the domain composites from the drill hole database. The estimated mineralisation displays a very good correlation between the drill hole composites and the grade estimated from the block model. Filling of the Ni grades in the block model behaved as expected and the graphs display an averaging effect of the high and low values within the drill hole data. F
or p
erso
nal u
se o
nly
Long section, Armstrong: showing mineralisation domains (looking west)
Cross Section, Armstrong deposit: 6522150mN showing pit and mineralisation domains
Plan view, Armstrong deposit: showing drill holes and nickel mineralisation domains
For
per
sona
l use
onl
y
Cooke deposit Mineral Resource
An interrogation and review of the Mineral Resource estimates for the Cooke deposit previously
evaluated by Titan Resources Limited in compliance with the JORC Code (2004 Edition) has resulted
in restatement of the Mineral Resource estimate by Neometals in accordance with the JORC Code
(2012 Edition). There are minor changes to the tonnage, grade and classifications but these are
considered immaterial in the context of this report.
The Cooke deposit is one of a series of nickel deposits located on the tenements acquired by
Neometals. A summary of geology, mineralisation, estimation methodology, drill information, drill
intercepts and JORC Code (2012 Edition) Table 1 is provided here and in Appendix 1 to 5. The Mineral
Resource estimate for the Cooke deposit is set out below:
Mineral Resources Metal Grade Contained Metal
Category Cut off Tonnage Nickel Arsenic Nickel Arsenic
(Ni %) (Kt) (%) (ppm) (t) (t)
Inferred 1 154 1.3 801 2003 123
Total 1 154 1.3 801 2003 123
The Cooke deposit nickel sulphide mineralisation is developed on and above an ultramafic‐mafic
contact and has a steep northerly plunging syncline structure. The syncline dips steeply east and both
east and west limbs contain nickel mineralisation.
The Mineral Resource estimate is based on a nominal 1.0% Ni wireframe cut‐off with a maximum
internal dilution of two metres. Grade was interpolated using a combination of, ordinary kriging and
inverse distance squared using Micromine software.
Bulk density was derived from WMC’s historical regression where Bulk density (t/m3) =
167.0654/(57.6714 – Ni%).
Mineral Resource classification was determined on the basis of geological continuity, confidence, and
the number of drill hole intersections. The basis was as follows:
No QAQC data was available for the historical drilling that made up the bulk of the data. Only the Titan Resources Limited drilling had QAQC data
All domains and blocks defined by less than three drill holes were assigned as unclassified and not included in the Mineral Resource estimate
Areas where the nominal drill hole spacing approached 30 x 15m or better, were classified as Inferred Mineral Resource
Oxidised resources as defined by Hellman & Schofield (2005) were assigned as unclassified irrespective of geology or the drill hole spacing. This is due to the uncertainties relating to mineralogy and processing routes. Classifying this material as unclassified has the effect of excluding it from the Mineral Resource estimate and any further conomic evaluations.
As a result of points 1 to 4 above only blocks classified as Inferred Mineral Resource were included in this Mineral Resource estimate
The block model was validated by viewing in vertical section and plan and comparing to the samples.
Declustered sample grades were compared to the resource model block grades.
For
per
sona
l use
onl
y
Long section, Cooke deposit: showing mineralisation domains (looking west)
Cross Section, Cooke deposit: 6519850mN showing drilling and mineralisation domains
For
per
sona
l use
onl
y
Plan view, Cooke deposit: showing drill holes and nickel mineralisation domains
Hellman & Schofield (2005) on behalf of Titan Resources Limited completed an unpublished Mineral
Resource estimate for the Cooke resource in September 2005 in compliance with the JORC Code (2004
Edition). This estimate differed from previous models in that all oxide and sulphide resources were re‐
interpreted and interpolated.
A detailed review and interrogation of the September 2005 Mineral Resource estimate was completed
to determine if any further work was required to generate an updated Mineral Resource estimate in
compliance with the JORC Code (2012 Edition). Data, interpretations and methodologies were all
found to be of a reasonable standard and it was determined that no further work was necessary to
report the Mineral Resource estimate in compliance with the JORC Code (2012 Edition), although the
classifications and reporting methods in some areas of the model were changed.
It should be noted that re‐interpretation of the wireframes and re‐estimation of the Mineral Resource
are recommended before any future economic evaluations are completed on the project.
Zabel deposit and McEwen deposits Mineral Resource
An interrogation and review of the Mineral Resource estimates for the Zabel deposit and the McEwen
deposits previously evaluated by Australian Nickel Mines NL in compliance with the JORC Code (2004
Edition) has resulted in restatement of the Mineral Resource estimate by Neometals in accordance
with the JORC Code (2012 Edition). There are minor changes to the tonnage, grade and classifications
but these are considered immaterial in the context of this report.
The Zabel deposit and McEwen deposits are part of a series of nickel deposits located on the
tenements acquired by Neometals. A summary of geology, mineralisation, estimation methodology,
drill information, drill intercepts, and JORC Code (2012 Edition) Table 1 are provided here and in
Appendices 1 to 5. The JORC 2012 Mineral Resource statement estimate for the Zabel deposit and the
McEwen deposits are set out below:
For
per
sona
l use
onl
y
Zabel Mineral Resource Estimate
Mineral Resources Metal Grade Contained Metal
Category Cut off Tonnage Nickel Arsenic Nickel Arsenic (Ni %) (Kt) (%) (ppm) (t) (t)
Inferred 1.0 333 1.75 399 5812 133 Total 1.0 333 1.75 399 5812 133
McEwen Mineral Resource Estimate
Mineral Resources Metal Grade Contained Metal
Category Cut off Tonnage Nickel Arsenic Nickel Arsenic (Ni %) (Kt) (%) (ppm) (t) (t)
Inferred 1.0 1068 1.25 253 13340 270 Total 1.0 1068 1.25 253 13340 270
McEwen Hangingwall Mineral Resource Estimate
Resources Metal Grade Contained Metal
Category Cut off Tonnage Nickel Arsenic Nickel Arsenic (Ni %) (Kt) (%) (ppm) (t) (t)
Inferred 1.0 1058 1.40 4 14782 4 Total 1.0 1058 1.40 4 14782 4
Mineralisation at the Zabel deposit and McEwen deposits is interpreted to be structurally modified
“Kambalda Style” nickel occurrence. The mineralisation is essentially draped over the hinge of a gently
north plunging tight anticlinal structure. Mineralisation is generally parallel to the basal contact of the
ultramafic package, so the geometry is controlled by which part of the anticline the mineralisation
occurs. Mineralisation occurs as basal contact massive and stringer mineralisation as well as hanging‐
wall disseminated mineralisation higher up in the ultramafic sequence.
The Mineral Resource estimate is based on a nominal 0.5% Ni wireframe cut‐off with a maximum
internal dilution of two metres. Grade was interpolated using ordinary kriging, Surpac Block Maths
and direct assignment techniques using Surpac software.
Statistics and a regression were completed between nickel and specific gravity measurements. That
work was also used as the basis for specific gravity measurements in the current model. SGs were
assigned to fresh mineralised material in the block model using the formula (Ni * 0.152) + 2.911.
Drill data, interpretations and models are in AMG84 Coordinates.
Mineral Resource classification was determined on the basis of geological continuity and confidence
in the methodology used in the estimation of the Mineral Resource in accordance with the JORC Code
(2004 Edition) as follows:
Given the thin and structurally complex nature of the mineralisation and resulting uncertainties around the interpretation and grade estimation techniques applied, all blocks were assigned Inferred Mineral Resource classification
Resources above the base of supergene sulphide (completely weathered) were assigned as unclassified irrespective of geology or the drill hole spacing. This is due to the uncertainties relating to mineralogy and processing routes. Classifying this material as unclassified has the effect of excluding it from the Mineral Resource estimate and any further economic evaluations.
For
per
sona
l use
onl
y
A small number of blocks were not assigned grades in the block model. These were assigned as unclassified and not included in the Mineral Resource estimate
The block model was validated visually in vertical section and plan, comparing the samples and block estimates. The validation process compared block grades to input data to ensure that grade trends were reproduced. As expected the model represents a smoothed version of the original samples, without the strong local variability present in the sample data. Grade trends within the various domains are aligned with the orientations of the various search neighbourhoods.
Long section (oblique), Zabel deposit to McEwen deposits: showing mineralisation domains and basalt contact
Cross Section, McEwen deposits: showing drilling and mineralisation domains & basalt contact
For
per
sona
l use
onl
y
Plan view, Zabel deposit to McEwen desposits ‐ Plan view of the drill holes and nickel mineralisation domains
Hellman & Schofield completed a Mineral Resource estimate for the Zabel deposit and McEwen
deposits in September 2005 in accordance with the JORC Code (2004 Edition). An internal company
update was completed by Australian Nickel Mines NL in August 2006 due to errors in the SG
calculations by Hellman & Schofield.
A detailed review and interrogation of the August 2006 Mineral Resource estimate was completed to
determine if any further work was required to generate an updated Mineral Resource estimate in
compliance with the JORC Code (2012 Edition). Data, interpretations and methodologies were all
found to be of a reasonable standard and it was determined that no further work was necessary to
report the Mineral Resource in compliance with the JORC Code (2012 Edition), although the
classifications and reporting methods in some areas of the model were changed.
It should be noted that re‐interpretation of the wireframes and re‐estimation of the Mineral Resource
are recommended before any future economic evaluations are completed on the project.
For
per
sona
l use
onl
y
Appendix 3 – JORC Code (2012 Edition) Drill hole Location Information
132N deposit
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
ART5000Z DDH 6519093.17 361109.6 392.89 240 359.53 ‐90
RCGC_132N_001 RC 6518949.983 361182.609 359.528 55 270 ‐60
RCGC_132N_002 RC 6518790.168 361156.58 360.064 50 90 ‐50
RCGC_132N_003 RC 6518790.172 361168.42 360.144 35 94.48 ‐48.41
RCGC_132N_004 RC 6518799.596 361168.618 360.151 36 100.56 ‐60.82
RCGC_132N_006 RC 6518810.162 361172.219 360.041 50 90 ‐60
RCGC_132N_007 RC 6518809.974 361177.322 360.254 42 92.53 ‐58.5
RCGC_132N_008 RC 6518819.925 361166.417 359.336 40 90 ‐50.79
RCGC_132N_009 RC 6518820.008 361173.043 359.433 30 90 ‐50
RCGC_132N_010 RC 6518820.101 361180.77 359.859 20 90 ‐50
RCGC_132N_011 RC 6518830.014 361147.056 360.235 68 90 ‐60
RCGC_132N_012 RC 6518829.509 361157.966 359.403 62 90 ‐60
RCGC_132N_013 RC 6518830.047 361177.164 359.414 40 84.74 ‐59.66
RCGC_132N_014 RC 6518830.288 361184.806 359.716 25 79.96 ‐59.3
RCGC_132N_015 RC 6518840.067 361162.408 359.268 65 94.18 ‐59.89
RCGC_132N_016 RC 6518840.052 361168.653 359.291 60 87.62 ‐58.58
RCGC_132N_017 RC 6518840.039 361180.283 359.525 45 92.89 ‐59.06
RCGC_132N_018 RC 6518850.23 361153.12 359.732 62 90 ‐60
RCGC_132N_019 RC 6518849.974 361188.534 359.742 25 270 ‐50
RCGC_132N_020 RC 6518850.02 361201.788 359.733 50 270 ‐50
RCGC_132N_021 RC 6518859.909 361163.366 359.728 45 87.19 ‐59.15
RCGC_132N_022 RC 6518860.579 361169.353 359.933 38 90 ‐60
RCGC_132N_023 RC 6518859.959 361176.257 359.911 24 89.75 ‐58.81
RCGC_132N_024 RC 6518870.343 361149.158 360.085 62 90 ‐58
RCGC_132N_025 RC 6518869.943 361170.943 359.795 33 110.81 ‐58.19
RCGC_132N_025A RC 6518869.935 361170.88 359.789 33 90 ‐60
RCGC_132N_026 RC 6518879.802 361153.24 359.833 60 90 ‐60
RCGC_132N_027 RC 6518879.773 361160.965 359.927 52 91.97 ‐60.74
RCGC_132N_028 RC 6518879.921 361167.138 359.952 40 90 ‐60
RCGC_132N_029 RC 6518880.008 361172.043 359.933 27 95.1 ‐59.82
RCGC_132N_030 RC 6518880.122 361177.121 359.956 22 93.88 ‐60.47
RCGC_132N_031 RC 6518890.099 361149.944 359.913 69 86.82 ‐60.87
RCGC_132N_032 RC 6518890.155 361156.98 359.962 60 89.48 ‐60.08
RCGC_132N_033 RC 6518889.965 361181.892 360.017 43 271.31 ‐59.86
RCGC_132N_034 RC 6518889.915 361187.59 360.046 32 270.86 ‐59.93
RCGC_132N_035 RC 6518899.828 361147.767 360.005 65 94.47 ‐59.33
RCGC_132N_036 RC 6518910.126 361137.436 359.966 63 90 ‐60
RCGC_132N_037 RC 6518909.962 361144.14 360.015 55 90 ‐60
RCGC_132N_038 RC 6518910.226 361148.439 360.251 45 85.75 ‐60.66
RCGC_132N_039 RC 6518909.999 361154.354 360.182 35 90.93 ‐58.21
RCGC_132N_040 RC 6518909.882 361163.104 360.102 20 265.58 ‐60.67
RCGC_132N_040A RC 6518909.872 361162.943 360.003 20 90 ‐60
RCGC_132N_041 RC 6518920.239 361136.898 360.071 57 90.99 ‐48.43
RCGC_132N_041A RC 6518920.344 361137.045 360.142 57 90 ‐51
RCGC_132N_042 RC 6518919.972 361155.371 360.496 40 90 ‐61
RCGC_132N_043 RC 6518920.203 361160.072 360.422 22 88.11 ‐60.7
RCGC_132N_044 RC 6518930.172 361151.491 360.515 35 90 ‐60
RCGC_132N_045 RC 6518929.879 361188.847 359.934 65 266.37 ‐57.95
RCGC_132N_047 RC 6518939.943 361188.969 359.434 68 270 ‐62
RCGC_132N_048 RC 6518939.407 361145.132 360.597 45 90 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
RCGC_132N_049 RC 6518949.981 361196.902 359.639 82 270.28 ‐69.2
RCGC_132N_050 RC 6518949.985 361171.051 360.532 36 270 ‐60
RCGC_132N_051 RC 6518959.892 361144.425 362.651 35 91.21 ‐61.29
RCGC_132N_052 RC 6518960.053 361174.032 360.564 42 264.22 ‐58.15
RCGC_132N_053 RC 6518970.423 361145.721 362.507 35 67.47 ‐57.05
RCGC_132N_059 RC 6518810.102 361174.245 360.136 36 90 ‐60
RCGC_132N_060 RC 6518819.955 361157.146 359.714 58 90 ‐60
WD1010A PERC 6519017.1 361221.21 372.89 34 259.53 ‐45
WD10518 PERC 6519342.9 360927.8 376.69 60.96 359.53 ‐90
WD3298 PERC 6519213.79 361099.06 388.89 21.34 359.53 ‐90
WD3304 DDH 6518775.51 361139 382.25 131.98 80.53 ‐45
WD3305 DDH 6519009.593 361048.337 372.542 206.35 80.53 ‐46
WD3306 DDH 6518908.1 361106.12 374.7 149.66 80.53 ‐45
WD3311 DDH 6519009.05 361045.7 372.07 208.97 80.53 ‐65
WD3313 DDH 6518970.389 361198.545 379.416 240.49 260.53 ‐45
WD3317 DDH 6518992.45 361115.43 374.61 124.36 260.53 ‐89.5
WD3321 DDH 6518997.61 361099.43 378.69 127.1 260.53 ‐89.8
WD3323 DDH 6518995 361156 381.69 178.61 260.53 ‐89.9
WD3326 PERC 6519052.832 361120.334 378.281 39.62 359.53 ‐90
WD3327 PERC 6519048.328 361094.101 375.463 121.92 359.53 ‐90
WD3328 PERC 6518992.61 361069.36 375.89 30.48 359.53 ‐90
WD3329 PERC 6518997.61 361099.43 378.69 38.1 359.53 ‐90
WD3330 PERC 6519002.6 361129.49 380.79 120.4 359.53 ‐90
WD3331 PERC 6518973.29 361138.99 379.29 103.63 359.53 ‐90
WD3332 PERC 6519032.17 361121.49 381.79 118.87 359.53 ‐90
WD3333 PERC 6518887.84 361182.53 381.29 41.15 359.53 ‐90
WD3334 PERC 6518903.77 361166.41 374.97 83.21 359.53 ‐90
WD3335 PERC 6518944.72 361153 378.89 25.91 359.53 ‐90
WD3336 PERC 6519002.6 361129.49 380.79 51.82 80.53 ‐60
WD3337 PERC 6518822.97 361163.95 384.49 39.62 80.53 ‐60
WD3431 PERC 6518709.56 361039.13 382.19 19.81 359.53 ‐90
WD3432 PERC 6518712.07 361054.16 381.89 22.86 359.53 ‐90
WD3433 PERC 6518714.56 361069.19 382.89 30.48 359.53 ‐90
WD3434 PERC 6518717.05 361084.22 384.89 32 359.53 ‐90
WD3444 PERC 6518935.09 360909 371.89 22.86 359.53 ‐90
WD3445 PERC 6518937.59 360924.04 371.89 25.91 359.53 ‐90
WD3812 PERC 6518735.02 361192.45 387.89 33.53 80.53 ‐50
WD3813 PERC 6518733.03 361180.43 387.89 42.67 80.53 ‐50
WD3840 DDH 6518726.04 361138.33 387.89 196.9 80.53 ‐45
WD3843 DDH 6518939.34 360934.56 371.89 336.8 80.53 ‐45
WD4113 DDH 6518980.206 361258.108 381.473 222.81 260.53 ‐55
WD4123 DDH 6519204.882 361081.637 380.168 13.72 359.53 ‐90
WD4126 DDH 6519100.213 361221.307 375.59 206.35 260.53 ‐50
WD4127 DDH 6518851.01 361238 374.89 120.4 260.53 ‐44
WD4133 DDH 6519103.509 361239.594 371.987 291.08 260.53 ‐65
WD4136 DDH 6518894.58 361048.24 372.34 221.59 80.53 ‐55
WD4138 DDH 6519167.988 361222.747 384.332 229.82 260.53 ‐60
WD4143 DDH 6519000.58 360990.89 370.39 284.68 80.53 ‐65
WD4146 DDH 6519232.918 361251.891 375.267 306.32 260.53 ‐65
WD4147 DDH 6519067.45 360940.9 368.15 318.21 80.53 ‐66
WD4148 DDH 6519010.481 361235.958 379.665 193.24 260.53 ‐55
WD4475 PERC 6518759.6 361154.38 389.89 22.86 80.53 ‐45
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WD4476 PERC 6518763.09 361175.43 391.39 32 80.53 ‐70
WD4477 PERC 6518767.09 361199.49 392.19 21.34 359.53 ‐90
WD4478 PERC 6518797.15 361194.49 389.49 38.71 359.53 ‐90
WD4479 PERC 6518828.71 361198.52 385.79 28.96 260.53 ‐55
WD4480 PERC 6518812.29 361186.57 380.56 30.48 359.53 ‐90
WD4481 PERC 6518858.77 361193.53 383.19 32.61 260.53 ‐60
WD4482 PERC 6518844.65 361180.74 376.92 24.38 359.53 ‐90
WD4483 PERC 6518886.59 361175.01 380.69 30.48 80.53 ‐50
WD4484 PERC 6518886.59 361175.01 380.69 18.29 260.53 ‐50
WD4485 PERC 6518904.74 361181.88 376.44 42.67 260.53 ‐50
WD4486 PERC 6518947.46 361169.54 380.89 35.66 260.53 ‐50
WD4487 PERC 6519166.5 361000.33 377.19 27.43 80.53 ‐60
WD4488 PERC 6519155.5 361004.66 372.63 30.48 260.53 ‐60
WD4489 PERC 6519160.29 361068.63 378.32 30.48 80.53 ‐60
WD4490 PERC 6518943.72 361146.99 378.59 12.19 260.53 ‐55
WD4491 PERC 6518856.28 361178.5 381.69 27.43 359.53 ‐90
WD4492 PERC 6518858.27 361190.52 382.89 24.38 359.53 ‐90
WD4493 PERC 6518857.78 361187.51 382.59 27.43 359.53 ‐90
WD4494 PERC 6518856.78 361181.5 382.09 33.53 359.53 ‐90
WD4495 PERC 6518855.78 361175.49 381.39 21.34 359.53 ‐90
WD4839 PERC 6519000.1 361114.46 379.59 86.87 359.53 ‐90
WD4840 PERC 6519005.09 361144.52 381.59 37.8 359.53 ‐90
WD4892 PERC 6519204.18 361066.05 378.52 45.72 359.53 ‐90
WD4893 PERC 6519087.55 361082.95 380.89 33.53 359.53 ‐90
WD4894 PERC 6519091.04 361104 382.89 42.67 359.53 ‐90
WD4895 PERC 6519094.79 361126.55 385.89 29.57 359.53 ‐90
WD4948 PERC 6518990.12 361054.33 375.39 47.24 359.53 ‐90
WD4949 PERC 6518995.1 361084.4 376.99 38.1 359.53 ‐90
WD4950 PERC 6519005.34 361146.03 381.69 47.24 359.53 ‐90
WD4971 DDH 6519090.29 361099.48 382.39 276.45 89.53 ‐89.5
WD4971Z DDH 6519090.29 361099.48 382.39 276.45 27.4 ‐89.45
WD4974 PERC 6519081.61 361067.13 375.77 24.38 359.53 ‐90
WD4979 PERC 6519094.03 361122.03 384.89 30.48 359.53 ‐90
WD4980 PERC 6519077.55 361037.64 373.82 15.24 359.53 ‐90
WD4981 PERC 6519071.97 361010.8 372.15 21.34 359.53 ‐90
WD4982 PERC 6519189.3 360994.44 372.68 12.19 359.53 ‐90
WD4983 PERC 6519194.821 361020.74 375.561 33.53 359.53 ‐90
WD4984 PERC 6519199.68 361051.63 377.73 19.81 359.53 ‐90
WD4985 PERC 6519208.61 361110.03 384.63 15.24 359.53 ‐90
WD5301 DDH 6519069 361239 372.89 248.11 260.53 ‐63
WD5303 DDH 6518945.359 361248.907 381.913 159.72 260.53 ‐51
WD5305 DDH 6518879.705 361241.408 379.989 177.7 261 ‐60
WD5308 DDH 6519175.31 361261.808 382.033 360.88 260.53 ‐66
WD5309 DDH 6519080 361302 365.89 452.63 260.53 ‐70
WD5311 DDH 6518937.889 361195.987 379.232 105.46 260.53 ‐50
WD5316 DDH 6519139.739 361252.649 375.544 321.26 260.53 ‐65
WD5317 DDH 6519062.803 361212.008 374.203 209.4 260.53 ‐60
WD5320 DDH 6519122.226 361178.478 384.632 205.44 260.53 ‐70
WD5322 DDH 6519237.63 361287.25 376.89 375.21 260.53 ‐65
WD5322W1 DDH 6519237.63 361287.25 376.89 473.66 260.53 ‐65
WD5324 DDH 6518952.825 361302.829 377.161 227.69 260.53 ‐51
WD5331 DDH 6518824.34 361242.16 379.51 119.48 260.53 ‐47
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WD5333 DDH 6519019.44 361295.12 375.88 321.87 260.53 ‐60.5
WD5334 DDH 6519242.844 361314.469 369.617 275.84 260.53 ‐75
WD5345 DDH 6519171.245 361240.805 383.505 298.7 260.53 ‐60
WD5456 PERC 6518706.96 361209.47 396.49 9.14 80.53 ‐70
WD5457 PERC 6518707.96 361215.48 396.89 15.24 359.53 ‐90
WD5458 PERC 6518705.96 361203.46 395.79 15.24 359.53 ‐90
WD5459 PERC 6518690.93 361205.95 396.89 12.19 359.53 ‐90
WD5460 PERC 6518689.93 361199.94 396.59 4.57 359.53 ‐90
WD5461 PERC 6518691.93 361211.96 397.09 15.24 359.53 ‐90
WD5462 PERC 6518692.93 361217.97 397.49 13.72 359.53 ‐90
WD5806 DDH 6518850.26 361268.78 374.89 190.5 260.53 ‐49
WD5816 DDH 6519109.922 361274.746 368.785 418.8 260.53 ‐65
WD5817 DDH 6519179.696 361284.31 378.07 82.3 260.53 ‐67
WDC289 RC 6518831.884 361155.75 378.327 90 88.1 ‐60.4
WDC290 RC 6518980.194 361118.715 371.335 80 91.16 ‐60.49
WDC292 RC 6518910.094 361150.737 373.875 70 89.82 ‐59.91
WDC293 RC 6518965.428 361127.39 371.387 95 89.82 ‐59.58
WDC297 RC 6518825.108 361103.679 376.501 132 90 ‐50
WDC298 RC 6518830.284 361158.672 378.43 75 90 ‐50
WDC299 RC 6518824.637 361136.914 378.41 96 90 ‐50
WDC300 RC 6518810.13 361137.263 379.396 90 90.4 ‐55
WDC301 RC 6518809.767 361135.73 381.492 108 90 ‐58
WDC302 RC 6518862.489 361163.115 375.665 60 90 ‐60
WDC303 RC 6518848.77 361222.139 382.109 120 257 ‐60
WDC304 RC 6519012.075 361139.555 377.782 132 279.52 ‐82.31
WDC305 RC 6518949.752 361131.397 371.703 102 90 ‐58
WDC306 RC 6518849.459 361164.936 379.122 70 90 ‐60
WDC307 RC 6518862.422 361132.011 375.192 96 90 ‐60
WDC308 RC 6518862.425 361130.319 377.306 66 90 ‐66
WDC309 RC 6518924.38 361140.979 372.116 70 90 ‐56
WDC310 RC 6518863.223 361173.43 377.845 36 90 ‐60
WDC311 RC 6518865.082 361130.302 377.189 120 94.4 ‐66
WDC312 RC 6518875.493 361179.433 377.918 36 90 ‐60
WDC313 RC 6518875.281 361171.633 377.366 42 90 ‐60
WDC314 RC 6518887.227 361171.646 377.524 46 90 ‐60
WDC315 RC 6518950.179 361147.4 372.158 54 90 ‐60
WDC316 RC 6518962.379 361133.804 371.418 54 90 ‐60
WDC317 RC 6518962.373 361143.097 372.024 36 90 ‐60
WDC318 RC 6518974.481 361125.168 371.358 76 90 ‐60
WDC319 RC 6518974.506 361137.44 371.977 42 90 ‐60
WDD102 DDH 6518949.809 361124.721 371.537 94.12 90.57 ‐59.96
WDD103 DDH 6518857.276 361140.631 375.767 100.12 89.28 ‐59.51
WDD104 DDH 6518925.123 361114.673 371.689 111.43 88 ‐60.75
WDD105 DDH 6518820.711 361141.486 378.872 81.5 87.44 ‐50.78
WDD106 DDH 6518942.91 361109.844 370.929 114.5 88.47 ‐60.22
WDD107 DDH 6518952.014 361087.361 370.64 154 89.41 ‐60.27
WDD115 DDH 6518935.166 361137.112 372.052 86 91.22 ‐60.95
WDD116 DDH 6519060.261 361204.195 374.134 210 269.02 ‐58.06
WDD117 DDH 6518959.991 361035.576 369.642 250 91.22 ‐58.7
WDD118 DDH 6518914.979 361020.76 369.733 262 91.02 ‐60.14
WDD141 DDH 6518854.477 361132.847 375.927 105.4 90 ‐60
WDD142 DDH 6518810.063 361132.008 379.145 108 90 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WDD147 DDH 6518824.774 361136.168 378.296 111 90 ‐58
WDD148 DDH 6518845.616 361152.235 379.046 91.2 89.77 ‐60.11
WDD149 DDH 6518912.278 361122.965 372.732 105 90.4 ‐60
WDD150 DDH 6518912.379 361103.123 372.026 137.7 90 ‐60
WDD151 DDH 6518937.34 361102.564 370.912 162.04 90 ‐64
WDD152 DDH 6518962.308 361106.733 371.029 126 90 ‐60
WDD153 DDH 6518887.389 361162.759 376.825 72 94.12 ‐70.54
WDD154 DDH 6518874.764 361157.06 376.908 68.8 90.31 ‐60.73
WDD155 DDH 6518887.15 361132.264 373.741 105 94.34 ‐60.15
WDD156 DDH 6518899.755 361153.513 374.427 66.1 90.89 ‐60.36
WDD157 DDH 6518899.735 361144.896 373.976 69 90 ‐60
WDD158 DDH 6518962.324 361086.644 370.416 150 90 ‐60
WDD159 DDH 6519037.846 361070.224 373.909 192.15 90 ‐67
WDD160 DDH 6518874.919 361121.564 374.058 108 90.75 ‐59.94
WDD160S DDH 6518795.996 361161.458 361.105 61.9 93.5 ‐48.7
WDD161 DDH 6518795.996 361161.468 361.107 53.52 78.5 ‐57.4
WDD162 DDH 6518814.161 361172.084 365.684 41.8 91.7 ‐66.2
WID1005 DDH 6518890.3 361080.63 371.56 181 82.53 ‐55
WID1007 DDH 6518911.34 361225.223 380.776 172.3 259.53 ‐57
WID1008 DDH 6519022.295 361297.123 376.059 247 260.53 ‐54.8
WID1009 DDH 6519071.678 361265.642 367.384 236.23 259.53 ‐49
WID1010 DDH 6519008.681 361222.744 379.981 13 259.53 ‐45
WID1010A DDH 6519008.842 361224.791 379.924 225 254.53 ‐45
WID1280 RC 6518842.81 361164.74 377.02 80 89.53 ‐60
WID1281 RC 6518802.4 361149.72 381.63 34 89.53 ‐60
WID1281A RC 6518802.06 361153.34 381.42 90 89.53 ‐60
WID1282 RC 6518809.34 361165.71 381.15 50 89.53 ‐60
WID1283 RC 6518781.89 361156.54 383.7 80 89.53 ‐60
WID1284 RC 6518783.2 361173.79 384.76 50 89.53 ‐60
WID1285 RC 6518757.89 361176.66 386.68 50 89.53 ‐60
WID1317 RC 6518842.075 361143.708 377.216 70 89.53 ‐60
WID1317A RC 6518841.69 361146.12 377.37 88 89.53 ‐60
WID1318 RC 6518849.26 361123.99 375.76 120 89.53 ‐60
WID1319 RC 6518846.666 361103.646 374.943 150 84.5 ‐59.23
WID1320 RC 6518804.247 361139.826 380.285 94 89.53 ‐60
WID1321 RC 6518805.05 361129.39 379.59 80 89.53 ‐60
WID1322 RC 6518754.47 361182.74 387.21 50 89.53 ‐60
WID1323 RC 6518764.57 361171.4 386.02 50 89.53 ‐60
WID1323A RC 6518764.58 361171.37 386.24 80 89.53 ‐60
WID1324 RC 6518725.58 361168.88 386.33 60 90 ‐60
WID1350 RC 6518872.83 361128.09 374.25 90 89.53 ‐60
WID1351 RC 6518871.83 361137.86 374.59 78 89.53 ‐60
WID1352 RC 6518870.94 361148.12 374.9 64 89.53 ‐60
WID1353 RC 6518783.89 361187.47 385.17 40 89.53 ‐60
WID1355 RC 6518724.14 361169.77 386.37 70 89.53 ‐60
WID1356 RC 6518722.79 361179.43 387.4 54 89.53 ‐60
WID1357 RC 6518722 361187.29 388.2 40 89.53 ‐60
WID1358 RC 6518709.81 361171.21 386.49 70 89.53 ‐60
WID1359 RC 6518709.5 361180 387.63 55 89.53 ‐60
WID1360 RC 6518709.79 361188.22 388.61 40 89.53 ‐60
WID1361 RC 6518753.63 361188.73 387.45 39 89.53 ‐60
WID1362 RC 6518961.25 361149.15 375.59 30 89.53 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID1392 RAB 6518736.87 361188.52 387.89 55 89.53 ‐60
WID1393 RAB 6518736.87 361188.52 387.89 44.5 89.53 ‐45
WID1419 DDH 6519146.631 361137.734 386.461 235.1 281 ‐70.2
WID1421 DDH 6519024.795 361129.661 377.628 110 89.53 ‐62.5
WID1561 DDH 6518816.378 361121.482 378.222 100 89.53 ‐49
WID1562 DDH 6518816.336 361121.864 378.262 105 89.53 ‐52
WID1564 DDH 6518836.425 361123.775 376.8 111 89.53 ‐54
WID1565 DDH 6518836.468 361124.022 376.808 116 90.9 ‐57.12
WID1566 DDH 6518836.451 361124.396 376.861 105 90.1 ‐50.12
WID1595 DDH 6518846.468 361141.111 376.91 115 89.53 ‐50
WID1596 DDH 6518867.437 361274.23 376.559 196 269.53 ‐49.5
WID1597 DDH 6518896.209 361131.842 373.666 91 89.53 ‐60
WID1598 PERC 6518887.045 361245.817 378.432 33 269.53 ‐50
WID1599 DDH 6518887.41 361257.247 377.783 175 269.53 ‐50
WID1959 RC 6518834.303 361161.313 378.003 80 89.53 ‐60
WID1960 RC 6518859.297 361152.156 376.05 80 89.53 ‐60
WID1961 RC 6518881.16 361136.5 373.92 84 89.53 ‐60
WID1962 RC 6518886.47 361151.981 374.348 72 89.53 ‐60
WID1963 RC 6518902.395 361137.207 373.714 80 89.53 ‐60
WID1964 DDH 6519053.66 361004.91 371.07 276 89.53 ‐55
WID1965 DDH 6519136.774 360978.98 370.638 286.1 89.53 ‐60
WID1966 DDH 6519005.1 361010.98 371.05 231 92.53 ‐45.8
WID1967 DDH 6518987.966 361100.233 370.889 202 80.53 ‐64.7
WID1968 DDH 6518956.23 361090.45 370.6 143.6 89.53 ‐45.8
WID1969 RC 6518839.177 361176.627 377.687 60 89.53 ‐60
WID1970 RC 6518864.924 361166.608 375.658 60 71.5 ‐59.64
WID1971 RC 6518887.67 361153.42 374.89 80 84.1 ‐59.73
WID1972 RC 6518902.37 361163.84 374.32 60 89.53 ‐60
WID1973 RC 6518927.842 361131.176 371.849 100 89.53 ‐60
WID1974 DDH 6518931.12 361064.6 373.26 244.9 89.53 ‐58
WID1975 RC 6519064.588 361110.357 377.779 64 79.2 ‐57.09
WID1976 RC 6519144.739 361063.64 378.199 64 89.53 ‐55
WID1977 RC 6519235.424 361060.902 376.476 70 89.53 ‐55
WID1978 RC 6519302.679 361026.455 378.626 106 89.53 ‐55
WID1979 RC 6519385.79 361008.02 373 126 89.53 ‐55
WID2601 DDH 6518935.433 361043.631 370.056 240.1 89.53 ‐60
WID2923 DDH 6518911.19 361080.08 371.36 186 89.53 ‐65
WID2924 DDH 6518911.086 361080.051 371.26 230 88.53 ‐72.8
WID2925 DDH 6518935.71 361100.856 370.937 135 93.53 ‐61
WID2926 DDH 6518976.573 361065.122 370.123 197 92.53 ‐66
WID2927 DDH 6519074.631 361019.201 373.055 229 90 ‐60.93
WID2928 DDH 6519135.621 360924.322 367.839 360 89.53 ‐62
WID3029 DDH 6519074.631 361020.37 373.102 275.5 88.9 ‐72.27
WID3030 DDH 6518937.77 361143.39 374.73 76 89.53 ‐60
WID3031 DDH 6519001.646 361179.584 379.407 187 264.53 ‐67
WID3168 DDH 6518937.324 361018.573 369.318 263.6 89.53 ‐60
WID3169 DDH 6518872.033 361119.284 374.518 207 89.53 ‐71.5
WID3170 DDH 6518872.025 361118.825 374.574 213 89.53 ‐78
WID3171 DDH 6519075.303 361019.015 373.05 286 88.53 ‐66
WID3172 DDH 6519015.858 361038.747 372.663 250 89.53 ‐60
WID3289 DDH 6518977.252 361037.052 370.586 289.8 89.53 ‐69
WID3290 DDH 6518977.302 361037.381 370.583 240 89.53 ‐63
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID92 PERC 6518750.934 360955.622 373.775 2 359.53 ‐90
WID93 PERC 6518759.7 360969.02 377.89 4 359.53 ‐90
WID94 PERC 6518763.45 360991.56 377.89 3 359.53 ‐90
WID95 PERC 6518759.21 360966.01 377.89 4 359.53 ‐90
WID96 PERC 6518756.022 360972.902 373.727 16 359.53 ‐90
WID97 PERC 6518762.2 360984.05 377.89 16 359.53 ‐90
WID98 PERC 6518757.501 360979.836 373.902 22 359.53 ‐90
Armstrong deposit
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
AMB_1 PERC 6522519.99 360129.6 339.14 103 0 ‐90
AMB_2 PERC 6522075 359885 330 97 0 ‐90
AMB_3 PERC 6521934.81 360192.59 338.3 103 0 ‐90
AMB_4 PERC 6522220 359309 330 93 0 ‐90
AMB_5 PERC 6522459 360760 330 96 0 ‐90
Decline01 DDH 6521869.71 360395.75 336 45.5 165 ‐60
Decline02 DDH 6521964.62 360369.65 337 36.5 165.47 ‐59.87
Decline03 DDH 6522130.12 360326.26 337 58.3 166.08 ‐59.51
FAW DDH 6522179.42 360308.36 329 81 142.92 ‐89.42
PitWall01 DDH 6522284.14 360263.87 331 120.6 360 ‐90
PitWall02 DDH 6522204.13 360066.86 333 150.6 360 ‐90
PitWall03 DDH 6522008.13 360143.86 337 129.5 360 ‐90
Portal01 DDH 6521874.31 360383.75 339 29 74 ‐60
Portal02 DDH 6521882.41 360409.15 336 30.5 254 ‐60
RAW DDH 6522146.72 360266.05 330 71 8.03 ‐89.83
WD10 DDH 6522389.32 360133.19 333.56 106 79.53 ‐60
WD10541 DDH 6524113.98 359354.01 323.89 45.72 359.53 ‐90
WD10542 DDH 6524094.02 359233.76 324.39 45.72 359.53 ‐90
WD10543 DDH 6524096.51 359248.79 324.39 45.72 359.53 ‐90
WD10544 DDH 6524089.02 359203.69 324.89 28.96 359.53 ‐90
WD10545 DDH 6524066.56 359068.41 325.39 22.86 359.53 ‐90
WD10546 DDH 6524061.57 359038.34 325.39 21.34 359.53 ‐90
WD10560 DDH 6523622.98 359373.75 323.59 48.77 359.53 ‐90
WD10561 DDH 6523617.99 359343.69 323.79 57.91 359.53 ‐90
WD10562 DDH 6523612.99 359313.63 323.89 54.86 359.53 ‐90
WD10563 DDH 6523608 359283.56 324.09 54.86 359.53 ‐90
WD10564 DDH 6523603.01 359253.5 324.19 54.86 359.53 ‐90
WD10565 DDH 6523598.02 359223.43 324.29 57.91 359.53 ‐90
WD10566 DDH 6523593.03 359193.37 324.39 50.29 359.53 ‐90
WD10567 DDH 6523588.04 359163.3 324.59 51.82 359.53 ‐90
WD10568 DDH 6523568.07 359043.05 325.29 42.67 359.53 ‐90
WD10569 DDH 6523563.08 359012.99 325.49 36.58 359.53 ‐90
WD10570 DDH 6523558.08 358982.92 325.69 36.58 359.53 ‐90
WD10571 DDH 6523553.1 358952.87 325.89 42.67 359.53 ‐90
WD10572 DDH 6523548.1 358922.8 326.09 48.77 359.53 ‐90
WD10573 DDH 6523543.11 358892.74 326.29 54.86 359.53 ‐90
WD10574 DDH 6523538.11 358862.67 326.49 21.34 359.53 ‐90
WD11 DDH 6522504.79 360100.03 336 84 79.53 ‐60
WD12 DDH 6522734.57 359976.92 340.93 52 79.53 ‐60
WD13 DDH 6522851.09 359934.41 339.77 44 77.53 ‐60
WD14 DDH 6522964.1 359870.85 334.89 58 82.53 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WD15 DDH 6523080.37 359826.84 333.89 49 79.53 ‐60
WD16 DDH 6523020.24 359836.82 333.89 51 79.53 ‐60
WD17 DDH 6522906.22 359894.36 336.81 64 79.53 ‐60
WD18 DDH 6522792.21 359951.91 340.8 41 79.53 ‐60
WD19 DDH 6522674.45 359986.9 339.8 106 79.53 ‐60
WD3299 DDH 6524136.45 359489.3 323.09 54.86 359.53 ‐90
WD3300 DDH 6524143.94 359534.39 322.89 54.86 359.53 ‐90
WD3301 DDH 6523157.93 359549.83 327.99 306.32 80.53 ‐50
WD3314 DDH 6523103.77 359223.63 324.69 168.25 80.53 ‐47
WD3319 DDH 6522937.4 359710.01 331.69 202.39 80.53 ‐45
WD3844 DDH 6523186.14 359719.68 330.59 183.49 80.53 ‐47
WD4 DDH 6522153.98 360200.72 332.47 56 79.53 ‐60
WD4112 DDH 6521524.26 360130 349.89 203.91 80.53 ‐43
WD4117 DDH 6523291.73 360355.52 322.49 217.63 260.53 ‐55
WD4120 DDH 6523681.39 359725.5 321.29 89.31 260.53 ‐45
WD4125 DDH 6523684.39 359725 321.29 275.84 260.53 ‐47.5
WD4496 DDH 6523201.87 359814.38 331.09 24.38 359.53 ‐90
WD4497 DDH 6523199.37 359799.35 330.99 39.62 359.53 ‐90
WD4498 DDH 6523196.87 359784.32 330.89 39.62 359.53 ‐90
WD4499 DDH 6523194.38 359769.29 330.79 42.67 359.53 ‐90
WD4500 DDH 6523171.91 359634 329.39 39.62 359.53 ‐90
WD4701 DDH 6523169.42 359618.97 329.19 39.62 359.53 ‐90
WD4702 DDH 6523166.92 359603.94 328.89 42.67 359.53 ‐90
WD4703 DDH 6523174.41 359649.04 329.69 56.39 359.53 ‐90
WD4704 DDH 6523181.9 359694.13 330.29 45.72 359.53 ‐90
WD4705 DDH 6523184.39 359709.16 330.49 45.72 359.53 ‐90
WD4823 DDH 6523417.41 359624.13 326.09 38.1 359.53 ‐90
WD4824 DDH 6523419.91 359639.17 326.19 41.15 359.53 ‐90
WD4825 DDH 6523422.41 359654.2 326.19 39.62 359.53 ‐90
WD4826 DDH 6523447.37 359804.51 327.19 38.1 359.53 ‐90
WD4827 DDH 6523449.86 359819.55 327.09 45.11 359.53 ‐90
WD4828 DDH 6523452.36 359834.58 326.99 44.2 359.53 ‐90
WD4829 DDH 6522938.89 359719.03 330.53 22.86 359.53 ‐90
WD4830 DDH 6522941.39 359734.07 330.88 42.67 359.53 ‐90
WD4831 DDH 6522943.88 359749.09 331.18 38.1 359.53 ‐90
WD4832 DDH 6522958.86 359839.29 335.19 42.67 359.53 ‐90
WD4833 DDH 6522961.36 359854.32 335.89 36.58 359.53 ‐90
WD4834 DDH 6522963.85 359869.35 336.69 45.72 359.53 ‐90
WD4835 DDH 6523662.91 359614.26 321.09 60.96 359.53 ‐90
WD4836 DDH 6523665.42 359629.3 321.09 57.91 359.53 ‐90
WD4837 DDH 6523670.4 359659.35 321.19 60.96 359.53 ‐90
WD4838 DDH 6523675.4 359689.42 321.29 60.96 359.53 ‐90
WD4889 DDH 6521530.75 360169.09 351.09 39.62 359.53 ‐90
WD4890 DDH 6521533.25 360184.11 351.59 33.53 359.53 ‐90
WD4891 DDH 6521535.74 360199.15 351.99 42.67 359.53 ‐90
WD4907 DDH 6521538.24 360214.18 352.49 51.82 359.53 ‐90
WD4908 DDH 6521540.74 360229.2 352.89 42.67 359.53 ‐90
WD4909 DDH 6521543.23 360244.24 353.69 21.34 359.53 ‐90
WD4910 DDH 6521545.72 360259.27 354.49 39.62 359.53 ‐90
WD4911 DDH 6521548.23 360274.31 355.39 18.29 359.53 ‐90
WD4912 DDH 6521550.72 360289.34 355.89 19.81 359.53 ‐90
WD4957 DDH 6523680.39 359719.48 321.29 55.78 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WD4958 DDH 6523274.25 360250.31 325.09 28.96 359.53 ‐90
WD4959 DDH 6523276.75 360265.34 324.79 28.96 359.53 ‐90
WD4960 DDH 6523279.24 360280.37 324.39 32.92 359.53 ‐90
WD4961 DDH 6523281.74 360295.4 323.89 30.48 359.53 ‐90
WD4962 DDH 6523284.24 360310.43 323.39 28.96 359.53 ‐90
WD4963 DDH 6522896.46 359463.48 328 22.86 359.53 ‐90
WD4964 DDH 6522893.97 359448.46 328 21.34 359.53 ‐90
WD4965 DDH 6522891.46 359433.42 328.07 19.81 359.53 ‐90
WD4966 DDH 6522888.97 359418.39 328.25 16.76 359.53 ‐90
WD4969 DDH 6522886.48 359403.36 328.04 15.24 359.53 ‐90
WD4970 DDH 6522964.36 359853.82 335.89 48.77 359.53 ‐90
WD5 DDH 6522036.75 360239.52 334.13 76 359.53 ‐90
WD5101 DDH 6524138.94 359504.33 322.89 36.58 359.53 ‐90
WD5102 DDH 6524141.44 359519.36 322.89 60.96 359.53 ‐90
WD5132 DDH 6524133.95 359474.27 323.39 22.86 359.53 ‐90
WD5133 DDH 6524146.43 359549.43 322.39 45.72 359.53 ‐90
WD5134 DDH 6524148.92 359564.46 322.39 48.77 359.53 ‐90
WD5141 DDH 6523928.39 359724.64 321.79 51.82 359.53 ‐90
WD5142 DDH 6523893.44 359514.21 323.09 48.77 359.53 ‐90
WD5143 DDH 6523898.44 359544.26 322.89 15.24 359.53 ‐90
WD5144 DDH 6523903.43 359574.33 322.49 18.29 359.53 ‐90
WD5145 DDH 6523908.42 359604.39 322.19 16.76 359.53 ‐90
WD5146 DDH 6523913.41 359634.46 322.09 37.19 359.53 ‐90
WD5404 DDH 6521790.3 360150.7 343.89 45.72 359.53 ‐90
WD5405 DDH 6521787.79 360135.67 343.89 27.43 359.53 ‐90
WD5406 DDH 6521785.3 360120.63 343.89 48.77 359.53 ‐90
WD5412 DDH 6521828.9 360104.13 342.99 44.2 359.53 ‐90
WD5413 DDH 6521831.39 360119.16 342.89 15.24 359.53 ‐90
WD5414 DDH 6521833.64 360132.69 342.89 19.81 80.53 ‐80
WD5415 DDH 6521832.9 360128.18 342.89 32 80.53 ‐80
WD5416 DDH 6521836.39 360149.23 342.59 57.91 359.53 ‐90
WD5417 DDH 6521838.88 360164.26 342.49 53.34 359.53 ‐90
WD5418 DDH 6521786.8 360129.66 343.89 45.72 80.53 ‐80
WD5478 DDH 6523432.4 359714.33 326.09 42.67 359.53 ‐90
WD5479 DDH 6523434.89 359729.35 326.19 47.24 359.53 ‐90
WD5480 DDH 6523437.38 359744.39 326.39 36.58 359.53 ‐90
WD5481 DDH 6523439.88 359759.42 326.69 28.96 359.53 ‐90
WD5482 DDH 6523442.38 359774.45 326.99 38.1 359.53 ‐90
WD5607 DDH 6521708.65 360124.1 345.39 33.53 359.53 ‐90
WD5608 DDH 6521711.14 360139.13 345.49 33.53 359.53 ‐90
WD5609 DDH 6521713.64 360154.16 345.89 64.01 359.53 ‐90
WD5610 DDH 6521716.13 360169.2 346.09 41.15 359.53 ‐90
WD5611 DDH 6521889.03 360094.14 342.39 45.72 359.53 ‐90
WD5612 DDH 6521891.52 360109.18 342.39 50.29 359.53 ‐90
WD5613 DDH 6521894.02 360124.21 342.19 54.86 359.53 ‐90
WD5614 DDH 6521896.51 360139.24 342.09 33.53 359.53 ‐90
WD5808 DDH 6521760.18 360062.41 338.73 137.46 80.53 ‐45
WD6 DDH 6522089.92 360180.1 333.6 80 359.53 ‐90
WD6297 DDH 6522437.79 359864.01 337.69 67.06 359.53 ‐90
WD6298 DDH 6522440.28 359879.05 337.79 65.53 359.53 ‐90
WD6299 DDH 6522442.78 359894.08 337.89 60.96 359.53 ‐90
WD6300 DDH 6522445.27 359909.11 337.69 60.96 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WD6492 DDH 6521597.87 360201.19 350.39 60.96 359.53 ‐90
WD6493 DDH 6521600.36 360216.21 350.69 60.96 359.53 ‐90
WD6494 DDH 6521602.86 360231.25 351.09 41.15 359.53 ‐90
WD6501 DDH 6522447.77 359924.14 334.46 19.81 359.53 ‐90
WD6502 DDH 6522420.87 359669.12 337.43 74.68 359.53 ‐90
WD6503 DDH 6522419.37 359660.1 337.36 71.63 359.53 ‐90
WD6504 DDH 6522418.12 359652.58 337.2 51.82 359.53 ‐90
WD6540 DDH 6523888.89 358742.65 326.39 53.34 359.53 ‐90
WD6686 DDH 6521512.84 360805.36 342.99 24.38 359.53 ‐90
WD6687 DDH 6521515.34 360820.39 341.59 36.58 359.53 ‐90
WD6688 DDH 6521517.83 360835.42 340.49 45.72 359.53 ‐90
WD6689 DDH 6521520.32 360850.45 338.99 54.86 359.53 ‐90
WD6690 DDH 6521522.83 360865.49 338.09 42.67 359.53 ‐90
WD6691 DDH 6522595.61 359884.15 335.2 60.96 359.53 ‐90
WD6692 DDH 6522600.59 359914.21 336.12 60.96 359.53 ‐90
WD6693 DDH 6522605.58 359944.28 336.95 59.44 359.53 ‐90
WD6694 DDH 6522610.58 359974.34 337.67 60.96 359.53 ‐90
WD6695 DDH 6523893.89 358772.7 326.09 54.86 359.53 ‐90
WD7 DDH 6522147.47 360171.97 332.74 98 79.53 ‐60
WD8 DDH 6522208.48 360149.4 332 98 359.53 ‐90
WD8004 DDH 6523973.54 359624.47 322.39 45.72 359.53 ‐90
WD8005 DDH 6523968.54 359594.41 322.39 49.38 359.53 ‐90
WD8006 DDH 6523966.05 359579.38 322.39 51.82 359.53 ‐90
WD8007 DDH 6523963.56 359564.34 322.89 48.77 359.53 ‐90
WD8008 DDH 6523958.56 359534.28 322.89 53.34 359.53 ‐90
WD8009 DDH 6524209.06 359554.47 322.39 27.43 359.53 ‐90
WD8010 DDH 6524204.06 359524.41 322.89 45.72 359.53 ‐90
WD8011 DDH 6524201.56 359509.38 322.89 41.15 359.53 ‐90
WD8012 DDH 6524199.07 359494.34 322.89 40.23 359.53 ‐90
WD8013 DDH 6524196.58 359479.32 323.39 32 359.53 ‐90
WD8014 DDH 6524194.38 359466.09 323.39 28.96 359.53 ‐90
WD8015 DDH 6524189.09 359434.22 323.39 44.2 359.53 ‐90
WD9 DDH 6522278.51 360207.11 331.79 72 359.53 ‐90
WD9513 DDH 6522327.63 359758.74 338 41.15 359.53 ‐90
WD9514 DDH 6522325.13 359743.7 338 60.96 359.53 ‐90
WD9515 DDH 6522322.64 359728.68 338 60.96 359.53 ‐90
WD9516 DDH 6522380.27 359703.66 338 54.86 359.53 ‐90
WD9517 DDH 6522377.77 359688.63 338 60.96 359.53 ‐90
WD9518 DDH 6522375.28 359673.59 338 60.96 359.53 ‐90
WD9519 DDH 6522372.77 359658.56 338 60.96 359.53 ‐90
WD9520 DDH 6522387.98 359378 329.83 60.96 359.53 ‐90
WD9521 DDH 6522385.48 359362.98 329.52 60.96 359.53 ‐90
WD9522 DDH 6522382.98 359347.95 329.24 60.96 359.53 ‐90
WD9523 DDH 6522490.54 359623.57 333.56 57.91 359.53 ‐90
WD9524 DDH 6522493.04 359638.59 333.61 60.96 359.53 ‐90
WD9525 DDH 6522495.54 359653.62 333.62 60.96 359.53 ‐90
WD9526 DDH 6522498.03 359668.66 333.52 54.86 359.53 ‐90
WDA001 AC 6523860.15 359234.86 320 32 360 ‐90
WDA003 AC 6523947.15 359237.86 320 50 360 ‐90
WDA004 AC 6523907.15 359242.86 320 45 360 ‐90
WDA005 AC 6523804.15 359238.86 320 44 360 ‐90
WDA006 AC 6523751.15 359240.86 320 25 360 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WDA007 AC 6523959.15 359481.86 320 40 360 ‐90
WDA008 AC 6523909.15 359479.86 320 44 360 ‐90
WDA009 AC 6523854.15 359483.86 320 49 360 ‐90
WDA010 AC 6523798.15 359489.86 320 43 360 ‐90
WDA011 AC 6523765.15 359490.86 320 40 360 ‐90
WDA012 AC 6523857.15 359986.87 320 34 360 ‐90
WDA013 AC 6523957.15 359724.87 320 32 360 ‐90
WDA014 AC 6523907.15 359734.87 320 50 360 ‐90
WDA015 AC 6523857.15 359731.87 320 46 360 ‐90
WDA016 AC 6523804.15 359731.87 320 32 360 ‐90
WDA017 AC 6523751.15 359739.87 320 32 360 ‐90
WDA018 AC 6523888.15 359752.87 320 53 360 ‐90
WDC001 RC 6522117.94 360197.56 333.08 150 90 ‐60
WDC002 RC 6522118.18 360157.35 333.26 174 90 ‐60
WDC003 RC 6522117.72 360106.49 333.62 200 90 ‐60
WDC004 RC 6522119.16 360048.57 333.98 240 90 ‐60
WDC005 RC 6522078.07 360258.75 333.27 100 90 ‐60
WDC006 RC 6522047.8 360258.59 333.77 100 90 ‐60
WDC007 RC 6522047.8 360208.77 334.2 110 90 ‐60
WDC008 RC 6522047.9 360158.38 334.87 130 90 ‐60
WDC009 RC 6522048.47 360109.89 335.62 208 90 ‐60
WDC010 RC 6522198.53 360130.31 332.29 180 90 ‐60
WDC011 RC 6522197.1 360032.22 333.38 268 90 ‐60
WDC012 RC 6522224.05 360213.54 331.74 80 90 ‐60
WDC013 RC 6522449.63 360128.09 335.71 120 90 ‐60
WDC014 RC 6522447.2 360079.64 335.35 133 90 ‐60
WDC015 RC 6522229.07 360059.08 332.88 246 90 ‐60
WDC016 RC 6522132.13 360186.86 332.89 110 76.03 ‐60.13
WDC017 RC 6522182.13 360176.86 332.19 82 88.42 ‐59.69
WDC018 RC 6522407.14 360071.86 334.49 178 90.41 ‐60.17
WDC054 RC 6524059.75 359337.96 323 120 90 ‐60
WDC055 RC 6524060.25 359287.86 323.1 120 90 ‐60
WDC056 RC 6524059.15 359238.56 324.1 120 90 ‐60
WDC057 RC 6524062.15 359188.76 323.4 120 90 ‐60
WDC058 RC 6524060.15 359137.06 324.4 120 90 ‐60
WDC059 RC 6522082.43 360214.06 336.3 120 90 ‐60
WDC060 RC 6522008.03 360239.56 338.4 100 90 ‐60
WDC061 RC 6522033.53 360218.26 337.4 100 90 ‐60
WDC062 RC 6522106.93 360287.66 335.2 80 270 ‐60
WDC063 RC 6522107.53 360337.47 335.1 120 270 ‐60
WDC064 RC 6522107.13 360388.37 334.8 142 270 ‐60
WDC065 RC 6522307.94 360138.56 334.4 150 90 ‐60
WDC075 RC 6523859.45 359488.86 322.5 140 90 ‐60
WDC076 RC 6523859.25 359436.76 321.9 138 90 ‐60
WDC077 RC 6523858.05 359385.16 322.2 150 90 ‐60
WDC078 RC 6523859.55 359336.46 321.7 150 90 ‐60
WDC079 RC 6523858.55 359286.56 322 150 90 ‐60
WDC080 RC 6523858.85 359236.46 322.6 150 90 ‐60
WDC098 RC 6523857.15 359461.86 320 186 91.52 ‐60.19
WDC099 RC 6523857.15 359411.86 320 210 92.03 ‐60.65
WDC173 RC 6523657.15 359639.86 318.5 120 90 ‐60
WDC174 RC 6523664.15 359586.86 319 120 90 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WDC175 RC 6523662.15 359537.86 320.5 148 87.44 ‐60.43
WDC176 RC 6523458.15 359687.86 322 114 86.17 ‐60.41
WDC177 RC 6523456.15 359639.86 322 126 90 ‐60
WDC178 RC 6523457.15 359589.86 322.5 160 86.31 ‐60.39
WDC190 RC 6523243.15 358576.86 323.5 198 88.45 ‐60.29
WDC225 RC 6524257.05 359787.47 319.4 140 268.75 ‐50.15
WDC226 RC 6524256.15 359845.47 320.1 218.8 271.12 ‐51.08
WDC227 RC 6524256.55 359891.77 320.9 150 269.72 ‐50.69
WDC228 RC 6524258.55 359388.46 323.4 138 88.3 ‐60.8
WDC229 RC 6523258.05 359736.86 328.7 130 94.59 ‐60.27
WDC230 RC 6523259.45 359690.46 328.4 200 90.89 ‐61.13
WDC231 RC 6523059.95 359835.76 333.9 150 88.38 ‐60.45
WDD001 DDH 6522132.13 360122.86 333.3 159.9 88.71 ‐60.23
WDD002 DDH 6522132.13 360051.86 333.76 231.97 93.97 ‐59.81
WDD003 DDH 6522182.13 360130.86 332.5 151.11 87.96 ‐60.33
WDD004 DDH 6522182.13 360076.86 333.03 193.03 92.27 ‐59.98
WDD005 DDH 6522182.13 360006.86 333.76 252.3 93.21 ‐59.69
WDD006 DDH 6522232.14 360010.86 333.39 229 90.88 ‐59.79
WDD007 DDH 6522282.14 359976.86 333.62 247 92.74 ‐59.75
WDD008 DDH 6522357.14 359936.86 334.16 277 88.99 ‐60.88
WDD009 DDH 6522332.14 359851.86 336.66 342 93.7 ‐59.95
WDD010 DDH 6522362.14 359811.86 337.3 352.6 91.11 ‐60.5
WDD011 DDH 6522407.14 359906.86 334.59 363.2 90.69 ‐59.85
WDD012 DDH 6522409.14 359846.86 335.7 358 89.36 ‐60.38
WDD013 DDH 6522382.14 359811.86 336.89 400 93.01 ‐59.6
WDD014 DDH 6522181.93 360037.96 336 230.1 93.34 ‐60.28
WDD015 DDH 6522183.83 359988.26 336.3 300 92.52 ‐60.75
WDD017 DDH 6522133.43 360090.16 337.1 219.7 88.56 ‐61.06
WDD018 DDH 6522157.53 360012.26 337 249.7 93.78 ‐60.29
WDD023 DDH 6522168.82 360151.25 331.3 129.6 87.59 ‐60.86
WDD024 DDH 6522171.72 360124.65 332.9 153.6 86.91 ‐61.18
WDD025 DDH 6522174.92 360098.25 332.9 180.6 90 ‐60
WDD026 DDH 6522133.72 360165.15 330.5 133.5 90 ‐60
WDD027 DDH 6522257.33 360075.85 332.6 255.6 89.82 ‐61.55
WDD028 DDH 6522336.63 360018.25 333 300.6 91.27 ‐60.58
WDD074 DDH 6523649.15 359441.86 320 282.5 92.26 ‐60.68
WDD075 DDH 6523866.15 359317.86 320.5 217 89.54 ‐60.45
WDD091 DDH 6522224.89 360041.55 333.14 197.85 91.61 ‐59.52
WDD092 DDH 6522253.68 360001.62 334.24 206 90.95 ‐60.13
WDD093 DDH 6522297.43 360001.13 334.84 201.2 89.52 ‐60.84
WDD094 DDH 6522297.94 359974.96 344.14 295 90.93 ‐60.58
WDD095 DDH 6522318.46 359935.32 337.24 285 91.14 ‐60
WDD165 DDH 6522162.86 360159.64 275.66 135 274.93 ‐79.94
WDD166 DDH 6522186.68 360157.45 275.94 84 50.6 ‐73.5
WDD167 DDH 6522086.94 360205.28 274.79 78.1 165 ‐88.2
WDMT004 DDH 6522105.67 360249.05 236.14 42.5 0 ‐90
WDMT005 DDH 6522145.79 360205.17 259.54 57.4 0 ‐90
WDMT006 DDH 6522187.24 360192.9 274.04 33.5 0 ‐90
WDR001 RAB 6522957.15 360136.87 336 3 90 ‐60
WDR002 RAB 6522957.15 360086.87 338.18 8 90 ‐60
WDR003 RAB 6522957.15 360036.87 340.41 10 90 ‐60
WDR004 RAB 6522957.15 359986.87 342.41 26 90 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WDR005 RAB 6522957.15 359936.87 340.27 2 90 ‐60
WDR006 RAB 6522957.15 359886.86 337.45 23 90 ‐60
WDR007 RAB 6522957.15 359836.86 335.37 11 90 ‐60
WDR008 RAB 6522957.15 359786.86 333.9 3 90 ‐60
WDR009 RAB 6522957.15 359736.86 332.75 19 90 ‐60
WDR010 RAB 6522957.15 359686.86 331.69 2 90 ‐60
WDR011 RAB 6522957.15 359636.86 330.83 15 90 ‐60
WDR012 RAB 6522957.15 359586.86 330.02 29 90 ‐60
WDR013 RAB 6522957.15 359536.86 329.24 2 90 ‐60
WDR014 RAB 6523157.15 360136.87 331 12 90 ‐60
WDR015 RAB 6523157.15 360086.87 332.85 1 90 ‐60
WDR016 RAB 6523157.15 360036.87 333.04 26 90 ‐60
WDR017 RAB 6523157.15 359936.87 332.23 13 90 ‐60
WDR018 RAB 6523157.15 359886.87 331.97 23 90 ‐60
WDR019 RAB 6523157.15 359836.87 331.5 41 90 ‐60
WDR020 RAB 6523157.15 359786.86 331 6 90 ‐60
WDR021 RAB 6523157.15 359736.86 330.37 33 90 ‐60
WDR022 RAB 6523157.15 359686.86 329.68 16 90 ‐60
WDR023 RAB 6523157.15 359636.86 328.77 38 90 ‐60
WDR024 RAB 6523157.15 359586.86 327.87 4 90 ‐60
WDR025 RAB 6523157.15 359536.86 327.07 17 90 ‐60
WDR026 RAB 6523157.15 359486.86 326.38 5 90 ‐60
WDR027 RAB 6523157.15 359436.86 326.44 3 90 ‐60
WDR028 RAB 6523157.15 359386.86 326.03 25 90 ‐60
WDR029 RAB 6523357.15 360036.87 327.27 1 90 ‐60
WDR030 RAB 6523357.15 359986.87 327.56 2 90 ‐60
WDR031 RAB 6523357.15 359936.87 327.75 7 90 ‐60
WDR032 RAB 6523357.15 359886.87 327.87 21 90 ‐60
WDR033 RAB 6523357.15 359836.87 327.87 42 90 ‐60
WDR034 RAB 6523357.15 359786.87 327.64 28 90 ‐60
WDR035 RAB 6523357.15 359736.86 327.28 33 90 ‐60
WDR036 RAB 6523357.15 359686.86 326.76 6 90 ‐60
WDR037 RAB 6523357.15 359636.86 326.32 18 90 ‐60
WDR038 RAB 6523357.15 359586.86 326.06 43 90 ‐60
WDR039 RAB 6523357.15 359536.86 325.53 43 90 ‐60
WDR040 RAB 6523357.15 359486.86 325.05 42 90 ‐60
WDR041 RAB 6523357.15 359436.86 324.71 46 90 ‐60
WDR042 RAB 6523357.15 359386.86 324.28 29 90 ‐60
WDR043 RAB 6523357.15 359336.86 324.43 23 90 ‐60
WDR044 RAB 6523757.15 359836.87 322 35 90 ‐60
WDR045 RAB 6523757.15 359786.87 322 23 90 ‐60
WDR046 RAB 6523757.15 359736.87 322 36 90 ‐60
WDR047 RAB 6523757.15 359686.87 322 23 90 ‐60
WDR048 RAB 6523757.15 359636.87 322 17 90 ‐60
WDR049 RAB 6523757.15 359586.86 322 20 90 ‐60
WDR050 RAB 6523757.15 359536.86 322 16 90 ‐60
WDR051 RAB 6523757.15 359486.86 322 20 90 ‐60
WDR052 RAB 6523757.15 359436.86 322 17 90 ‐60
WDR053 RAB 6523757.15 359386.86 322 18 90 ‐60
WDR054 RAB 6523757.15 359336.86 322 17 90 ‐60
WDR055 RAB 6523757.15 359286.86 322 16 90 ‐60
WDR056 RAB 6523757.15 359236.86 322 19 90 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WDR057 RAB 6523757.15 359186.86 322 20 90 ‐60
WDR058 RAB 6523757.15 359136.86 322 20 90 ‐60
WDR059 RAB 6523557.15 359936.87 324.37 11 90 ‐60
WDR060 RAB 6523557.15 359886.87 324.18 12 90 ‐60
WDR061 RAB 6523557.15 359836.87 324.17 26 90 ‐60
WDR062 RAB 6523557.15 359786.87 324.02 53 90 ‐60
WDR063 RAB 6523557.15 359736.87 323.9 63 90 ‐60
WDR064 RAB 6523557.15 359686.87 323.69 39 90 ‐60
WDR065 RAB 6523557.15 359636.86 323.45 24 90 ‐60
WDR066 RAB 6523557.15 359586.86 323.36 14 90 ‐60
WDR067 RAB 6523557.15 359536.86 323.5 23 90 ‐60
WDR068 RAB 6523557.15 359486.86 323.64 47 90 ‐60
WDR069 RAB 6523557.15 359436.86 323.78 34 90 ‐60
WDR070 RAB 6523557.15 359386.86 323.92 27 90 ‐60
WDR071 RAB 6523557.15 359336.86 324 31 90 ‐60
WDR072 RAB 6523557.15 359286.86 324.31 49 90 ‐60
WDR073 RAB 6523557.15 359236.86 324.62 47 90 ‐60
WDR074 RAB 6523957.15 359836.87 322.84 25 90 ‐60
WDR075 RAB 6524157.15 359736.87 322.08 29 90 ‐60
WDR076 RAB 6524157.15 359686.87 322.32 21 90 ‐60
WDR077 RAB 6524157.15 359636.87 322.56 24 90 ‐60
WDR078 RAB 6524157.15 359586.87 322.79 26 90 ‐60
WDR079 RAB 6524157.15 359536.87 323.01 11 90 ‐60
WDR080 RAB 6524157.15 359486.86 323.27 12 90 ‐60
WDR081 RAB 6524157.15 359436.86 323.53 26 90 ‐60
WDR082 RAB 6524157.15 359386.86 323.8 5 90 ‐60
WDR083 RAB 6524157.15 359336.86 324.04 33 90 ‐60
WDR084 RAB 6524157.15 359286.86 324.24 61 90 ‐60
WDR085 RAB 6524157.15 359236.86 324.44 56 90 ‐60
WDR086 RAB 6524157.15 359186.86 324.63 67 90 ‐60
WDR087 RAB 6524157.15 359136.86 324.63 17 90 ‐60
WDR088 RAB 6524157.15 359036.86 324.63 23 90 ‐60
WDR089 RAB 6523957.15 359536.86 323.08 48 90 ‐60
WDR090 RAB 6523957.15 359486.86 323.32 50 90 ‐60
WDR091 RAB 6523957.15 359436.86 323.56 54 90 ‐60
WDR092 RAB 6523957.15 359386.86 323.8 65 90 ‐60
WDR093 RAB 6523957.15 359336.86 324 59 90 ‐60
WDR094 RAB 6523957.15 359286.86 324.06 57 90 ‐60
WDR095 RAB 6523957.15 359236.86 324.27 49 90 ‐60
WDR096 RAB 6523957.15 359186.86 324.49 45 90 ‐60
WDR097 RAB 6523957.15 359136.86 324.7 55 90 ‐60
WDR098 RAB 6523957.15 359086.86 324.7 18 90 ‐60
WDR099 RAB 6523957.15 359586.87 322.84 51 90 ‐60
WDR100 RAB 6523957.15 359636.87 322.84 20 90 ‐60
WID10 DDH 6522389.32 360133.19 333.56 8 359.53 ‐90
WID1000 DDH 6522087.57 360164.99 333.7 151 79.53 ‐60
WID1001 DDH 6522146.47 360157.74 332.82 201 79.53 ‐60
WID1002 DDH 6522140.27 360118.34 333.2 196 79.53 ‐60
WID1003 DDH 6522205.14 360137.51 332.14 189 79.53 ‐60
WID1004 DDH 6522198.59 360097.35 332.69 255 79.53 ‐60
WID1006 DDH 6522265.42 360127.53 332.18 103 79.53 ‐60
WID1006A DDH 6522264.94 360124.25 332 188.1 79.53 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID1011 DDH 6522094.45 360209.16 333.36 144 79.53 ‐60
WID1012 DDH 6522151.45 360080.99 333.3 250 89.53 ‐60
WID1013 DDH 6522153.27 360040.56 333.58 293 89.53 ‐60
WID1014 DDH 6522209.09 360055.49 333.05 302 94.53 ‐60
WID1015 DDH 6522210.22 360015.58 333.48 340 89.53 ‐60
WID1016 DDH 6522086.61 360134.03 333.84 222 89.53 ‐60
WID1017 DDH 6522084.17 360095.13 334.48 120.6 89.53 ‐60
WID1017A DDH 6522083.98 360093.84 335.16 40 89.53 ‐60
WID1017B DDH 6522083.8 360091.58 334.53 244 83.53 ‐60
WID1018 DDH 6522082.17 360059.01 335.06 301 83.53 ‐65
WID1019 DDH 6522228.49 360096.4 332.46 231.5 89.53 ‐60
WID1020 DDH 6522387.96 360112.14 333.79 125 89.53 ‐60
WID1020A DDH 6522388.2 360109.97 333.82 179.35 89.53 ‐60
WID1021 DDH 6522146.19 359984.07 334 180 89.53 ‐60
WID1021A DDH 6522146.55 359980.98 334 297 89.53 ‐60
WID1022 DDH 6522204.56 359972.12 334 369 84.53 ‐60.7
WID1023 DDH 6522265.49 360089.16 332.32 259.1 84.53 ‐60.7
WID1024 DDH 6522264.14 360048.91 332.78 271 89.53 ‐60
WID1025 DDH 6522262.78 360008.69 333.24 311 89.53 ‐60
WID1026 DDH 6522261.84 359962.92 333.78 342 89.53 ‐60
WID1031 DDH 6521927.29 360097.34 338 294 89.53 ‐60
WID1032 DDH 6521928.85 360186.99 336.53 200.1 89.53 ‐60
WID1033 DDH 6522027.77 360155.95 335.67 218 89.53 ‐60
WID1034 DDH 6522386.5 360022.35 334 328.1 89.53 ‐60
WID1035 DDH 6522385.86 360071.29 333.92 199 89.53 ‐60
WID1035A DDH 6522385.55 360070.87 333.91 263 89.53 ‐60
WID1036 DDH 6522506.25 360002.17 335.81 241 89.53 ‐60
WID1037 RC 6522686.98 359901.55 336.01 105 89.53 ‐60
WID1037A DDH 6522686.86 359898.66 335.92 258 82.53 ‐60
WID1038 DDH 6522506.68 359832.88 334 418 89.53 ‐60
WID1039 DDH 6522387.2 359923.4 334.25 402 94.53 ‐60
WID1040 DDH 6522258.89 359854.1 335.89 131 89.53 ‐60
WID1041 DDH 6522145.6 359938.64 334 237 89.53 ‐62
WID1042 DDH 6522023.21 359975.94 336.04 295.1 89.53 ‐62
WID1043 DDH 6522024.14 360042.85 336.72 304 89.53 ‐61
WID1248 RC 6521700 360164.48 341.03 46 89.53 ‐60
WID1249 RC 6521956.84 360249.31 335.99 64 89.53 ‐60
WID1250 RC 6521955.17 360269.17 335.75 60 89.53 ‐60
WID1251 RC 6521955.01 360289.58 335.52 64 89.53 ‐60
WID1252 RC 6521993.61 360242.67 335.19 58 89.53 ‐60
WID1252A RC 6521992.58 360239.69 335.25 64 89.53 ‐60
WID1253 RC 6521996.41 360266.5 334.85 70 89.53 ‐60
WID1254 RC 6521999.79 360289.65 334.49 78 89.53 ‐60
WID1255 RC 6522110.22 360254.52 332.76 70 89.53 ‐60
WID1271 RC 6521778.67 360120.81 338.94 58 89.53 ‐60
WID1271A RC 6521778.53 360118.64 338.93 68 89.53 ‐60
WID1272 RC 6521779.63 360135.74 339.04 52 89.53 ‐60
WID1273 RC 6521777.94 360156.62 339.17 54 89.53 ‐60
WID1274 RC 6521740 360127.49 339.72 58 89.53 ‐60
WID1274A RC 6521740 360127.49 339.72 70 89.53 ‐60
WID1275 RC 6521738.83 360147.24 339.94 54 89.53 ‐60
WID1276 RC 6521739.54 360166.96 340.03 40 89.53 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID1277 RC 6521700.04 360123.65 340.48 46 89.53 ‐60
WID1277A RC 6521699.86 360125.69 340.52 70 89.53 ‐60
WID1278 RC 6521699.42 360148.52 340.93 52 89.53 ‐60
WID1483 DDH 6522326.9 359960.3 334 361.1 88.53 ‐70.9
WID1484 DDH 6522266.18 359917.82 336.47 167.5 89.53 ‐60
WID1485 DDH 6522326.94 359960 334 311 89.53 ‐56.5
WID1486 DDH 6522388.72 359891.7 335.45 360 92.53 ‐61
WID1487 DDH 6522326.89 359960.6 334 357.6 93.53 ‐60
WID1528 AC 6523390.53 359274.44 312.89 39 359.53 ‐90
WID1530 AC 6523470.35 359253.78 312.89 31 359.53 ‐90
WID1532 AC 6523550.18 359233.13 312.89 44 359.53 ‐90
WID1534 AC 6523630 359212.47 312.89 48 359.53 ‐90
WID1536 AC 6523709.82 359191.82 312.89 54 359.53 ‐90
WID1537 AC 6521996.72 360005.82 312.89 57 359.53 ‐90
WID1539 AC 6522096.53 359985 312.89 57 359.53 ‐90
WID154 DDH 6521211.22 360384.33 363.09 2 359.53 ‐90
WID1541 AC 6522196.35 359964.18 312.89 50 359.53 ‐90
WID1543 AC 6522296.17 359943.36 312.89 38 359.53 ‐90
WID1593 DDH 6522342.9 359820.71 337.38 360 86.53 ‐51
WID1594 DDH 6522388.7 359891.62 335.45 408 82.53 ‐50
WID1602 AC 6522207.83 360144.06 332.04 28 359.53 ‐90
WID1603 AC 6522207.99 360164.05 332 35 359.53 ‐90
WID1604 AC 6522208.16 360184.05 332 40 359.53 ‐90
WID1605 AC 6522208.32 360204.05 331.89 43 359.53 ‐90
WID1606 AC 6522208.49 360224.04 331.6 55 359.53 ‐90
WID1607 AC 6522208.65 360244.04 331.48 48 359.53 ‐90
WID1608 AC 6522208.86 360269.04 331.35 37 359.53 ‐90
WID1609 AC 6522208.98 360284.04 331.26 36 359.53 ‐90
WID1610 AC 6522447.79 360142.08 335.5 50 359.53 ‐90
WID1611 AC 6522447.96 360162.09 335.16 67 359.53 ‐90
WID1612 AC 6522448.12 360182.08 334.6 52 359.53 ‐90
WID1613 AC 6522448.29 360202.08 333.88 5 359.53 ‐90
WID1614 AC 6522547.6 360102.94 336.75 50 359.53 ‐90
WID1615 AC 6522546.19 360122.09 336.52 52 359.53 ‐90
WID1616 AC 6522549.33 360141.48 336.42 43 359.53 ‐90
WID1617 AC 6522550.01 360162.23 335.96 4 359.53 ‐90
WID1618 AC 6522160.79 360259.43 331.93 37 359.53 ‐90
WID1677 DDH 6522443.99 359732.29 337.59 414 90.53 ‐61
WID1678 DDH 6522443.99 359732.29 335.93 495.8 83.53 ‐50.5
WID1679 DDH 6522206.6 359991.16 333.78 254 89.53 ‐59.3
WID1680 DDH 6522107.13 360055.05 334.27 279 107.53 ‐60.2
WID1681 DDH 6522205.84 359951.5 335.11 325.7 93.53 ‐60.2
WID1682 DDH 6522296.31 359952.97 333.94 320 95.53 ‐60
WID1683 DDH 6522297.41 360033.72 332.93 303.8 92.53 ‐60
WID1684 DDH 6522028.29 360182.42 335 159 89.53 ‐60
WID1685 DDH 6522152 360191.54 332.55 117.5 76.53 ‐60.5
WID1686 DDH 6522157.21 360208.7 332.35 96 88.53 ‐60.2
WID1687 DDH 6522088.18 360185.04 333.61 170.1 87.53 ‐60.3
WID1688 DDH 6522127.25 360084.6 333.64 254.4 106.53 ‐65
WID1717 DDH 6522148.17 360184.54 332.64 87 89.53 ‐65
WID1720 DDH 6522384.06 359851.83 336.02 390 85.53 ‐60.5
WID1739 RC 6522499.57 360131.02 336 66 89.53 ‐60
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID1740 RC 6522501.11 360100.79 336 84 89.53 ‐60
WID1741 RC 6522497.8 360081.83 336 94 89.53 ‐60
WID1742 RC 6522548.3 360122.35 336.58 60 89.53 ‐60
WID1743 RC 6522548.58 360101.65 336.79 76 89.53 ‐60
WID1744 RC 6522546.29 360082.11 336.76 108 89.53 ‐60
WID1745 RC 6522597.86 360119.09 338.08 60 89.53 ‐60
WID1746 RC 6522594.17 360093.04 338.07 60 89.53 ‐60
WID1747 RC 6522594.09 360081.62 338.18 108 89.53 ‐60
WID1761 RC 6522003.56 360835.66 330.57 60 89.53 ‐60
WID1762 RC 6522003.39 360815.66 330.64 100 89.53 ‐60
WID1763 RC 6522003.23 360795.67 330.68 118 89.53 ‐60
WID1767 RC 6521903.4 360816.49 331.65 85 89.53 ‐60
WID1768 RC 6521903.24 360796.49 331.74 90 89.53 ‐60
WID1769 RC 6521903.07 360776.5 331.82 120 89.53 ‐60
WID1857 RC 6522795.87 359858.36 337.49 131 89.53 ‐60
WID1858 RC 6522798.97 359896.52 337.32 74 89.53 ‐60
WID1859 RC 6522796.4 359931.58 342.64 84 89.53 ‐60
WID1861 RC 6522995.7 359809.67 333.48 118 89.53 ‐60
WID1862 RC 6522997.31 359847.55 334.53 80 89.53 ‐60
WID1864 RC 6523194.28 359723.77 327.77 120 89.53 ‐60
WID1865 RC 6523191.19 359758.99 328.31 74 89.53 ‐60
WID1871 RC 6523393.99 359682.28 323.72 120 89.53 ‐60
WID1872 RC 6523391.74 359720.97 324.17 80 89.53 ‐60
WID3175A AC 6523173.92 358469.32 327.89 28 269.53 ‐60
WID340 DDH 6522440.17 360064.41 335.15 22 359.53 ‐90
WID341 DDH 6522435.18 360034.36 334.79 12 359.53 ‐90
WID3460 PERC 6522068.13 360141.86 334.28 160 89.53 ‐60
WID3461 PERC 6522068.13 360184.86 333.93 140 90.53 ‐60
WID3462 PERC 6522068.13 360229.86 333.64 90 89.53 ‐59
WID3463 PERC 6522093.63 360241.86 333.13 70 90.53 ‐60
WID3464 PERC 6522093.63 360241.86 333.13 140 37.53 ‐90
WID3465 PERC 6522093.63 360287.86 332.8 50 297.53 ‐89
WID3466 PERC 6522208.13 360173.86 332 100 89.53 ‐60
WID3467 PERC 6522208.13 360206.86 331.85 100 88.53 ‐61
WID3468 PERC 6522268.14 360173.86 332 140 89.53 ‐60
WID3469 PERC 6522327.14 360052.86 333 200 89.53 ‐60
WID374 DDH 6521312.92 359973.56 345.69 11 359.53 ‐90
WID375 DDH 6521307.93 359943.5 344.89 4 359.53 ‐90
WID376 DDH 6521310.42 359958.53 345.39 4 359.53 ‐90
WID377 DDH 6521297.95 359883.37 343.79 4 359.53 ‐90
WID378 DDH 6521538.45 359843.44 342.69 14 359.53 ‐90
WID379 DDH 6521528.47 359783.31 342.89 21 359.53 ‐90
WID380 DDH 6521518.5 359723.19 341.69 10 359.53 ‐90
WID381 DDH 6521523.48 359753.24 342.39 12 359.53 ‐90
WID382 DDH 6521525.98 359768.28 342.69 10 359.53 ‐90
WID383 DDH 6521527.23 359775.8 342.79 10 359.53 ‐90
WID384 DDH 6521778.97 359803.5 335.37 10 359.53 ‐90
WID385 DDH 6521778.97 359803.5 335.37 30 359.53 ‐90
WID386 DDH 6521773.99 359773.43 335.04 38 359.53 ‐90
WID387 DDH 6521771.48 359758.4 334.89 10 359.53 ‐90
WID388 DDH 6521770.24 359750.89 334.81 34 359.53 ‐90
WID389 DDH 6522014.5 359733.5 333.6 16 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID390 DDH 6522024.48 359793.63 334 16 359.53 ‐90
WID391 DDH 6522034.47 359853.76 334.59 20 359.53 ‐90
WID392 DDH 6522044.45 359913.88 335.24 14 359.53 ‐90
WID393 DDH 6522054.44 359974 335.29 15 359.53 ‐90
WID394 DDH 6522049.45 359943.94 335.26 32 359.53 ‐90
WID395 DDH 6522046.95 359928.91 335.25 28 359.53 ‐90
WID396 DDH 6522045.7 359921.39 335.18 14 359.53 ‐90
WID397 DDH 6522284.97 359873.94 335.69 28 359.53 ‐90
WID398 DDH 6522245.03 359633.44 335.61 48 359.53 ‐90
WID399 DDH 6522255.02 359693.56 336.53 39 359.53 ‐90
WID400 DDH 6522265 359753.69 337.14 44 359.53 ‐90
WID401 DDH 6522260.02 359723.62 337.03 40 359.53 ‐90
WID402 DDH 6522257.51 359708.6 336.81 38 359.53 ‐90
WID403 DDH 6522235.05 359573.31 334.96 26 359.53 ‐90
WID404 DDH 6522225.06 359513.18 334.11 34 359.53 ‐90
WID405 DDH 6522230.06 359543.24 334.66 22 359.53 ‐90
WID406 DDH 6522227.56 359528.22 334.46 38 359.53 ‐90
WID407 DDH 6522226.32 359520.7 334.29 44 359.53 ‐90
WID412 DDH 6521948.94 360454.92 334.3 30 359.53 ‐90
WID413 DDH 6521953.92 360484.98 334 28 359.53 ‐90
WID414 DDH 6523462.12 360265.45 322.09 24 359.53 ‐90
WID415 DDH 6522174.47 360324.79 331.38 38 359.53 ‐90
WID416 DDH 6522164.49 360264.65 331.86 34 359.53 ‐90
WID417 DDH 6522169.48 360294.72 331.6 36 359.53 ‐90
WID418 DDH 6522171.98 360309.76 331.49 36 359.53 ‐90
WID419 DDH 6522173.22 360317.27 331.44 36 359.53 ‐90
WID420 DDH 6522400.01 360194.67 333.11 58 359.53 ‐90
WID421 DDH 6522405.01 360224.72 332.36 36 359.53 ‐90
WID422 DDH 6522402.51 360209.7 332.8 44 359.53 ‐90
WID423 DDH 6522403.76 360217.21 332.6 50 359.53 ‐90
WID424 DDH 6522630.55 360094.6 339.95 13 359.53 ‐90
WID425 DDH 6522635.53 360124.67 339.65 3 359.53 ‐90
WID426 DDH 6522633.04 360109.64 339.87 3 359.53 ‐90
WID427 DDH 6522631.8 360102.12 339.93 4 359.53 ‐90
WID428 DDH 6522856.08 359964.48 341.97 6 359.53 ‐90
WID429 DDH 6522858.57 359979.51 343.17 3 359.53 ‐90
WID430 DDH 6522857.33 359971.99 342.59 4 359.53 ‐90
WID431 DDH 6523086.6 359864.41 332.99 4 359.53 ‐90
WID432 DDH 6523081.61 359834.35 331.69 6 359.53 ‐90
WID433 DDH 6523084.11 359849.39 332.79 4 359.53 ‐90
WID434 DDH 6523085.35 359856.9 332.89 6 359.53 ‐90
WID435 DDH 6523166.48 360345.44 332.49 4 359.53 ‐90
WID436 DDH 6523161.48 360315.37 326.89 16 359.53 ‐90
WID437 DDH 6523163.99 360330.4 326.79 4 359.53 ‐90
WID438 DDH 6523165.23 360337.92 326.39 8 359.53 ‐90
WID439 DDH 6522930.96 360415.42 326.01 8 359.53 ‐90
WID440 DDH 6522928.46 360400.4 326.57 10 359.53 ‐90
WID441 DDH 6522929.71 360407.92 326.29 8 359.53 ‐90
WID442 DDH 6522705.43 360545.55 326.51 10 359.53 ‐90
WID443 DDH 6522710.42 360575.62 326.07 33 359.53 ‐90
WID444 DDH 6522707.92 360560.58 326.29 14 359.53 ‐90
WID445 DDH 6522706.68 360553.06 326.4 14 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID446 DDH 6522474.89 360645.61 326.48 42 359.53 ‐90
WID447 DDH 6522473.65 360638.1 326.57 20 359.53 ‐90
WID448 DDH 6522479.89 360675.68 326.13 38 359.53 ‐90
WID449 DDH 6522469.9 360615.55 326.84 26 359.53 ‐90
WID450 DDH 6522467.41 360600.52 327.02 36 359.53 ‐90
WID451 DDH 6522464.92 360585.49 327.19 24 359.53 ‐90
WID452 DDH 6522459.92 360555.43 327.55 34 359.53 ‐90
WID453 DDH 6522462.41 360570.45 327.79 4 359.53 ‐90
WID454 DDH 6522468.65 360608.04 326.93 34 359.53 ‐90
WID455 DDH 6522239.38 360715.61 328.47 24 359.53 ‐90
WID456 DDH 6522241.87 360730.65 328.33 36 359.53 ‐90
WID457 DDH 6522243.12 360738.16 328.27 26 359.53 ‐90
WID458 DDH 6522008.84 360815.68 330.57 2 359.53 ‐90
WID459 DDH 6522011.35 360830.71 330.51 6 359.53 ‐90
WID460 DDH 6522010.09 360823.19 330.55 3 359.53 ‐90
WID461 DDH 6521956.42 360500.01 334 26 359.53 ‐90
WID462 DDH 6521955.17 360492.49 334 28 359.53 ‐90
WID463 DDH 6521753.35 360765.42 334 4 359.53 ‐90
WID464 DDH 6521758.35 360795.49 333.48 4 359.53 ‐90
WID465 DDH 6521748.37 360735.36 334.77 4 359.53 ‐90
WID466 DDH 6521745.87 360720.33 334.82 2 359.53 ‐90
WID467 DDH 6521747.11 360727.85 334.78 4 359.53 ‐90
WID468 DDH 6521272.32 360845.3 340.99 2 359.53 ‐90
WID469 DDH 6521272.67 360852.96 340.89 6 359.53 ‐90
WID473 DDH 6522472.4 360630.58 326.66 34 359.53 ‐90
WID474 DDH 6523317.13 359764.36 329.29 4 359.53 ‐90
WID475 DDH 6523322.12 359794.41 329.69 6 359.53 ‐90
WID476 DDH 6523319.63 359779.39 329.39 6 359.53 ‐90
WID477 DDH 6523320.88 359786.91 329.49 12 359.53 ‐90
WID478 DDH 6523387.02 360185.24 323.89 8 359.53 ‐90
WID479 DDH 6523389.52 360200.28 323.69 6 359.53 ‐90
WID480 DDH 6523392.01 360215.31 323.49 6 359.53 ‐90
WID481 DDH 6523390.76 360207.79 322.69 6 359.53 ‐90
WID482 DDH 6523612.55 360055.12 323.09 13 359.53 ‐90
WID483 DDH 6523607.56 360025.06 323.89 21 359.53 ‐90
WID484 DDH 6523602.57 359994.99 323.89 12 359.53 ‐90
WID485 DDH 6523617.54 360085.19 322.79 10 359.53 ‐90
WID486 DDH 6523615.05 360070.15 322.89 10 359.53 ‐90
WID487 DDH 6523616.3 360077.67 322.89 7 359.53 ‐90
WID488 DDH 6523615.7 360074.06 322.99 20 359.53 ‐90
WID489 DDH 6523843.08 359955.06 319.09 22 359.53 ‐90
WID490 DDH 6523838.08 359924.99 318.89 30 359.53 ‐90
WID491 DDH 6523840.58 359940.03 318.99 32 359.53 ‐90
WID492 DDH 6523839.33 359932.51 318.89 30 359.53 ‐90
WID493 DDH 6524068.61 359824.94 317.68 38 359.53 ‐90
WID494 DDH 6524073.6 359855 317.61 58 359.53 ‐90
WID495 DDH 6524071.1 359839.96 317.65 52 359.53 ‐90
WID507 DDH 6522259.35 360835.86 327.41 18 359.53 ‐90
WID508 DDH 6522249.36 360775.74 327.95 12 359.53 ‐90
WID509 DDH 6522251.86 360790.77 327.83 18 359.53 ‐90
WID510 DDH 6522246.87 360760.71 328.07 13 359.53 ‐90
WID511 DDH 6522244.38 360745.68 328.2 37 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID512 DDH 6522240.63 360723.13 328.4 38 359.53 ‐90
WID513 DDH 6522715.41 360605.67 325.77 40 359.53 ‐90
WID514 DDH 6522940.94 360475.55 324.94 22 359.53 ‐90
WID515 DDH 6522938.45 360460.53 325.19 10 359.53 ‐90
WID516 DDH 6522939.7 360468.04 325.07 19 359.53 ‐90
WID517 DDH 6523171.47 360375.49 324.99 28 359.53 ‐90
WID518 DDH 6523168.97 360360.46 325.29 7 359.53 ‐90
WID519 DDH 6523170.23 360367.98 325.49 16 359.53 ‐90
WID520 DDH 6523397.01 360245.37 322.89 16 359.53 ‐90
WID521 DDH 6523394.5 360230.34 322.89 8 359.53 ‐90
WID522 DDH 6523395.75 360237.85 322.89 10 359.53 ‐90
WID523 DDH 6523622.54 360115.25 321.89 18 359.53 ‐90
WID524 DDH 6523625.03 360130.28 321.69 20 359.53 ‐90
WID525 DDH 6523627.52 360145.31 321.29 12 359.53 ‐90
WID526 DDH 6523630.03 360160.34 320.79 42 359.53 ‐90
WID527 DDH 6523628.78 360152.83 320.89 28 359.53 ‐90
WID529 DDH 6523856.56 360036.24 318.89 28 359.53 ‐90
WID530 DDH 6523858.55 360048.26 318.79 18 359.53 ‐90
WID531 DDH 6523863.05 360075.32 318.69 30 359.53 ‐90
WID532 DDH 6523865.54 360090.34 318.69 24 359.53 ‐90
WID533 DDH 6524093.57 359975.25 317.3 48 359.53 ‐90
WID534 DDH 6524072.36 359847.48 317.63 46 359.53 ‐90
WID535 DDH 6524285.41 359642.2 318.32 24 359.53 ‐90
WID536 DDH 6522223.82 359505.67 334 44 359.53 ‐90
WID537 DDH 6522258.76 359716.11 336.95 42 359.53 ‐90
WID538 DDH 6522709.17 360568.1 326.18 14 359.53 ‐90
WID539 DDH 6522017.59 360868.29 330.2 22 359.53 ‐90
WID540 DDH 6522021.33 360890.84 330 7 359.53 ‐90
WID541 DDH 6522026.32 360920.9 329.98 4 359.53 ‐90
WID542 DDH 6522028.81 360935.93 330.89 6 359.53 ‐90
WID543 DDH 6522023.82 360905.86 330 10 359.53 ‐90
WID544 DDH 6522025.08 360913.38 330 10 359.53 ‐90
WID545 DDH 6521768.33 360855.62 331.35 8 359.53 ‐90
WID546 DDH 6521755.86 360780.45 334 4 359.53 ‐90
WID547 DDH 6521750.86 360750.39 334.35 6 359.53 ‐90
WID548 DDH 6521279.81 360890.39 339.89 6 359.53 ‐90
WID549 DDH 6521282.31 360905.43 340.39 4 359.53 ‐90
WID550 DDH 6521284.8 360920.45 338.89 7 359.53 ‐90
WID551 DDH 6521287.3 360935.48 337.89 8 359.53 ‐90
WID552 DDH 6521292.29 360965.55 336.89 16 359.53 ‐90
WID553 DDH 6521297.28 360995.61 335.39 12 359.53 ‐90
WID554 DDH 6521294.79 360980.58 336.39 12 359.53 ‐90
WID555 DDH 6521293.54 360973.07 336.89 13 359.53 ‐90
WID585 DDH 6522508.82 360477.79 328.42 34 359.53 ‐90
WID586 DDH 6522166.98 360279.7 331.74 38 359.53 ‐90
WID587 DDH 6522162 360249.62 331.96 40 359.53 ‐90
WID670 DDH 6521315.41 359988.6 343.37 10 359.53 ‐90
WID671 DDH 6521314.17 359981.08 343.08 4 359.53 ‐90
WID672 DDH 6521316.66 359996.1 343.65 4 359.53 ‐90
WID673 DDH 6521317.91 360003.62 343.94 9 359.53 ‐90
WID674 DDH 6521693.66 360033.91 339.23 20 359.53 ‐90
WID675 DDH 6521698.65 360063.97 339.65 14 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID676 DDH 6521696.15 360048.94 339.44 16 359.53 ‐90
WID677 DDH 6521697.4 360056.46 339.56 32 359.53 ‐90
WID678 DDH 6521919.2 359903.78 336.91 16 359.53 ‐90
WID679 DDH 6521914.21 359873.72 336.07 16 359.53 ‐90
WID680 DDH 6521919.2 359903.78 336.91 12 359.53 ‐90
WID681 DDH 6521924.19 359933.84 337.63 10 359.53 ‐90
WID682 DDH 6521929.18 359963.91 338 30 359.53 ‐90
WID683 DDH 6522048.2 359936.42 335.32 38 359.53 ‐90
WID684 DDH 6522401.26 360202.18 333 52 359.53 ‐90
WID685 DDH 6522740.81 360014.5 344.18 5 359.53 ‐90
WID686 DDH 6522735.83 359984.44 341.64 6 359.53 ‐90
WID687 DDH 6522738.32 359999.47 342.98 6 359.53 ‐90
WID688 DDH 6522739.57 360006.98 343.59 16 359.53 ‐90
WID689 DDH 6522971.34 359914.45 337.89 8 359.53 ‐90
WID690 DDH 6522966.35 359884.38 336.89 4 359.53 ‐90
WID691 DDH 6522968.85 359899.41 337.89 17 359.53 ‐90
WID692 DDH 6522940.03 359911.93 337.15 4 359.53 ‐90
WID693 DDH 6523200.62 359806.87 332.69 14 359.53 ‐90
WID694 DDH 6523436.13 359736.87 326.39 22 359.53 ‐90
WID695 DDH 6523399.5 360260.4 322.79 6 359.53 ‐90
WID696 DDH 6523399.5 360260.4 322.79 12 359.53 ‐90
WID697 DDH 6523868.04 360105.37 316.79 38 359.53 ‐90
WID698 DDH 6523866.78 360097.86 316.69 28 359.53 ‐90
WID699 DDH 6524183.87 359774.9 317.57 32 359.53 ‐90
WID700 DDH 6524188.86 359804.97 317.51 30 359.53 ‐90
WID701 DDH 6524186.37 359789.93 317.54 44 359.53 ‐90
WID702 DDH 6524185.12 359782.42 317.56 34 359.53 ‐90
WID703 DDH 6524193.86 359835.03 317.44 44 359.53 ‐90
WID704 DDH 6524196.35 359850.06 317.41 42 359.53 ‐90
WID714 DDH 6521943.94 360424.86 334.57 28 359.53 ‐90
WID715 DDH 6521938.95 360394.79 334.65 24 359.53 ‐90
WID716 DDH 6521933.95 360364.72 334.94 28 359.53 ‐90
WID717 DDH 6521923.97 360304.59 335.93 22 359.53 ‐90
WID718 DDH 6521928.97 360334.65 335.34 26 359.53 ‐90
WID719 DDH 6521926.46 360319.62 335.62 28 359.53 ‐90
WID720 DDH 6521925.22 360312.1 335.78 32 359.53 ‐90
WID721 DDH 6522153.8 360205.53 332.43 39 359.53 ‐90
WID722 DDH 6522157.88 360219.98 332.25 43 359.53 ‐90
WID723 DDH 6522159.08 360233.48 332.12 38 359.53 ‐90
WID724 DDH 6522158.25 360227.08 332.19 46 359.53 ‐90
WID742 DDH 6522279.76 360214.63 331.68 50 359.53 ‐90
WID743 DDH 6522274.76 360184.56 332 44 359.53 ‐90
WID744 DDH 6522269.78 360154.5 332 58 359.53 ‐90
WID745 DDH 6522259.79 360094.37 332.29 44 359.53 ‐90
WID746 DDH 6522264.78 360124.43 332 40 359.53 ‐90
WID747 DDH 6523169.2 359989.72 329.39 40 359.53 ‐90
WID748 DDH 6522266.03 360131.95 332 44 359.53 ‐90
WID749 DDH 6522515.28 360144.64 336 20 359.53 ‐90
WID750 DDH 6522510.3 360114.56 336 34 359.53 ‐90
WID751 DDH 6522512.79 360129.6 336 28 359.53 ‐90
WID752 DDH 6522514.03 360137.12 336 28 359.53 ‐90
WID753 DDH 6522039.24 360254.56 333.94 32 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID Hole_Type MGA_North MGA_East RL Depth Azimuth Dip
WID754 DDH 6522044.24 360284.62 333.64 38 359.53 ‐90
WID755 DDH 6522049.23 360314.68 333.38 44 359.53 ‐90
WID756 DDH 6522046.73 360299.66 333.5 46 359.53 ‐90
WID757 DDH 6522045.48 360292.14 333.57 50 359.53 ‐90
WID762 DDH 6522099.37 360244.58 333.01 42 359.53 ‐90
WID763 DDH 6522094.38 360214.51 333.32 34 359.53 ‐90
WID764 DDH 6522096.88 360229.54 333.17 42 359.53 ‐90
WID765 DDH 6522098.12 360237.06 333.09 58 359.53 ‐90
WID766 DDH 6522220.75 360222.2 331.62 44 359.53 ‐90
WID767 DDH 6522216.23 360193.85 332 58 359.53 ‐90
WID768 DDH 6522216.76 360207.51 331.84 42 359.53 ‐90
WID769 DDH 6522215.64 360199.75 331.95 58 359.53 ‐90
WID785 DDH 6522277.2 360147.87 332 91 359.53 ‐90
WID786 DDH 6522282.26 360229.66 331.46 62 359.53 ‐90
WID787 DDH 6522284.75 360244.7 331.24 49 359.53 ‐90
WID788 DDH 6522287.25 360259.73 331.01 57 359.53 ‐90
WID789 DDH 6522680.69 360024.48 341.78 14 359.53 ‐90
WID790 DDH 6522681.94 360032 341.97 8 359.53 ‐90
WID791 DDH 6523958.33 359905.02 317.19 18 359.53 ‐90
WID792 DDH 6522683.19 360039.52 342.23 10 359.53 ‐90
Cooke deposit
Hole_ID MGA_North MGA_East RL Depth Azimuth Dip
WD3216 6519981.98 361260.36 349 18.29 359.53 ‐90
WD3217 6519984.48 361275.39 348.03 30.48 359.53 ‐90
WD5000 6519979.49 361245.32 349.58 15.24 359.53 ‐90
WD5326 6519817.53 361386.21 347.11 153.01 260.53 ‐44
WD5335 6519827.07 361443.64 343.34 238.66 260.53 ‐44.59
WD5336 6519877.16 361371.53 346.35 150.88 260.53 ‐40.73
WD5339 6519847.36 361193.17 354.14 333.45 80.53 ‐65
WD5340 6519909.38 361195.19 355.6 238.96 89.12 ‐40.8
WD5348 6519996.78 361348.62 343.57 183.79 257.26 ‐45.28
WD5350 6519944.08 361404.02 344 232.87 245.9 ‐46.74
WD5408 6519781.52 361355.43 350.06 45.72 359.53 ‐90
WD5409 6519784.02 361370.46 348.99 18.29 359.53 ‐90
WD5410 6519786.52 361385.5 347.92 25.91 359.53 ‐90
WD5419 6519839.15 361330.42 349.18 42.67 80.53 ‐80
WD5420 6519808.59 361332.4 350.41 51.82 80.53 ‐80
WD5421 6519810.34 361342.93 349.82 39.62 80.53 ‐80
WD5422 6519806.59 361320.38 351.18 19.81 80.53 ‐80
WD5423 6519865.69 361307.22 348.89 51.82 80.53 ‐85
WD5424 6519869.21 361325.42 347.87 47.24 359.53 ‐90
WD5425 6519872.21 361343.47 347.45 24.38 359.53 ‐90
WD5426 6519864.72 361298.36 349.37 41.15 359.53 ‐90
WD5427 6519779.03 361340.41 351.06 22.86 359.53 ‐90
WD5428 6519810.59 361344.42 349.73 18.29 260.53 ‐50
WD5429 6519812.08 361353.45 349.21 44.2 260.53 ‐50
WD5430 6519810.59 361344.42 349.73 45.72 260.53 ‐50
WD5431 6519976.98 361230.3 350.22 36.58 359.53 ‐90
WD5432 6519974.49 361215.27 351.16 27.43 359.53 ‐90
WD5433 6519972 361200.23 352.19 13.72 359.53 ‐90
For
per
sona
l use
onl
y
Hole_ID MGA_North MGA_East RL Depth Azimuth Dip
WD5665 6519923.1 361277.87 349.7 51.82 260.53 ‐70
WD5666 6519926.85 361300.41 347.66 56.39 260.53 ‐70
WD5802 6520006.9 361410.38 342.04 349 260.53 ‐61
WD6059 6519897.37 361327.54 346.72 88.39 260.53 ‐60
WD6256 6519786.52 361385.5 347.92 64.01 260.53 ‐60
WD6257 6519870.21 361331.43 347.73 60.96 260.53 ‐60
WD6258 6519931.6 361328.97 345.89 109.73 260.53 ‐60
WD6543 6519775.24 361392 347.72 118.87 260.53 ‐60
WD6544 6519842.15 361348.45 348.47 80.77 260.53 ‐65
WDC145 6519869.964 361316.873 354.444 80 270 ‐60
WDC146 6519834.985 361323.817 355.444 100 360 ‐90
WDC147 6519813.336 361357.72 355.444 94 270 ‐60
WDC148 6519798.659 361360.101 355.644 100 270 ‐60
WDC149 6519765.248 361365.488 352.744 70 270 ‐60
WDC150 6519781.956 361360.212 347.244 70 270 ‐60
WDC159 6519786.556 361355.985 350.444 49 360 ‐90
WDGT01 6519816.08 361280.584 360.044 60.2 268.78 ‐60.55
WDGT02 6519849.389 361268.942 363.944 120.2 90.87 ‐60.26
WDGT03 6519802.772 361360.95 345.744 60 80.48 ‐59.49
WDGT04 6519879.883 361320.718 350.444 65 88.35 ‐60.47
WDMT01 6519821.092 361355.867 354 114.5 268.69 ‐59.5
WDMT02 6519785.963 361361.395 349.044 80 270 ‐55.46
WDMT03 6519805.75 361359.754 346.844 120 270 ‐60
WID1237 6519810.86 361271.15 359.25 200 83.4 ‐65
WID1238 6519810.6 361411.44 345.73 200 262.52 ‐60.79
WID1423 6519912.51 361389.66 344.77 240.5 273.53 ‐57
WID1425 6519810.17 361398.71 346.53 211 269.53 ‐62
WID1645 6519783.76 361363.12 349.49 30 269.53 ‐60
WID1646 6519784.02 361373.15 348.81 50 269.53 ‐60
WID1647 6519784.87 361381.82 348.2 70 269.53 ‐60
WID1648 6519807.89 361343.63 349.87 60 271.53 ‐60
WID1649 6519806.84 361353.09 349.43 80 269.53 ‐60
WID1650 6519806.77 361361.18 348.97 100 269.53 ‐60
WID1651 6519832.22 361333.8 349.38 30 269.53 ‐60
WID1652 6519833.61 361344.08 348.97 50 269.53 ‐60
WID1653 6519834.26 361352.95 348.52 70 269.53 ‐60
WID1654 6519857.38 361311.51 349.12 30 269.53 ‐60
WID1655 6519857.89 361322.28 348.45 58 269.53 ‐60
WID1656 6519858.21 361329.74 348.27 80 269.53 ‐60
WID1657 6519880.74 361290.7 348.57 30 269.53 ‐60
WID1658 6519881.96 361300.78 348.12 52 269.53 ‐60
WID1659 6519883.18 361311.73 347.72 70 269.53 ‐60
WID1675 6519806.98 361385.47 347.45 150 261.22 ‐44.06
WID1779 6519884.51 361341.71 347.02 157.3 269.8 ‐61
WID1781 6519784.19 361360.97 349.63 111 269.53 ‐59
WID1791 6519839.71 361363.52 347.8 100 269.53 ‐60
WID1792 6519840.95 361373.9 347.19 100 269.53 ‐60
WID1793 6519858.95 361336.5 348.08 118 269.53 ‐60
WID1794 6519883.89 361321.06 347.41 92 269.53 ‐60
WID1795 6519885.1 361329.59 347.14 120 269.53 ‐60
WID1796 6519858.87 361357.38 347.47 146 269.53 ‐60
WID1797 6519912.48 361287.21 348.59 40 269.53 ‐60
For
per
sona
l use
onl
y
Hole_ID MGA_North MGA_East RL Depth Azimuth Dip
WID1798 6519911.23 361296.72 347.74 60 269.53 ‐60
WID1799 6519909.75 361308.72 347.05 80 269.53 ‐60
WID1799Z 6519909.75 361308.71 347.05 80 269.53 ‐60
WID1800 6519907.94 361319.75 346.54 100 269.53 ‐60
WID1801 6519901.88 361329.34 346.5 112 269.53 ‐60
WID1803 6519762.64 361372.23 349.11 42 269.53 ‐60
WID1804 6519761.47 361384.18 348.31 80 269.53 ‐60
WID1836 6519811.03 361274.23 359.05 184.9 88.53 ‐56.8
WID1837 6519829.58 361285.05 354.49 144.5 86.53 ‐67.3
WID1838 6519832.83 361334.78 349.33 88 269.53 ‐60
WID1839 6519834 361343.78 348.97 100 269.53 ‐60
WID1840 6519932.11 361278.21 349.95 50 269.53 ‐60
WID1841 6519932.52 361287.68 348.91 70 269.53 ‐60
WID1842 6519932.93 361297.74 347.88 90 269.53 ‐60
WID1843 6519933.51 361309.6 347.14 106 269.53 ‐60
WID1844 6519934.09 361320.1 346.47 116 269.53 ‐60
WID2209 6519833.27 361336.2 349.27 215 257.53 ‐74.5
WID2211 6519913.52 361389.53 344.75 248.8 263.16 ‐52.05
WID2213 6519913.52 361389.62 344.75 234.3 266.53 ‐47
WID2215 6519781.56 361282.93 358.58 150 89.53 ‐44.5
WID2217 6519781.55 361281.01 358.85 175 90.53 ‐53.6
WID2221 6519953.63 361365.97 344 209.5 267.27 ‐46.61
WID2223 6519953.63 361365.97 344 228 265.5 ‐52.29
WID2225 6519953.63 361365.97 344 244 268.88 ‐57.74
WID2227 6519953.63 361365.18 344 326 264.53 ‐64
WID2229 6519956.24 361444.31 343.86 462 264.53 ‐60
WID2231 6520001.02 361377.67 342.66 469 266.55 ‐61.19
WID2267 6519936.31 361444.69 344 531 269.53 ‐64
WID2269 6519905.22 361434.48 343.37 451 263.53 ‐60
WID2271 6519905.21 361433.82 343.4 505 273.53 ‐62.9
WID2273 6519909.39 361060.31 372 540 84.53 ‐55.9
WID2350 6519829.78 361283.01 354.72 125 86.53 ‐46.9
WID2351 6519829.78 361283.01 354.72 133 86.5 ‐54.12
WID2351A 6519829.78 361283.01 354.72 133 89.53 ‐56
Zabel deposit, McEwen and McEwen Hangingwall deposits
Hole_ID Hole_Type Depth Dip AMG_Azi AMG_East AMG_North RL
WD3303 DDH 339.850 ‐44.00 80.53 358410.410 6525864.070 322.740
WD3309 DDH 293.830 ‐51.00 80.53 358375.960 6525981.220 322.770
WD3312 DDH 299.920 ‐53.50 80.53 358327.680 6526095.210 326.390
WD3837 DDH 267.000 ‐47.00 260.53 358670.290 6525966.740 324.390
WD3839 DDH 256.030 ‐27.00 260.53 358729.150 6525975.150 321.010
WD3841 DDH 253.290 ‐28.50 80.53 358395.860 6526168.320 325.890
WD3842 DDH 260.300 ‐37.00 80.53 358524.210 6525779.700 321.990
WD3848 DDH 199.950 ‐39.00 80.53 358450.420 6525992.970 322.320
WD3849 DDH 184.400 ‐44.00 80.53 358503.610 6525875.840 322.140
WD4111 DDH 294.130 ‐36.00 80.53 358765.010 6525210.140 323.890
WD4118 DDH 259.990 ‐35.50 80.53 359153.110 6524342.730 322.150
WD4124 DDH 174.650 ‐44.00 80.53 359100.670 6524369.990 325.190
WD4128 DDH 255.120 ‐39.50 80.53 358776.980 6525119.450 323.890
WD4130 DDH 189.890 ‐44.00 80.53 359106.000 6524399.250 324.410
For
per
sona
l use
onl
y
Hole_ID Hole_Type Depth Dip AMG_Azi AMG_East AMG_North RL
WD4132 DDH 201.470 ‐53.00 80.53 359077.320 6524325.000 324.460
WD4135 DDH 200.900 ‐45.00 80.53 358737.040 6525359.960 323.890
WD4140 DDH 223.420 ‐54.00 80.53 359055.030 6524272.460 321.420
WD4141 DDH 213.700 ‐46.00 80.53 358842.030 6525006.680 323.190
WD4144 DDH 247.800 ‐45.00 94.53 359047.710 6524389.540 320.860
WD4145 DDH 302.970 ‐41.00 79.53 358725.870 6525110.960 323.890
WD4149 DDH 125.880 ‐50.00 80.53 359182.380 6524445.340 320.500
WD4460 DDH 76.200 ‐90.00 359.53 358657.180 6525840.990 324.390
WD4473 DDH 73.150 ‐90.00 359.53 358697.220 6525785.860 324.390
WD4474 DDH 60.960 ‐90.00 359.53 358682.190 6525783.350 324.390
WD4738 DDH 57.910 ‐90.00 359.53 358456.830 6525931.290 325.890
WD4739 DDH 67.060 ‐90.00 359.53 358441.810 6525928.800 325.890
WD4740 DDH 54.860 ‐90.00 359.53 358426.770 6525926.310 325.890
WD4750 DDH 60.960 ‐90.00 359.53 358717.190 6525665.590 324.390
WD4794 DDH 57.910 ‐90.00 359.53 358702.160 6525663.100 324.390
WD4798 DDH 45.720 ‐90.00 359.53 358431.820 6525988.930 325.890
WD4978 DDH 50.290 ‐90.00 359.53 359227.470 6524452.830 324.890
WD4986 DDH 35.050 ‐90.00 359.53 359362.760 6524475.290 322.390
WD5119 DDH 44.200 ‐90.00 359.53 359257.540 6524457.820 324.890
WD5164 DDH 30.480 ‐90.00 359.53 359347.720 6524472.800 323.090
WD5302 DDH 213.360 ‐43.00 77.03 359212.440 6524450.340 320.680
WD5304 DDH 306.630 ‐49.00 65.53 358708.910 6525231.720 323.890
WD5310 DDH 307.850 ‐42.00 79.03 358664.890 6525347.990 324.390
WD5312 DDH 356.620 ‐36.00 80.53 358620.220 6525216.990 324.390
WD5313 DDH 250.850 ‐48.00 77.03 358982.750 6524305.780 321.040
WD5315 DDH 202.000 ‐41.00 80.53 358844.610 6525130.680 323.390
WD5318 DDH 302.670 ‐48.00 84.03 358927.550 6524362.200 321.100
WD5321 DDH 378.300 ‐41.00 80.53 358644.690 6525097.490 324.390
WD5323 DDH 99.360 ‐50.50 80.53 359203.070 6524387.020 323.230
WD5325 DDH 308.800 ‐49.00 80.53 358751.850 6524991.710 323.890
WD5329 DDH 136.250 ‐52.00 80.53 358798.200 6525246.540 323.890
WD5330 DDH 293.220 ‐51.00 80.53 358949.930 6524256.610 321.350
WD5337 DDH 409.040 ‐35.00 64.53 358819.290 6524343.310 321.230
WD5338 DDH 173.130 ‐45.80 80.53 358702.050 6525477.730 324.390
WD5341 DDH 382.520 ‐49.50 55.53 358660.150 6524976.480 324.390
WD5342 DDH 474.570 ‐40.50 80.53 358543.560 6525204.260 324.890
WD5343 DDH 242.930 ‐56.50 94.53 358799.650 6524999.640 323.390
WD5344 DDH 384.660 ‐45.50 80.53 358874.910 6524285.600 321.170
WD5466 DDH 51.820 ‐90.00 359.53 358411.740 6525923.810 325.890
WD5467 DDH 57.910 ‐90.00 359.53 358396.710 6525921.310 325.890
WD5493 DDH 53.340 ‐90.00 359.53 359297.580 6524402.680 324.890
WD5494 DDH 59.440 ‐90.00 359.53 359247.550 6524517.950 323.890
WD5496 DDH 41.150 ‐90.00 359.53 359307.680 6524527.930 319.630
WD5803 DDH 410.600 ‐41.50 80.53 358553.660 6525329.510 324.890
WD5804 DDH 283.460 ‐44.00 80.53 358760.960 6525055.010 323.890
WD5810 DDH 318.210 ‐72.50 67.53 359050.250 6524266.160 325.390
WD5813 DDH 202.400 ‐50.00 80.53 358767.770 6525303.280 323.890
WD5818 DDH 247.800 ‐81.00 260.53 359111.730 6524275.190 324.870
WD5819 DDH 332.540 ‐56.50 80.53 358723.890 6524987.060 323.890
WD5820 DDH 92.960 ‐87.00 80.53 359236.570 6524416.650 325.390
WD5821 DDH 304.800 ‐48.00 80.53 358734.770 6524927.090 324.390
WD5822 DDH 102.110 ‐86.00 80.53 359242.400 6524288.480 325.390
For
per
sona
l use
onl
y
Hole_ID Hole_Type Depth Dip AMG_Azi AMG_East AMG_North RL
WD5824 DDH 356.620 ‐46.50 80.53 358678.730 6525041.350 324.390
WD5826 DDH 185.930 ‐61.00 80.53 358883.910 6525075.420 323.390
WD5830 DDH 565.400 ‐37.00 80.53 358435.410 6525309.880 325.890
WD5832 DDH 225.550 ‐58.50 80.53 358829.040 6525066.310 323.890
WD6052 DDH 47.240 ‐90.00 359.53 359322.710 6524530.420 319.590
WD6053 DDH 50.290 ‐90.00 359.53 359292.640 6524525.440 319.600
WD6054 DDH 48.770 ‐90.00 359.53 359307.680 6524527.930 319.630
WD6055 DDH 33.530 ‐90.00 359.53 359322.710 6524530.420 319.590
WD6262 DDH 83.820 ‐90.00 359.53 359366.150 6524470.560 321.140
WD6513 DDH 51.820 ‐90.00 359.53 359312.610 6524405.180 324.390
WD6519 DDH 57.910 ‐90.00 359.53 359240.000 6524470.350 324.390
WD6522 DDH 65.530 ‐90.00 359.53 359262.580 6524520.440 323.690
WD6523 DDH 54.860 ‐90.00 359.53 359292.640 6524525.440 319.600
WD6524 DDH 45.720 ‐90.00 359.53 359322.710 6524530.420 319.590
WD8016 DDH 47.240 ‐90.00 359.53 359282.550 6524400.190 325.390
WD8017 DDH 48.770 ‐90.00 359.53 359369.740 6524433.200 322.390
WD8020 DDH 50.290 ‐90.00 359.53 359269.580 6524478.350 324.390
WD8130 DDH 436.200 ‐42.50 80.53 358596.480 6524904.120 323.890
WD8133 DDH 189.590 ‐52.25 80.53 359066.440 6524455.420 320.970
WD8137W1 DDH 431.000 ‐44.00 80.53 358591.240 6525026.820 323.890
WD8138 DDH 215.200 ‐38.00 80.53 358800.960 6525185.220 323.890
WD8142 DDH 195.070 ‐52.75 80.53 359090.880 6524278.210 324.770
WD8143 DDH 296.300 ‐48.00 80.53 358684.190 6525289.400 323.890
WD8148 DDH 217.630 ‐39.00 80.53 358702.110 6525415.940 323.890
WD8149 DDH 228.600 ‐51.75 80.53 358984.830 6524371.920 321.510
WD8150 DDH 256.030 ‐55.00 80.53 358704.270 6525354.520 323.890
WD8152 DDH 302.970 ‐48.00 80.53 358923.330 6524294.870 321.130
WD8156 DDH 290.170 ‐41.00 80.53 358727.610 6525173.040 323.890
WD8159 DDH 448.100 ‐44.25 80.53 358582.770 6525087.200 323.890
WD8160 DDH 554.130 ‐40.50 80.53 358440.380 6525185.580 323.890
WD8162 DDH 375.210 ‐50.00 80.53 358619.260 6525278.620 323.890
WD8163 DDH 252.700 ‐48.00 80.53 358652.200 6525407.660 323.890
WD8164 DDH 438.000 ‐50.00 80.53 358585.720 6524840.550 323.890
WD8165 DDH 566.930 ‐38.50 80.53 358468.340 6524944.630 323.890
WD8166 DDH 423.100 ‐45.50 80.53 358593.830 6525150.820 323.890
WD8167 DDH 175.260 ‐45.00 260.53 359444.760 6524519.430 318.090
WD8168 DDH 327.660 ‐50.00 80.53 358592.070 6525397.680 323.890
WD8172 DDH 457.200 ‐38.50 80.53 358533.270 6525264.340 323.890
WD8174 DDH 403.560 ‐39.75 80.53 358531.350 6525387.590 323.890
WD8175 DDH 155.750 ‐52.00 80.53 359113.220 6524331.360 325.060
WD8176 DDH 161.850 ‐54.50 260.53 359454.340 6524459.760 317.290
WD8177 DDH 354.180 ‐44.50 80.53 358659.060 6525161.660 323.890
WD8178 DDH 273.100 ‐55.50 260.53 359514.150 6524531.610 317.170
WD8179 DDH 224.030 ‐47.50 80.53 358663.570 6525471.330 323.890
WD8180 DDH 487.680 ‐49.50 80.53 358495.460 6525320.840 324.880
WD8181 DDH 177.390 ‐48.25 260.53 359434.370 6524580.020 317.220
WD8182 DDH 360.880 ‐40.00 80.53 358602.350 6525337.590 324.890
WD8183 DDH 545.590 ‐37.75 80.53 358470.320 6525068.530 322.040
WD8186 DDH 217.020 ‐54.00 260.53 359522.910 6524470.830 317.230
WD8189 DDH 110.950 ‐57.00 80.53 359159.340 6524468.630 320.900
WD8192 DDH 248.410 ‐55.50 260.53 359498.600 6524590.760 316.960
WD8199 DDH 364.240 ‐47.50 260.53 359597.340 6524544.310 316.480
For
per
sona
l use
onl
y
Hole_ID Hole_Type Depth Dip AMG_Azi AMG_East AMG_North RL
WD9697 DDH 32.920 ‐90.00 359.53 359255.040 6524472.850 320.670
WD10709 DDH 391.670 ‐46.50 260.53 359615.500 6524485.960 316.200
WD10714 DDH 346.560 ‐63.00 260.53 359503.300 6524652.120 316.800
WD10728 DDH 350.820 ‐55.00 259.53 359558.510 6524569.010 317.000
WD10731 DDH 254.050 ‐66.00 260.53 359452.870 6524653.300 317.310
WDC019 RC 90.000 ‐58.57 265.50 359343.000 6524517.400 321.250
WDC020 RC 140.000 ‐62.74 272.38 359392.600 6524518.400 319.520
WDC022 RC 250.000 ‐60.94 271.18 359501.200 6524480.000 317.420
WDC024 RC 160.000 ‐60.00 90.00 359160.500 6524280.900 325.080
WDC026 RC 220.000 ‐60.00 90.00 359040.000 6524320.000 323.330
WDC027 RC 202.000 ‐60.00 90.00 359038.300 6524359.600 322.570
WDC028 RC 220.000 ‐60.00 90.00 359026.000 6524400.400 322.550
WDC033 RC 170.000 ‐64.18 99.10 358600.000 6525850.000 320.000
WDC035 RC 200.000 ‐60.00 270.00 359477.100 6524441.300 320.000
WDC036 RC 110.000 ‐60.00 270.00 359348.900 6524482.700 320.000
WDC037 RC 150.000 ‐60.00 270.00 359398.700 6524481.200 320.000
WDC038 RC 80.000 ‐60.00 270.00 359300.300 6524523.700 320.000
WDC039 RC 200.000 ‐60.00 270.00 359458.600 6524522.100 320.000
WDC041 RC 120.000 ‐60.00 90.00 359162.800 6524443.200 323.700
WDC043 RC 120.000 ‐60.00 90.00 359203.400 6524481.100 323.200
WDC047 RC 120.000 ‐60.00 90.00 359200.900 6524283.400 324.000
WDC049 RC 163.000 ‐53.83 81.18 359140.400 6524323.600 324.000
WDC050 RC 120.000 ‐60.00 90.00 359159.600 6524364.000 325.600
WDC051 RC 100.000 ‐60.00 90.00 359185.800 6524518.800 324.500
WDC052 RC 160.000 ‐60.00 90.00 359123.000 6524441.900 323.600
WDC053 RC 240.000 ‐60.00 90.00 359041.700 6524440.300 324.300
WDC088 RC 192.000 ‐54.98 84.47 359060.000 6524440.000 320.000
WDC089 RC 212.000 ‐62.41 88.79 359020.000 6524440.000 320.000
WDC090 RC 220.000 ‐58.39 89.36 359040.000 6524480.000 320.000
WDC091 RC 208.000 ‐57.30 89.79 359010.000 6524480.000 320.000
WDC095 RC 219.000 ‐57.81 87.37 359000.000 6524360.000 320.000
WDC096 RC 192.000 ‐52.31 84.65 359080.000 6524320.000 320.000
WDC101 RC 180.800 ‐56.41 83.47 358500.000 6526000.000 320.000
WDC102 RC 249.000 ‐60.73 88.43 358460.000 6526000.000 320.000
WDC104 RC 120.000 ‐57.60 90.34 358560.000 6525925.000 320.000
WDC106 RC 150.000 ‐59.92 89.66 358550.000 6525875.000 320.000
WDC119 RC 100.000 ‐60.12 90.92 358618.000 6525881.000 321.000
WDC120 RC 120.000 ‐63.48 90.96 358580.000 6525940.000 321.000
WDC121 RC 80.000 ‐56.89 89.82 358620.000 6525919.000 322.000
WDC122 RC 120.000 ‐59.55 90.20 358560.000 6525979.000 322.000
WDC123 RC 140.000 ‐57.45 87.11 358499.000 6526059.000 323.000
WDC124 RC 160.000 ‐56.80 83.81 358509.000 6526017.000 324.000
WDC125 RC 100.000 ‐60.00 90.00 358580.000 6526000.000 321.000
WDC126 RC 140.000 ‐60.00 90.00 358479.000 6526099.000 321.000
WDC127 RC 168.000 ‐53.54 87.96 358400.000 6526179.000 322.000
WDC128 RC 220.000 ‐61.39 85.19 358377.000 6526198.000 322.000
WDC130 RC 120.000 ‐58.67 85.92 358678.000 6525659.000 321.000
WDC132 RC 80.000 ‐60.31 90.59 358661.000 6525781.000 322.000
WDC144 RC 252.000 ‐61.99 87.34 359011.000 6524319.000 320.000
WDC182 RC 170.000 ‐58.76 82.40 359095.000 6524440.000 320.000
WDC183 RC 150.000 ‐61.80 96.86 359110.000 6524480.000 320.000
WDC186 RC 175.000 ‐55.21 91.58 358707.000 6525499.000 321.500
For
per
sona
l use
onl
y
Hole_ID Hole_Type Depth Dip AMG_Azi AMG_East AMG_North RL
WDC189 RC 140.000 ‐60.19 88.42 358452.000 6526137.000 325.780
WDD016 DDH 200.000 ‐59.77 88.65 359083.900 6524401.500 324.000
WDD020 DDH 354.700 ‐62.01 272.52 359539.700 6524490.900 319.700
WDD021 DDH 219.700 ‐61.77 272.12 359451.200 6524582.500 318.500
WDD022 DDH 321.600 ‐59.98 276.75 359501.000 6524580.500 318.600
WDD029 DDH 237.700 ‐64.31 85.56 358980.000 6524397.000 320.000
WDD030 DDH 177.700 ‐56.04 89.79 359060.000 6524479.000 320.000
WDD033 DDH 159.600 ‐59.32 84.39 358547.000 6525899.000 322.000
WDD035 DDH 171.600 ‐57.27 83.90 358520.000 6525960.000 323.000
WDD036 DDH 120.600 ‐59.76 85.23 358579.000 6525917.000 322.000
WDD037 DDH 180.600 ‐57.92 86.83 358503.000 6525978.000 323.000
WDD039 DDH 231.700 ‐56.88 87.62 358420.000 6526039.000 323.000
WDD040 DDH 183.800 ‐53.80 83.21 358460.000 6526059.000 324.000
WDD041 DDH 252.800 ‐54.81 87.19 358400.000 6526080.000 323.000
WDD042 DDH 252.700 ‐55.77 87.58 358381.000 6526099.000 322.000
WDD043 DDH 165.700 ‐53.21 87.46 358441.000 6526120.000 320.000
WDD044 DDH 186.400 ‐56.00 92.21 358419.000 6526139.000 320.000
WDD045 DDH 216.700 ‐52.07 86.92 358378.000 6526140.000 320.000
WDD046 DDH 166.000 ‐57.83 86.95 358599.000 6525801.000 320.000
WDD051 DDH 220.000 ‐60.61 89.18 359022.000 6524382.000 321.000
WDD055 DDH 235.000 ‐60.68 83.22 359049.000 6524343.000 323.500
WDD056 DDH 225.500 ‐61.54 89.06 359046.000 6524385.000 322.500
WDD057 DDH 225.700 ‐56.65 89.33 359002.000 6524441.000 320.500
WDD060 DDH 280.000 ‐61.73 90.38 358382.000 6526040.000 325.000
WDD061 DDH 330.500 ‐61.90 89.64 358331.000 6526043.000 322.500
WDD062 DDH 350.000 ‐58.49 88.81 358290.000 6526079.000 325.000
WDD072 DDH 318.500 ‐58.77 87.17 358366.000 6526012.000 324.000
WDD073 DDH 372.500 ‐60.68 88.29 358292.000 6526047.000 324.000
WID1328 DDH 202.600 ‐51.50 83.53 358509.870 6525887.950 322.080
WID1337 RC 115.000 ‐60.00 89.53 358558.250 6525964.800 321.630
WID1339 RC 106.000 ‐60.00 89.53 358576.730 6525908.800 321.690
WID1340 RC 80.000 ‐60.00 89.53 358604.360 6525905.880 321.560
WID1341 RC 115.000 ‐60.00 89.53 358576.480 6525880.710 321.760
WID1342 RC 85.000 ‐60.00 89.53 358605.240 6525877.140 321.530
WID1343 RC 45.000 ‐60.00 89.53 358636.360 6525872.970 321.300
WID1344 RC 110.000 ‐60.00 89.53 358602.150 6525846.950 321.530
WID1346 RC 80.000 ‐60.00 89.53 358632.260 6525844.840 321.310
WID1347 RC 115.000 ‐60.00 89.53 358599.740 6525818.390 321.590
WID1348 RC 80.000 ‐60.00 89.53 358635.300 6525822.130 321.230
WID1349 RC 45.000 ‐60.00 89.53 358657.450 6526028.810 321.230
WID1374 RC 90.000 ‐60.00 89.53 358589.290 6525962.220 321.640
WID1375 RC 54.000 ‐60.00 89.53 358633.870 6525902.420 321.330
WID1376 RC 54.000 ‐60.00 89.53 358660.990 6525816.080 321.260
WID1380 RC 112.000 ‐60.00 89.53 358510.610 6526108.690 321.670
WID1402 DDH 251.000 ‐69.50 67.53 358364.250 6526207.230 322.690
WID1403 DDH 189.200 ‐50.00 72.53 358365.910 6526206.450 322.690
WID1479 DDH 524.200 ‐61.00 83.53 358569.460 6524945.160 321.500
WID1480 DDH 500.500 ‐60.80 93.53 358570.140 6524878.570 321.820
WID1481 DDH 468.000 ‐57.90 73.53 358588.980 6525006.070 321.340
WID1482 DDH 438.100 ‐41.00 88.53 358567.980 6524878.570 321.780
WID1544 RC 86.000 ‐90.00 359.53 359206.470 6524331.100 323.760
WID1545 RC 90.000 ‐90.00 359.53 359228.550 6524332.350 323.330
For
per
sona
l use
onl
y
Hole_ID Hole_Type Depth Dip AMG_Azi AMG_East AMG_North RL
WID1546 RC 82.000 ‐90.00 359.53 359247.890 6524333.510 323.320
WID1547 RC 88.000 ‐90.00 359.53 359268.170 6524334.170 323.000
WID1548 RC 82.000 ‐90.00 359.53 359286.770 6524335.110 322.750
WID1550 RC 70.000 ‐90.00 359.53 359230.710 6524385.930 323.300
WID1551 RC 82.000 ‐90.00 359.53 359249.850 6524383.550 322.900
WID1552 RC 82.000 ‐90.00 359.53 359270.610 6524388.360 322.990
WID1553 RC 64.000 ‐90.00 359.53 359288.630 6524387.270 323.090
WID1554 RC 74.000 ‐90.00 359.53 359313.650 6524383.850 322.480
WID1568 DDH 225.000 ‐45.00 83.53 358395.050 6526041.610 322.540
WID1569 DDH 204.000 ‐68.00 82.53 358504.700 6525968.570 322.090
WID1570 DDH 155.900 ‐44.00 79.53 358503.160 6525968.560 322.110
WID1724 DDH 427.000 ‐57.80 81.53 358663.390 6524825.230 321.200
WID1783 DDH 247.000 ‐58.00 81.53 358388.750 6526110.000 323.010
WID1784 DDH 223.050 ‐58.70 77.53 358390.090 6526146.900 323.080
WID1805 DDH 253.000 ‐52.80 82.53 358387.550 6526110.050 323.070
WID1806 DDH 249.000 ‐64.90 75.53 358389.880 6526146.820 323.090
WID1807 DDH 288.000 ‐67.80 76.53 358389.880 6526146.820 323.090
WID1818 DDH 283.000 ‐65.20 84.53 358387.860 6526110.090 322.910
WID1819 DDH 211.000 ‐50.00 89.53 358389.360 6526109.890 323.020
WID1820A DDH 168.800 ‐45.00 87.53 358526.060 6525936.080 322.390
WID1822 DDH 175.500 ‐56.50 80.53 358552.830 6525848.540 322.190
WID1848 RC 118.000 ‐60.00 89.53 358551.640 6526002.630 322.240
WID1867 RC 118.000 ‐60.00 89.53 358491.290 6526113.580 322.640
WID1869 RC 146.000 ‐60.00 89.53 358445.750 6526153.760 322.870
WID1898 DDH 307.000 ‐68.00 79.53 358337.370 6526163.490 323.270
WID1899 DDH 317.600 ‐67.00 84.53 358374.220 6526078.770 323.690
WID1900 DDH 283.000 ‐58.30 87.53 358374.840 6526078.830 323.660
WID1902 DDH 300.150 ‐55.20 89.53 358377.770 6526026.530 323.180
For
per
sona
l use
onl
y
Appendix 4 – JORC Code (2012 Edition) Drill hole Intersection Information
Note: All composited intersections used in the Mineral Resource estimation are set out below.
Composites created using the mineralisation wireframe boundaries as the cut‐off. Note not all historic
holes have As, Cu and/or Co assays.
132N deposit
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
RCGC_132N_001 50.00 51.00 1.00 1.50 23.00 902.00 250.00
RCGC_132N_001 51.00 52.00 1.00 2.32 37.00 1482.00 328.00
RCGC_132N_001 52.00 53.00 1.00 2.32 37.00 1451.00 327.00
RCGC_132N_001 53.00 54.00 1.00 1.26 38.00 849.00 198.00
RCGC_132N_001 54.00 55.00 1.00 2.01 31.00 1282.00 291.00
RCGC_132N_045 45.99 46.99 1.00 1.18 26.92 1038.46 222.15
RCGC_132N_045 46.99 47.99 1.00 1.78 38.88 1897.40 292.30
RCGC_132N_048 32.02 33.02 1.00 1.07 29.48 834.72 208.05
RCGC_132N_048 33.02 34.01 1.00 2.29 59.88 1491.36 338.98
RCGC_132N_048 34.01 35.01 1.00 7.50 205.12 2594.56 958.65
RCGC_132N_048 35.01 36.01 1.00 10.17 217.87 1951.47 1247.54
RCGC_132N_048 36.01 37.00 1.00 11.76 194.28 12198.82 1529.07
RCGC_132N_048 37.00 38.00 1.00 21.13 348.00 5539.00 2663.00
RCGC_132N_048 38.00 39.00 1.00 7.23 3564.12 2932.76 931.17
RCGC_132N_048 39.00 39.99 1.00 2.70 451.17 1788.27 408.86
RCGC_132N_048 39.99 40.99 1.00 2.49 61.43 1888.02 342.58
RCGC_132N_048 40.99 41.98 1.00 1.03 37.27 671.75 197.87
RCGC_132N_048 41.98 42.98 1.00 1.07 26.18 775.01 204.85
RCGC_132N_051 23.01 24.01 1.00 1.62 10.96 1726.67 198.49
WD3313 62.57 63.83 1.26 1.09 559.29
WD3313 58.13 59.03 0.90 4.10 2616.33
WD3313 59.03 59.93 0.90 1.39 984.22
WD3313 59.93 60.83 0.90 1.12 624.89
WD3323 129.66 130.67 1.01 1.50 1300.00
WD3323 130.67 131.68 1.01 1.04 949.31
WD3323 131.68 132.69 1.01 1.69 1321.88
WD3323 132.69 133.70 1.01 2.33 1488.51
WD3323 133.70 134.71 1.01 2.86 976.93
WD3323 134.71 135.72 1.01 2.50 1098.12
WD3323 111.07 112.52 1.45 1.71 1015.93
WD3330 79.25 80.27 1.02 3.25 2310.00
WD3330 80.27 81.28 1.02 1.95 1841.95
WD3330 81.28 82.30 1.02 0.67 1380.00
WD3330 82.30 83.31 1.02 0.40 542.76
WD3330 83.31 84.33 1.02 0.87 505.00
WD3330 84.33 85.34 1.02 1.34 471.54
WD3330 85.34 86.36 1.02 3.50 940.00
WD3330 86.36 87.37 1.02 2.41 790.98
WD3330 87.37 88.39 1.02 1.30 640.00
WD3330 67.06 68.08 1.02 1.70 1110.00
WD3330 68.08 69.09 1.02 2.24 1658.58
WD3330 69.09 70.11 1.02 2.79 2217.72
WD3330 70.11 71.12 1.02 4.75 4900.00
WD3330 71.12 72.14 1.02 3.43 3450.00
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WD3330 72.14 73.15 1.02 2.10 1996.49
WD3330 73.15 74.17 1.02 0.90 930.00
WD3330 74.17 75.18 1.02 1.01 790.92
WD3330 75.18 76.20 1.02 1.12 650.00
WD3330 62.48 63.25 0.77 1.00 700.00
WD3330 63.25 64.01 0.77 1.00 700.00
WD3330 109.73 110.49 0.76 1.09 780.00
WD3330 110.49 111.25 0.76 1.09 780.00
WD3332 114.30 115.32 1.02 4.00 1900.00
WD3332 115.32 116.33 1.02 7.03 1879.80
WD3332 116.33 117.35 1.02 10.00 1860.00
WD3332 111.26 112.02 0.76 1.15 490.00
WD3332 112.02 112.78 0.76 1.15 490.00
WD3334 79.21 80.23 1.02 1.85 2960.62
WD3334 80.23 81.24 1.02 2.26 3861.48
WD3334 81.24 82.26 1.02 2.66 4770.00
WD4113 148.49 148.96 0.47 10.01 12737.23
WD4133 218.05 219.11 1.06 7.62 1292.20
WD4133 219.11 220.17 1.06 4.72 2617.31
WD4133 220.17 221.22 1.06 6.75 3935.32
WD4133 221.22 222.28 1.06 19.25 12200.00
WD4138 214.87 215.64 0.77 1.14 465.42
WD4138 215.64 216.40 0.77 1.15 470.00
WD4143 233.59 234.42 0.83 2.82 480.00
WD4143 234.42 235.26 0.83 0.37 300.00
WD4143 235.26 236.09 0.83 1.69 552.48
WD4147 279.11 280.09 0.98 1.88 1150.34
WD4147 280.09 281.08 0.98 1.77 1058.51
WD4147 281.08 282.06 0.98 11.33 6171.12
WD4147 275.23 276.06 0.83 1.25 950.00
WD4971 155.68 156.77 1.09 1.57 1395.34
WD4971 156.77 157.87 1.09 2.59 1742.05
WD4971 157.87 158.96 1.09 3.78 1831.06
WD4971 158.96 160.06 1.09 12.55 2417.82
WD4971 160.06 161.15 1.09 7.33 2978.72
WD4971 177.29 178.24 0.95 4.83 2513.08
WD4971 178.24 179.19 0.95 6.28 2834.39
WD4971 179.19 180.13 0.95 8.35 25257.49
WD4971 180.13 181.08 0.95 3.58 1584.18
WD4971 181.08 182.03 0.95 2.41 900.00
WD5303 111.51 112.43 0.92 7.89 1703.91
WD5308 317.41 318.20 0.79 1.68 1863.04
WD5316 283.06 284.02 0.96 1.15 2035.73
WD5316 284.02 284.98 0.96 1.18 670.00
WD5316 288.64 290.13 1.49 1.48 874.03
WD5322 355.03 355.67 0.64 1.50 890.00
WD5322 351.95 353.26 1.31 1.24 955.34
WD5322 347.17 347.93 0.76 1.06 850.00
WD5322 347.93 348.69 0.76 1.06 850.00
WD5345 270.13 271.19 1.05 3.21 2166.75
WD5345 271.19 272.24 1.06 1.88 2058.36
WD5345 272.24 273.30 1.06 7.59 10439.75
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WDC293 58.10 59.08 0.98 1.23 51.92 657.92 154.00
WDC293 59.08 60.05 0.93 1.59 63.00 921.00 214.00
WDC303 102.00 103.02 1.02 2.07 8717.32 373.06 211.44
WDC303 103.02 104.03 1.02 6.62 40775.42 4597.57 430.80
WDC304 110.00 110.99 0.99 2.28 145.00 1403.00 274.00
WDC304 108.00 109.00 1.00 1.15 313.00 665.00 194.00
WDC311 98.01 99.01 1.00 1.82 772.23 6817.88 262.18
WDC316 39.00 39.99 0.99 1.07 57.00 624.00 169.00
WDC316 48.02 49.02 1.00 1.06 16.91 810.58 179.51
WDC316 49.02 50.02 1.00 0.59 115.89 1300.62 101.32
WDC316 50.02 51.01 1.00 4.58 6847.58 1928.13 446.07
WDC316 51.01 52.01 0.99 1.05 1062.00 1702.00 136.00
WDC317 27.01 28.02 1.01 1.32 31.53 1012.66 163.80
WDD102 56.07 57.03 0.96 1.10 37.82 1083.74 179.29
WDD102 57.03 58.00 0.96 1.66 61.00 1190.00 216.00
WDD102 58.00 58.96 0.01 1.66 61.00 1190.00 216.00
WDD102 58.96 59.92 0.92 0.68 25.00 488.00 149.00
WDD102 59.92 60.88 0.96 1.19 36.93 546.74 175.62
WDD102 60.88 61.85 0.96 1.93 91.63 1033.76 235.14
WDD102 61.85 62.81 0.15 2.03 99.00 1100.00 243.00
WDD102 62.81 63.77 0.77 1.76 51.00 1045.00 262.00
WDD102 63.77 64.74 0.96 2.60 47.95 1712.61 339.82
WDD102 64.74 65.70 0.27 2.86 47.00 1920.00 364.00
WDD102 65.70 66.66 0.66 0.78 12.00 401.00 146.00
WDD102 75.69 76.85 1.16 2.20 215.70 1806.10 282.27
WDD102 78.00 79.16 1.16 2.82 62.41 2493.70 360.36
WDD102 76.85 78.00 0.16 2.57 259.77 2228.30 320.17
WDD106 106.04 106.36 0.32 4.24 116.00 3073.75 450.69
WDD106 97.00 97.90 0.90 1.33 29.00 880.00 174.00
WDD106 97.90 98.80 0.50 2.87 49.80 1216.00 304.40
WDD106 98.80 99.70 0.70 9.79 146.00 9090.00 1045.00
WDD106 99.70 100.60 0.30 9.79 146.00 9090.00 1045.00
WDD106 100.60 101.50 0.50 13.05 178.00 3520.00 1255.00
WDD116 164.02 164.73 0.46 1.88 67.00 2050.00 206.00
WDD116 168.90 169.22 0.32 2.05 23.94 684.06 260.50
WDD152 108.67 110.10 1.43 3.79 117.17 3790.24 408.59
WDD152 67.00 68.00 1.00 1.37 3113.00 555.00 139.00
WDD158 131.67 132.59 0.92 3.20 213.00 1791.00 370.00
WDD158 132.59 133.51 0.92 4.48 181.95 1608.34 507.74
WDD158 128.79 129.81 1.02 2.54 3707.94 1969.01 187.23
WDD159 116.99 117.99 1.00 1.00 2208.17 716.51 156.65
WDD159 166.70 167.70 1.00 1.00 46.00 1181.00 150.00
WID1007 108.39 109.44 1.05 2.20 1803.52 188.76
WID1007 109.44 110.49 1.05 6.19 9027.81 558.67
WID1009 207.33 207.99 0.66 4.27 256.82 5385.76 274.39
WID1318 98.00 99.00 1.00 0.95 560.00 100.00
WID1318 99.00 100.00 1.00 0.95 560.00 100.00
WID1318 100.00 101.00 1.00 2.08 4500.00 1310.00 200.00
WID1318 101.00 102.00 1.00 2.08 4500.00 1310.00 200.00
WID1964 204.10 205.15 1.05 1.11 45.00 750.00 190.00
WID1964 205.15 206.20 1.05 1.59 66.43 1088.10 263.81
WID1964 206.20 207.25 1.05 1.06 126.19 812.38 219.29
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WID1964 201.67 202.10 0.43 7.07 1260.00 607.91 505.81
WID1965 182.60 183.60 1.00 1.04 100.00 700.00 200.00
WID1966 197.45 197.85 0.40 1.70 300.00 1130.00 120.00
WID1966 193.45 194.05 0.60 2.01 100.00 840.00 160.00
WID1967 132.66 134.07 1.41 2.82 130.92 2198.16 282.41
WID1967 131.37 131.44 0.07 0.73 37.14 461.43 135.71
WID1967 126.40 126.75 0.35 1.36 50.00 470.00 270.00
WID1967 65.53 66.48 0.95 1.42 6064.08 921.83 171.20
WID1967 66.48 67.42 0.95 1.84 4600.00 1540.00 220.00
WID1967 67.42 68.37 0.95 0.51 572.82 539.86 85.95
WID1967 68.37 69.32 0.95 3.33 633.87 1376.94 339.79
WID1967 69.32 70.26 0.95 0.96 2582.04 396.20 88.80
WID1967 70.26 71.21 0.95 4.26 2120.28 844.15 363.35
WID1967 72.76 73.76 1.00 1.06 128.80 189.20 128.90
WID1967 79.71 80.72 1.01 3.12 50.69 1201.58 455.05
WID1968 74.00 74.90 0.90 2.42 272.22 904.44 183.33
WID1973 77.97 79.05 1.08 4.04 37.78 915.00 447.41
WID1973 72.02 73.02 1.00 1.03 140.75 801.36 140.15
WID1973 73.02 74.01 1.00 1.08 190.10 882.16 148.89
WID2924 191.80 192.82 1.02 1.15 34.46 1180.87 197.12
WID2924 192.82 193.84 1.02 1.11 32.07 1264.13 189.46
WID2924 193.84 194.87 1.02 2.59 1211.41 1888.04 258.91
WID2924 194.87 195.89 1.02 3.82 2069.57 2600.00 304.57
WID2924 195.89 196.91 1.02 4.31 6844.57 4236.09 382.61
WID2924 196.91 197.93 1.02 3.00 3390.76 1593.26 333.80
WID2924 197.93 198.96 1.02 4.08 780.22 3396.74 495.49
WID2924 198.96 199.98 1.02 3.30 1660.00 1750.00 405.00
WID2924 199.98 201.00 1.02 1.48 65.43 3021.74 194.67
WID2927 180.10 181.25 1.15 5.31 54.13 2526.96
WID3029 240.60 241.50 0.90 1.40 22.00 1499.00
WID3029 241.50 242.40 0.90 2.24 483.89 2627.78
WID3029 242.40 243.30 0.90 2.98 1033.33 2040.00
WID3030 37.80 38.90 1.10 1.35 1920.00 140.00
WID3165 334.00 335.00 1.00 2.04 100.00 1360.00 330.00
WID3165 338.00 339.00 1.00 1.36 100.00 2880.00 210.00
WID3165 344.50 345.48 0.98 3.10 100.00 2360.00 370.00
WID3165 345.48 346.46 0.98 2.15 100.00 1538.57 271.43
WID3165 346.46 347.44 0.98 1.12 100.00 542.65 168.98
WID3165 347.44 348.42 0.98 2.75 148.98 912.04 365.10
WID3165 348.42 349.40 0.98 8.27 224.49 8315.10 918.37
WID3168 232.99 233.97 0.98 1.94 959.18 238.47
WID3168 233.97 234.95 0.98 4.75 2191.94 666.12
WID3168 234.95 235.93 0.98 5.01 4513.57 710.61
WID3168 235.93 236.91 0.98 3.93 2278.57 497.76
WID3168 236.91 237.89 0.98 2.16 1908.47 236.02
WID3172 189.72 189.88 0.16 1.00 286.25 139.38
For
per
sona
l use
onl
y
Armstrong deposit
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
AGC0007 69 70 1 13.27 1440 38638 1561
AGC0009 75 76 1 1.2 34 1032 231
AGC0009 76 77 1 1.62 52 1348 227
AGC0009 77 78 1 1.17 68 982 194
AGC0009 78 79 1 1.62 110 1568 234
AGC0009 79 80 1 4.13 314 1905 459
AGC0084 29.64 30.76 1.12 1.12 642.75 82.39 664
AGC0084 30.76 31.88 1.12 1.32 678.21 118.21 720.29
AGC0084 31.88 33 1.12 1.38 580.36 113.04 933.86
AGC0085 29.27 30.202 0.933 1.99 136.49 85.96 1226.53
AGC0085 30.202 31.135 0.933 1.73 108.95 71.53 948.2
AGC0085 31.135 32.068 0.933 1.14 86.01 52.52 411.58
AGC0085 32.068 33 0.933 1.46 99 72 560
AGC0115 35.37 36 0.63 1.07 4046 1024 144
AGC0122 35.3 36.21 0.91 4.09 237.38 3821.62 467.92
AGC0122 36.21 37.12 0.91 6.96 451.52 7752.12 762.27
AGC0122 37.12 38.03 0.91 5.68 579.27 3661.34 620.6
AGC0123 38.07 39.065 0.995 1.23 85.59 865.51 214.75
AGC0123 39.065 40.06 0.995 1.81 132.6 1130.24 289.64
AGC0123 40.06 41.055 0.995 0.98 65.88 718.76 179.2
AGC0123 41.055 42.05 0.995 1.66 98.6 1349.61 251.25
AGC0123 42.05 43.045 0.995 1.75 108.96 1388.28 254.64
AGC0123 43.045 44.04 0.995 1.4 86.44 1151.19 226
AGC0123 44.04 45.035 0.995 1.37 72.79 916.85 229.31
AGC0123 45.035 46.03 0.995 2.07 70.77 1626.03 320.63
AGC0123 46.03 47.025 0.995 2.74 724.86 3390.05 341.48
AGC0123 47.025 48.02 0.995 4.17 20975.54 3098.96 353.93
AGC0124 44.95 45.959 1.009 1.44 126.57 1004.41 283.05
AGC0124 45.959 46.968 1.009 0.78 85.82 400.72 170.03
AGC0124 46.968 47.977 1.009 1.17 105.31 846.61 191.15
AGC0124 47.977 48.986 1.009 1.98 145.1 1723.16 279
AGC0124 48.986 49.995 1.009 1.47 104.57 1133.35 229.7
AGC0124 49.995 51.005 1.009 1.48 94.15 1321.4 236.07
AGC0124 51.005 52.014 1.009 1.72 118.03 1407.16 259.18
AGC0124 52.014 53.023 1.009 2.56 120.56 2998.83 344.46
AGC0124 53.023 54.032 1.009 2.53 143.93 1848.97 323.84
AGC0124 54.032 55.041 1.009 2.44 115.26 1395.58 402
AGC0124 55.041 56.05 1.009 1.17 207.03 830.17 183.1
AGC0129 35.07 36.062 0.992 1.68 86.82 1526.63 240.56
AGC0129 36.062 37.054 0.992 1.6 112.35 1225.83 247.41
AGC0129 37.054 38.047 0.992 1.29 84.19 894.09 218.45
AGC0129 38.047 39.039 0.992 1.04 87.29 3228.46 187.86
AGC0129 39.039 40.031 0.992 1.24 69.81 1306.39 209.6
AGC0129 40.031 41.023 0.992 1.53 63.34 1395.29 227.13
AGC0129 41.023 42.016 0.992 0.96 106.82 764.1 192.32
AGC0129 42.016 43.008 0.992 2.15 4605.18 2089.22 274.5
AGC0129 43.008 44 0.992 2.17 11210 2117 211
AGC0133 35.24 36.127 0.887 1.58 119.43 405.86 249.71
AGC0133 36.127 37.013 0.887 1.15 43.77 340.25 177.11
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
AGC0133 37.013 37.9 0.887 1.29 29 422 250
AGC0148 48 49 1 1.67 2523 1561 251
AGC0148 49 50 1 4.86 1220 2647 523
AGC0148 50 51 1 2.75 13308 2919 257
AGC0163 65 66 1 1.95 1272 1281 265
AGC0163 66 67 1 1.34 4592 653 160
AGC0163 67 68 1 2.16 975 3274 287
AGC0163 68 69 1 1.26 496 1987 149
AGC0175 42 43 1 1.28 526 931 215
AGC0176 47 48 1 1.39 171 1520 212
AGC0176 48 49 1 2.24 537 1986 255
AGC0183 43.4 44 0.6 4.62 233 3486 590
AGC0189 25 26 1 2.27 118 3168 319
AGC0190 34.75 35.875 1.125 6.07 938.89 3066.67 829.56
AGC0190 35.875 37 1.125 1.49 429.33 1358.67 214
AGC0191 41.1 42.05 0.95 2.17 485.26 1316.84 268.58
AGC0191 42.05 43 0.95 1.12 544 576 153
AGC0192 45.97 46.97 1 1.12 58.01 781.41 196.3
AGC0192 46.97 47.97 1 4.15 127.87 2654.76 440.53
AGC0192 47.97 48.97 1 3.99 108.66 3381.3 427.63
AGC0192 48.97 49.97 1 1.34 37.19 1338.81 210.69
AGC0192 49.97 50.97 1 2.81 442.4 1662.03 343.68
AGC0192 50.97 51.97 1 2.13 32.08 9233.21 714.66
AGC0196 37.57 38 0.43 1.33 1397 1840 201
AGC0197 48 49 1 1.57 110 1243 210
AGC0197 49 50 1 2.89 308 1976 325
AGC0197 50 51 1 1.57 350 806 202
AGC0201 32.11 33.07 0.96 11.51 4198.24 4127.97 1375.38
AGC0201 33.07 34.03 0.96 5.19 1675.94 5003.72 614.09
WDC010 99 100 1 1.46 49 1370 197
WDC010 100 101 1 1.35 110 1120 204
WDC010 101 102 1 2.48 135 2210 285
WDC010 102 103 1 0.59 144 636 125
WDC010 103 104 1 2.63 232 1870 243
WDC010 104 105 1 5.35 567 2560 526
WDC010 105 106 1 1.27 878 1970 128
WDC015 146 147 1 1.07 102 895 169
WDC015 147 148 1 1.48 689 863 183
WDC015 148 149 1 1.44 362 895 196
WDC015 149 150 1 1.77 227 1080 237
WDC015 150 151 1 0.76 48 695 140
WDC015 151 152 1 1.62 416 1070 204
WDC015 152 153 1 3.37 231 1540 350
WDC059 96.11 96.99 0.88 1.27 6020 2730 194
WDD001 134 135 1 1.14 125 185 183
WDD001 135 136 1 1.51 180 730 206
WDD001 136 137 1 2.25 325 1480 315
WDD001 137 138 1 1.4 171 549 220
WDD001 139 140 1 3.58 313 1750 456
WDD001 140 141 1 3.21 325 3090 454
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WDD001 141 142 1 1.62 135 562 244
WDD001 142 143 1 2.42 208 1060 374
WDD001 143 144 1 2.31 131 887 313
WDD001 144 145 1 2.54 126 1220 351
WDD001 145 146 0.65 1.47 54 1040 223
WDD001 146 147 1 10.89 378 2520 1350
WDD001 147 148 0.45 1.89 2210 1560 248
WDD003 105 106 1 1.52 140 1030 225
WDD003 106 107 1 2.06 220 1380 287
WDD003 107 108 1 1.25 140 697 184
WDD003 108 109 1 2.11 167 1780 293
WDD003 109 110 1 1.07 86 691 186
WDD003 111 112 1 1.48 102 923 234
WDD003 112 113 1 2.12 127 1690 298
WDD003 113 114 1 1.5 65 1200 188
WDD003 114 115 1 2.98 277 2910 370
WDD003 115 116 1 2.5 1760 2410 303
WDD004 162.06 163.084 0.94 1.57 499 276 222
WDD004 163.084 164.107 0.107 1.38 192 457 203
WDD004 164.107 165.131 1.024 1.46 189.06 524.78 212.08
WDD004 165.131 166.155 1.024 1.92 172.93 1010.1 268.11
WDD004 166.155 167.178 1.024 1.5 183.16 1221.81 231.17
WDD004 167.178 168.202 1.024 1.33 119.31 1450.5 205.71
WDD004 168.202 169.225 1.024 1.02 80.51 771.05 168.29
WDD004 169.225 170.249 1.024 0.8 52.54 679.36 151.46
WDD004 170.249 171.273 1.024 1.16 77.57 914.76 188
WDD004 171.273 172.296 1.024 1.26 136.42 1264.84 192.63
WDD004 172.296 173.32 0.704 1.34 81 835 177
WDD005 220 221 1 1.68 352 1700 296
WDD005 221 222 1 8.02 245 2660 1380
WDD005 222 223 1 1.97 4992.5 1193 283.8
WDD005 223 224 1 10.63 88100 604.5 1210.5
WDD005 224 225 0.4 28.93 384000 1740 2840
WDD005 225 226 0.6 11.95 160666.7 15466.67 765.83
WDD005 226 227 1 13.35 181800 11550 831
WDD006 196.02 197.015 0.98 1.31 49 1070 177
WDD006 197.015 198.01 0.01 1.77 56 6440 220
WDD006 198.01 199.005 0.995 1.77 55.88 6414.22 219.8
WDD006 199.005 200 0.995 1.46 32 1310 180
WDD007 212 212.9 0.9 1.43 1330 1230 201
WDD007 212.9 213.8 0.1 1.43 1330 1230 201
WDD007 213.8 214.7 0.7 4.41 3980 3770 433
WDD008 240 241 1 1.4 211 534 204
WDD008 242 243 1 1.77 193 947 264
WDD008 243 244 1 1.32 134 1300 199
WDD008 244 245 1 1.75 181 1830 258
WDD008 245 246 1 0.98 91 831 172
WDD008 246 247 1 1.49 134 1060 233
WDD008 247 248 1 1.58 106 1090 246
WDD008 248 249 1 1.42 102 1230 219
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WDD008 249 250 1 2.4 118 1830 373
WDD014 190 191 1 2.48 1500 2210 392
WDD015 241.01 242.005 0.995 1.08 4162.1 984.88 213.99
WDD015 242.005 243 0.995 1.84 618 961 212
WDD017 185.1 186.2 1.1 1.73 58 884 225
WDD023 94.03 95.026 0.996 2.21 144.14 2170.11 295.24
WDD023 95.026 96.021 0.996 1.26 74.37 1415.7 191.67
WDD023 96.021 97.017 0.996 1.67 91.5 1255.29 225.17
WDD023 97.017 98.013 0.996 3.29 118.94 3246.63 403.31
WDD023 98.013 99.009 0.996 1.44 38.15 1461.89 198.46
WDD023 99.009 100.004 0.996 2.01 58.51 1690.37 252.64
WDD023 100.004 101 0.996 15.36 558.15 5922.86 1505.24
WDD024 109.94 110.947 0.947 1.27 87 813 181
WDD024 110.947 111.955 1.007 1.61 94.58 1482.99 224.59
WDD024 111.955 112.962 1.007 1.72 75.9 1882.85 227.95
WDD024 112.962 113.969 1.007 2.36 106.75 2082.8 289.57
WDD024 113.969 114.976 1.007 2.2 107.03 1750.74 284.25
WDD024 114.976 115.984 1.007 1.82 82.59 1388.45 259.59
WDD024 115.984 116.991 1.007 1.19 30.84 1330.81 188.17
WDD024 116.991 117.998 1.007 2.33 79.55 2023.68 325.74
WDD024 117.998 119.005 1.002 2.05 308.58 1910.22 267.11
WDD024 119.005 120.013 0.013 4.39 621 5400 474
WDD024 120.013 121.02 1.007 4.31 646.99 5313.03 466.18
WDD025 136.14 137.133 0.993 1.21 121.06 838.94 213.58
WDD025 137.133 138.126 0.993 2.03 193.41 1512.22 264.55
WDD025 138.126 139.119 0.874 1.76 155 1390 234
WDD025 139.119 140.112 0.112 1.23 109 771 166
WDD025 140.112 141.105 0.993 1.35 114.62 890.81 180.75
WDD025 141.105 142.098 0.993 2.34 161.01 1905.95 304.7
WDD025 142.098 143.092 0.993 2.28 152.09 1949.86 302.46
WDD025 143.092 144.085 0.993 2.17 147.04 1798.88 299.59
WDD025 144.085 145.078 0.993 1.55 82.61 1265.65 219.61
WDD025 145.078 146.071 0.993 1.56 80.21 1496.32 222.84
WDD025 146.071 147.064 0.993 2.31 116.65 2088.43 316.96
WDD025 147.064 148.057 0.993 1.71 231.84 2006.55 203.9
WDD025 148.057 149.05 0.943 2.5 295 3430 268
WDD027 139.07 140 0.93 2.09 5.5 10300 409
WDD091 175.75 176.765 1.015 1.67 143.45 1088.28 224.38
WDD091 176.765 177.78 1.015 2.27 78.9 3767.98 328.44
WDD092 189 189.987 0.988 1.41 126 1385 188
WDD092 189.987 190.975 0.988 3.06 311.62 1932.97 366.71
WDD092 190.975 191.963 0.988 2.52 232.13 1686.58 325.14
WDD092 191.963 192.95 0.988 1.46 129.54 988.15 220.3
WDD092 192.95 193.938 0.988 1.13 119.29 814.61 171.32
WDD092 193.938 194.925 0.988 0.9 60.99 1077.22 158.76
WDD092 194.925 195.913 0.988 2.05 114 1376.39 269.84
WDD092 195.913 196.9 0.837 1.96 1697.79 5313.36 208.22
WDD093 193 194.15 1.15 1.62 254 1095 214
WDD094 232 233.16 1.16 1.26 40 850 189
WDD095 246.02 247.08 1.06 1.4 144.21 729.19 223.81
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WDD095 252 252.984 0.984 1.98 144 1125 245
WDD095 252.984 253.968 0.984 4.85 371.01 2420.66 569.83
WDD095 253.968 254.953 0.984 4.43 266.26 3567.86 478.03
WDD095 254.953 255.937 0.984 7.59 495.11 12166.36 816.53
WDD095 255.937 256.921 0.984 5.05 296.44 3831.28 537.34
WDD095 256.921 257.905 0.984 3.56 219.45 4499.3 391.91
WDD095 257.905 258.889 0.984 3.69 235.69 2910.96 416.25
WDD095 258.889 259.874 0.111 3.71 238 2730 420
WDD095 259.874 260.858 0.858 4.37 252 4720 455
WDD095 260.858 261.842 0.142 4.37 252 4720 455
WDD095 261.842 262.826 0.826 4.25 208 3470 460
WDD095 262.826 263.811 0.984 7.13 295.9 3740.16 716.54
WDD095 263.811 264.795 0.984 3.63 158.13 2337.22 384.24
WDD095 264.795 265.779 0.984 2.64 131.84 1522.73 296.6
WDD095 265.779 266.763 0.984 3.61 135.3 2372.3 394.86
WDD095 266.763 267.747 0.484 5.18 152.82 3855 535.77
WDD095 267.747 268.732 0.984 8.21 310.46 2898.72 870.66
WDD095 268.732 269.716 0.984 8.82 405.82 2667.27 875.36
WDD095 269.716 270.7 0.984 11.71 61131.15 4150.53 553.16
WDD166 47 47.991 0.991 0.86 63.4 453.88 150.24
WDD166 47.991 48.981 0.991 0.89 63.69 545.05 167.44
WDD166 48.981 49.972 0.991 1.09 80.62 825.01 184.68
WDD166 49.972 50.963 0.991 1.88 103.4 1117.53 281.78
WDD166 50.963 51.953 0.991 1.96 108 1487 271
WDD166 51.953 52.944 0.991 1.6 94.66 1016.38 229.08
WDD166 52.944 53.934 0.991 2 110.03 1456.12 260.96
WDD166 53.934 54.925 0.991 1.46 74.58 900.4 221.91
WDD166 54.925 55.916 0.991 1.45 65.53 780.44 214.38
WDD166 55.916 56.906 0.991 1.6 84.21 1709.87 226.81
WDD166 56.906 57.897 0.991 1.63 60.65 967.69 219.85
WDD166 57.897 58.888 0.991 0.76 19.51 536.24 132.17
WDD166 58.888 59.878 0.991 2.35 64.3 2079.32 279.1
WDD166 59.878 60.869 0.822 1.51 89.74 1221.54 198.65
WDD166 60.869 61.859 0.659 3.59 310.69 3916.05 438.03
WDD166 61.859 62.85 0.991 2.86 379.14 2905.49 341.83
WDD167 56.3 57.278 0.978 1.17 363.77 759.68 399.36
WDD167 57.278 58.256 0.978 1.47 136.47 516.51 214.31
WDD167 58.256 59.233 0.978 1.63 179.84 837.14 227.25
WDD167 59.233 60.211 0.767 1.77 224 1163 244
WDD167 60.211 61.189 0.189 1.37 143 264 191
WDD167 61.189 62.167 0.978 1.39 144.88 304.23 195.77
WDD167 62.167 63.144 0.978 1.5 158.43 467.35 220.48
WDD167 63.144 64.122 0.978 1.58 190 341.5 232.5
WDD167 64.122 65.1 0.978 1.88 290.3 849.88 254.65
WDD167 65.1 66.078 0.978 1.47 386.52 963.35 222.6
WDD167 66.078 67.056 0.978 1.39 144.5 928.91 214.14
WDD167 67.056 68.033 0.978 1.14 106.31 2173.78 168.27
WDD167 68.033 69.011 0.978 1.02 49.9 484.51 178.87
WDD167 69.011 69.989 0.978 0.99 19 776 163
WDD167 69.989 70.967 0.978 1.71 50.64 1365.23 237.15
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WDD167 70.967 71.944 0.978 9.72 225.72 5354.01 1195.77
WDD167 71.944 72.922 0.978 11 179.75 4048.97 1239.73
WDD167 72.922 73.9 0.978 9.29 384.94 4057.94 1126.09
WDMT005 17.9 18.888 0.988 1.36 73.81 1018.81 218.7
WDMT005 18.888 19.876 0.988 2.02 90 1435 277
WDMT005 19.876 20.864 0.988 2.02 90 1435 277
WDMT005 20.864 21.852 0.988 2.02 90 1435 277
WDMT005 21.852 22.84 0.988 2.02 90 1435 277
WDMT005 22.84 23.828 0.988 2.02 90 1435 277
WDMT005 23.828 24.816 0.988 2.02 90 1435 277
WDMT005 24.816 25.804 0.988 2.37 246.84 1650.68 306.47
WDMT005 25.804 26.792 0.988 5.3 1580 3484 557
WDMT005 26.792 27.78 0.988 5.3 1580 3484 557
WID1001 96 97 0.34 1.43 64 1375 211
WID1001 97 98 1 1.92 71 1525 235
WID1001 98 99 1 2.57 90 2350 313
WID1001 99 100 1 1.94 94 1640 249
WID1002 138.99 139.997 0.997 1.75 158 570 234
WID1002 139.997 141.004 1.007 1.51 139.14 519.41 209.24
WID1002 141.004 142.011 1.007 1.9 160.93 1355.89 250.74
WID1002 142.011 143.018 0.869 1.62 154 513 227
WID1002 143.018 144.025 0.875 1.65 160.79 501.08 235.58
WID1002 144.025 145.032 1.007 1.76 142.35 780.85 260.41
WID1002 145.032 146.038 1.007 1.94 182.17 801.39 271.62
WID1002 146.038 147.045 1.007 1.67 133.57 672.12 237
WID1002 147.045 148.052 1.007 1.43 82.94 939.7 235.91
WID1002 148.052 149.059 1.007 1.57 101.94 1134.41 228.82
WID1002 149.059 150.066 0.941 6.8 365.15 1862.91 918.2
WID1002 150.066 151.073 0.073 9.46 236 11800 1155
WID1002 151.073 152.08 1.007 8.16 196.17 9699.14 990.61
WID1003 95.07 96.018 0.948 1.31 144.68 922.31 169.06
WID1003 96.018 96.966 0.948 0.9 128 520 120
WID1003 96.966 97.913 0.948 0.98 149.2 394.72 177.82
WID1003 97.913 98.861 0.948 1.3 123.65 853.36 207.26
WID1003 98.861 99.809 0.948 0.88 67.91 444.55 135.98
WID1003 99.809 100.757 0.948 0.71 61.38 440.33 106.13
WID1003 100.757 101.704 0.948 0.84 352.38 489.19 149.46
WID1003 101.704 102.652 0.948 0.55 452 375.49 121.83
WID1003 102.652 103.6 0.948 0.94 2600 1143.95 188.21
WID1004 127.19 128.203 1.013 1.19 111.6 760.13 196.05
WID1004 128.203 129.217 1.013 1.54 112.93 954.21 247.17
WID1004 129.217 130.23 1.013 1.41 111.95 1350.1 206.81
WID1004 130.23 131.243 1.013 1.68 120.08 2003.45 232.4
WID1004 131.243 132.257 1.013 1.78 116.79 1200.53 245.07
WID1004 132.257 133.27 1.013 1.87 123.4 1218.75 252.01
WID1004 133.27 134.283 1.013 1.61 107.88 920.76 225.07
WID1004 134.283 135.297 1.013 1.42 80.93 844.9 214.64
WID1004 135.297 136.31 1.013 1.64 76.07 985.76 228.59
WID1004 136.31 137.323 1.013 1.32 43.38 1174.8 195.95
WID1004 137.323 138.337 1.013 1.41 62.61 1500.26 233.32
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WID1004 138.337 139.35 1.013 2.84 149.94 2393.75 321.41
WID1012 180 181 1 1.5 947 1260 260
WID1012 181 182 1 1.28 164.76 1666.4 212.7
WID1012 182 183 1 1.01 228 753.8 181.8
WID1012 183 184 1 1.09 190.32 639.6 202
WID1012 184 185 1 1.18 76.46 1615 185.4
WID1012 185 186 1 6.66 359.8 3318 876
WID1014 174 175 1 1.08 103 710 220
WID1014 175 176 1 1.58 140.1 732 248
WID1014 176 177 1 1.79 88.28 1186 252
WID1014 177 178 1 1.49 82.34 1091.8 221
WID1014 178 179 1 1.49 30 1280 220
WID1014 179 180 1 2.03 40.76 1922.8 252.8
WID1014 180 181 1 2 1620 1440 230
WID1015 197.08 198.09 1.01 2.29 261.45 1428.91 311.98
WID1015 198.09 199.1 1.01 2.63 4850.99 2981.78 286.83
WID1016 139.81 140.792 0.982 1.25 165 110 120
WID1016 140.792 141.775 0.982 0.88 129.51 62.69 112.11
WID1016 141.775 142.757 0.982 1.17 193.2 42.29 117.71
WID1016 142.757 143.739 0.982 1.77 290.25 348.54 120
WID1016 143.739 144.722 0.982 1.99 237.87 1368.17 90.62
WID1016 144.722 145.704 0.982 2.01 181.34 1628.35 115.83
WID1016 145.704 146.686 0.982 1.39 194.45 761.79 123.01
WID1016 146.686 147.668 0.982 1.24 232.22 542.91 120
WID1016 147.668 148.651 0.982 1.6 228.44 861.75 100.13
WID1016 148.651 149.633 0.982 1.55 129.77 1028.67 186.67
WID1016 149.633 150.615 0.982 2.14 145.91 1281.9 292.13
WID1016 150.615 151.598 0.982 11.97 294.6 6951.84 1290.05
WID1016 151.598 152.58 0.982 11.37 660.21 6332.34 1221.28
WID1022 230.04 230.79 0.75 1.25 800 200
WID1024 156.99 157.992 1.002 1.09 74.75 498.8 199.4
WID1024 157.992 158.994 1.002 1.03 60.12 470.24 190.08
WID1024 158.994 159.996 1.002 0.66 35.15 420.3 150.24
WID1024 159.996 160.998 1.002 1.04 223.16 473.65 166.93
WID1024 160.998 162 1.002 0.98 265 790 170
WID1025 183.5 184.56 1.06 2.7 131.89 1743.21 339.81
WID1025 184.56 185.62 1.06 0.82 523.4 632.26 173.4
WID1025 185.62 186.68 1.06 1.08 156.42 799.43 201.7
WID1025 186.68 187.74 1.06 2.02 1563.21 1453.21 265.85
WID1025 187.74 188.8 1.06 8.86 4209.53 4620.94 918.3
WID1039 261.01 261.867 0.857 1.3 50 860 190
WID1039 261.867 262.723 0.857 1.72 54.22 1391.95 240.66
WID1039 262.723 263.58 0.857 1.35 37.55 917.55 193.39
WID1483 264.94 265.894 0.954 4.62 100 5514.36 485.22
WID1483 265.894 266.848 0.954 4.1 100 2615.66 424.47
WID1483 266.848 267.802 0.954 3.62 100 2530.57 370.5
WID1483 267.802 268.756 0.954 3.12 100 1909.48 328.53
WID1483 268.756 269.71 0.954 4.89 163.94 1696.92 493.79
WID1483 269.71 270.664 0.954 7.9 269.6 2663.46 731.36
WID1483 270.664 271.618 0.954 7.76 429.56 2731.45 734.65
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WID1483 271.618 272.572 0.954 9.4 530.19 6387.38 821.61
WID1483 272.572 273.526 0.954 4.99 443.4 8603.31 447.44
WID1483 273.526 274.48 0.954 1.34 300 1560 210
WID1485 223.02 223.877 0.857 1.95 2100 1270 240
WID1485 223.877 224.733 0.857 1.21 2100 1381.28 154.4
WID1485 224.733 225.59 0.857 2.58 6750.58 2237.2 220.78
WID1486 290.5 291.5 1 1.33 100 820 210
WID1486 291.5 292.5 1 1.01 100 680 180
WID1486 297.58 298.522 0.942 1.69 100 1804.23 219.54
WID1486 298.522 299.463 0.942 1.77 100 1685.86 214.76
WID1486 299.463 300.405 0.942 1.52 100 1399.49 195.59
WID1486 300.405 301.347 0.942 1.01 100 647.91 153.68
WID1486 301.347 302.288 0.942 2.29 194.34 1817.5 244.9
WID1486 302.288 303.23 0.942 1.49 200 1397.47 183.84
WID1487 227.05 228.05 1 1.43 251.35 1928 223.7
WID1487 233 234.006 1.006 1.2 199.42 700.46 190
WID1487 234.006 235.012 1.006 1.2 100 774.66 189.65
WID1487 235.012 236.017 1.006 0.83 101.74 325.74 160.52
WID1487 236.017 237.023 1.006 1.27 202.32 671.11 193.48
WID1487 237.023 238.029 1.006 2.76 297.1 1549.27 337.1
WID1487 238.029 239.035 1.006 1.94 206.96 1248.11 245.57
WID1487 239.035 240.041 1.006 3.37 400 2843.76 401.62
WID1487 240.041 241.047 1.006 3.84 395.36 2406.18 439.07
WID1487 241.047 242.052 1.006 3.37 289.56 1292.69 404.86
WID1487 242.052 243.058 1.006 0.89 100 1173.34 135.22
WID1487 243.058 244.064 1.006 1.65 100 1403.4 217.45
WID1487 244.064 245.07 1.006 1.28 100 1551.98 177.22
WID1487 250.08 251.069 0.989 1.3 100 1156.99 207.92
WID1487 251.069 252.057 0.989 1.24 100 700.81 193.87
WID1487 252.057 253.046 0.989 2.5 100 1604.02 308.44
WID1487 253.046 254.034 0.989 3.48 110.4 1394.45 385.95
WID1487 254.034 255.023 0.989 8.83 400 2938.67 828.15
WID1487 255.023 256.011 0.989 1.86 400 4150 750
WID1487 256.011 257 0.989 1.82 217.92 3540.03 258.38
WID1593 325 326.023 1.023 1.37 100 1245.11 244.44
WID1593 326.023 327.046 1.023 1.29 100 1230.66 218.65
WID1593 327.046 328.069 1.023 1.05 100 803.14 188.65
WID1593 328.069 329.092 1.023 0.92 100 584.39 170.9
WID1593 329.092 330.115 1.023 1 100 694.03 178.88
WID1593 330.115 331.138 1.023 0.81 100 415.4 170
WID1593 331.138 332.161 1.023 0.92 100 553.87 171.57
WID1593 332.161 333.184 1.023 1.28 117.99 1131.58 185.4
WID1593 333.184 334.207 1.023 1.56 220.23 1268.45 214.05
WID1593 334.207 335.23 1.023 3.42 585.44 2155 394.13
WID1679 218.11 219.04 0.93 1.88 2013.98 473.87 245.7
WID1720 317 318 1 1.1 100 750 190
WID1720 318 319 1 1.06 100 806 190
WID1720 319 320 1 2.1 100 1213 268
WID1720 320 321 1 5.43 140 2220 514
WID1720 321 322 1 5.21 240 2100 474
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WID3460 148.02 149.035 1.015 14.65 261.55 9562.07 1893.28
WID3460 149.035 150.05 1.015 2.05 158.6 2763.05 292.44
WID3461 123.96 125.01 1.05 4.72 409.86 759.86 554.81
WID3464 97 98 1 1.05 230 1030 155
WID3464 98 99 1 2.4 660 1140 240
Cooke deposit
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WD5336 55.78 57.3 1.52 0.50 380
WD5336 111.4 116.43 5.03 1.77 1690
WD5339 267.92 269.44 1.52 0.50 470
WD5340 139.9 148.93 9.03 1.01 994
WD5340 149.08 152.4 3.32 2.04 1015
WD5340 172.21 173.74 1.53 0.74 560
WD5348 131.98 133.5 1.52 0.57 250
WD5348 150.27 151.79 1.52 0.66 480
WD5350 192.94 197.51 4.57 0.60 514
WD5350 207.17 208.48 1.31 2.07 2660
WD5408 7.62 19.81 12.19 1.05 406
WD5408 21.34 22.86 1.52 0.61 290
WD5409 3.05 12.19 9.14 1.09 6265
WD5419 0 10.67 10.67 1.10 1213
WD5419 33.53 35.05 1.52 0.55 500
WD5420 10.67 18.29 7.62 1.68 1935
WD5420 41.15 51.82 10.67 1.50 1891
WD5421 12.19 13.72 1.53 0.50 240
WD5421 19.81 28.96 9.15 1.00 1063
WD5423 7.62 21.34 13.72 1.15 2015
WD5423 27.43 30.48 3.05 0.73 1551
WD5423 35.05 50.29 15.24 0.99 1417
WD5424 0 1.52 1.52 0.54 540
WD5424 3.05 6.1 3.05 0.69 625
WD5428 10.67 18.29 7.62 1.43 1712
WD5429 13.72 15.24 1.52 0.86 990
WD5429 30.48 39.62 9.14 1.63 1694
WD5429 42.67 44.2 1.53 0.54 520
WD5430 4.57 7.62 3.05 1.16 1172
WD5802 266.09 268.83 2.74 0.57 275
WD5802 313.82 314.95 1.13 0.66 560
WD5802 329.18 330.71 1.53 0.52 240
WD5802 331.9 333.54 1.64 0.71 246
WD6059 77.72 82.3 4.58 0.62 517
WD6059 85.34 88.39 3.05 0.76 510
WD6257 30.48 41.15 10.67 0.98 1429
WD6257 53.34 56.39 3.05 0.95 795
WD6258 94.49 97.54 3.05 0.72 640
WDC145 13 14 1 0.53 51 372 142
WDC145 15 21 6 0.77 214 894 297
WDC145 22 24 2 0.71 454 1270 321
WDC146 13 14 1 0.56 1360 2040 417
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WDC146 54 55 1 0.50 6 395 184
WDC146 77 79 2 0.59 11 1023 236
WDC147 36 54 18 1.71 37 1850 456
WDC147 64 78 14 1.60 83 2353 474
WDC147 79 80 1 0.55 21 876 198
WDC147 81 82 1 0.69 286 752 246
WDC148 5 6 1 0.58 100 1575 200
WDC148 19 38 19 2.49 70 4243 712
WDC148 43 44 1 0.59 13 768 225
WDC148 53 69 16 1.42 21 1871 419
WDC148 72 73 1 1.16 8 1455 338
WDC148 74 75 1 1.09 11 1165 315
WDC149 18 19 1 0.68 1300 3950 242
WDC149 22 24 2 1.05 212 1002 447
WDC150 1 15 14 1.40 92 2556 479
WDC150 16 28 12 1.09 179 1563 376
WDC150 51 53 2 0.61 7 932 214
WDC150 54 56 2 2.78 73 3875 857
WDC159 0 16 16 3.23 55 5304 835
WDGT02 78 83 5 2.13 38 3321 636
WDMT01 37.6 44 6.4 2.43 27 2753 707
WDMT01 47.7 53 5.3 2.01 156 3558 600
WDMT01 70 87 17 1.57 42 1888 506
WDMT02 8 11 3 4.20 82 5180 824
WDMT02 12 22 10 1.54 79 4686 447
WDMT02 23 26 3 0.99 114 23 202
WDMT02 31 33 2 0.63 111 1458 170
WDMT02 39 46 7 1.29 10 1571 419
WDMT03 31 47 16 1.99 29 2606 568
WDMT03 70 77 7 1.94 13 1614 612
WID1237 104 114 10 1.19 1398 320
WID1237 118 120 2 0.64 770 220
WID1423 137 138 1 1.23 100 2031 368
WID1423 142.3 146.2 3.9 2.25 100 2090 451
WID1423 155.5 156.5 1 0.72 100 1675 295
WID1423 179.9 180.9 1 0.51 100 220 160
WID1423 199.5 204 4.5 1.80 100 2017 574
WID1645 8 30 22 1.58 100 3259 379
WID1648 27 40.5 13.5 1.53 43 1200 458
WID1648 42 43.5 1.5 0.50 0 380 170
WID1649 0 6 6 0.64 100 573 217
WID1649 8 28 20 0.65 100 802 220
WID1649 42 60 18 1.47 100 2470 423
WID1649 68 70 2 0.58 100 730 200
WID1650 32 52 20 2.08 190 2735 518
WID1650 66 86 20 1.21 100 1368 363
WID1651 24 28 4 1.18 100 1365 405
WID1652 42 50 8 2.36 125 2675 695
WID1653 16 18 2 0.74 100 1450 370
WID1653 22 24 2 0.55 100 760 240
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WID1654 10 18 8 0.96 100 1408 328
WID1655 2 10 8 0.59 100 585 208
WID1655 22 32 10 1.51 100 1828 496
WID1655 34 36 2 0.97 100 1310 380
WID1656 10 16 6 0.57 100 620 227
WID1656 34 38 4 1.21 150 2135 430
WID1656 42 46 4 1.10 200 1120 210
WID1656 54 56 2 0.52 200 350 160
WID1657 2 6 4 0.75 100 1120 290
WID1658 14 18 4 0.84 250 1490 445
WID1658 26 28 2 0.53 100 580 230
WID1659 20 22 2 0.54 200 800 240
WID1659 26 46 20 0.87 490 1217 325
WID1659 56 62 6 0.71 133 953 243
WID1675 69.3 72.3 3 0.58 100 675 217
WID1675 86.8 97 10.2 1.17 3385 1282 297
WID1675 99.5 100.5 1 0.52 100 1160 190
WID1779 77.35 78.45 1.1 0.51 470 190
WID1779 84.7 85.8 1.1 0.54 650 210
WID1779 109.1 110.15 1.05 2.98 2870 860
WID1781 0 19 19 2.38 105 3781 696
WID1781 39 45 6 1.04 100 1278 328
WID1781 46 47 1 0.84 100 730 230
WID1781 50 52 2 0.71 100 1150 230
WID1781 53 54 1 0.55 3700 520 180
WID1791 52 58 6 1.85 1430 553
WID1791 68 70 2 0.79 1110 260
WID1793 58 70 12 1.38 4350 1007 290
WID1793 74 78 4 0.98 1320 285
WID1794 20 22 2 0.57 610 200
WID1794 34 54 20 0.83 80 1084 267
WID1794 58 60 2 0.53 670 210
WID1794 62 64 2 0.51 390 170
WID1794 68 78 10 0.71 702 226
WID1795 22 34 12 0.95 5595 313
WID1795 64 70 6 0.54 660 203
WID1795 76 78 2 0.57 500 190
WID1795 82 92 10 1.99 2430 472
WID1795 104 106 2 0.56 720 190
WID1796 58 62 4 0.73 725 240
WID1796 92 96 4 0.68 1450 310
WID1796 134 144 10 1.16 60 1774 322
WID1797 18 22 4 0.72 1155 320
WID1798 30 32 2 0.53 710 210
WID1798 36 38 2 1.05 1340 400
WID1800 58 60 2 0.54 350 190
WID1800 62 64 2 1.18 790 420
WID1801 68 70 2 0.59 780 200
WID1801 74 84 10 0.86 1072 284
WID1801 94 96 2 0.66 740 220
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WID1836 86.85 91 4.15 2.23
WID1837 71.35 87.55 16.2 2.07 121 3393 455
WID1838 28 34 6 1.14 42 2063 370
WID1839 48 70 22 2.17 252 2724 591
WID1842 50 52 2 0.60 710 240
WID1843 48 52 4 0.68 610 245
WID1843 68 70 2 0.53 440 190
WID1843 74 78 4 1.07 2340 370
WID1844 54 56 2 0.55 450 200
WID1844 94 102 8 0.60 653 258
WID2209 72.3 101.15 28.85 1.95 100 2356 484
WID2209 104.35 107.3 2.95 2.18 344 2532 483
WID2211 164.55 167.7 3.15 2.40 1711 243 661
WID2221 129 131.9 2.9 0.68 100 540 210
WID2221 149.5 151.2 1.7 0.58 100 762 245
WID2223 144.6 147.6 3 0.69 0 893 257
WID2223 169 170.5 1.5 0.57 233 447 203
WID2225 151 166.4 15.4 0.65 100 1355 226
WID2225 179.5 180.5 1 0.60 100 510 265
WID2225 181 183.5 2.5 0.61 100 574 242
WID2225 184.5 190.25 5.75 1.25 100 1955 443
WID2227 206.6 207.6 1 3.13 74350 975 620
WID2227 209.4 215.2 5.8 1.40 10758 1108 384
WID2227 218.2 221.4 3.2 0.56 2288 235 161
WID2227 224.2 225.2 1 1.08 100 1084 310
WID2227 226.35 227.5 1.15 0.52 800 340 190
WID2227 240.65 241.65 1 0.62 200 510 190
WID2229 412.55 418.6 6.05 3.38 100 4027 610
WID2231 308.6 319.5 10.9 1.44 100 1734 433
WID2231 321.7 335.25 13.55 1.38 100 1890 419
WID2267 210.55 211.65 1.1 0.52 100 980 350
WID2269 302.7 303.75 1.05 0.63 300 700 250
WID2271 377 378 1 0.53 100 670 190
WID2350 48 55 7 1.10 100 1893 310
WID2351A 57 66 9 2.08 55 2368 551
WID2652 133 135 2 0.54 100 695 205
WID2652 136 147 11 0.88 100 1107 322
WID2652 148 164 16 0.73 100 898 268
WID2652 165 167 2 0.68 100 715 245
WID2652 185.3 189 3.7 1.25 1381 1175 372
WID2653 203.7 205 1.3 1.77 100 2465 580
WID2653 207.4 208.7 1.3 1.28 100 1370 358
WID2657 151 153 2 0.55 350 900 205
WID2657 157 159.8 2.8 1.03 764 891 273
WID2657 164 169 5 1.34 480 1456 402
WID2657 169.2 170.2 1 0.75 980 924 198
WID2658 244 245 1 0.53 35 490
WID2658 247.5 250.2 2.7 2.27 37 2261
WID2658 254 261 7 1.15 33 1899
WID2812 252 254 2 0.85 100 735 370
For
per
sona
l use
onl
y
Hole_ID mFrom mTo Width Ni_pct As_ppm Cu_ppm Co_ppm
WID2814 232.9 235.8 2.9 1.78 46 2707
WID2814 236.6 241.2 4.6 1.22 31 1308
WID2815 254.8 256.2 1.4 0.56 314 391 191
WID2815 269 270 1 0.55 100 1570 170
Zabel deposit, McEwen and McEwen Hangingwall deposits
Hole_ID From To Width Ni_pct As_ppm Cu_ppm Co_ppm
WD3303 19.810 27.430 7.62 0.716 0.00 100.04 0.00
WD3309 260.330 262.590 2.26 0.550 0.00 532.70 0.00
WD3312 269.750 272.490 2.74 1.083 0.00 1568.28 0.00
WD3837 72.240 82.200 9.96 1.336 0.00 45638.96 0.00
WD3839 202.080 205.560 3.48 0.814 0.00 545.52 0.00
WD3841 140.970 142.650 1.68 1.928 0.00 5806.25 0.00
WD3842 173.280 174.800 1.52 1.565 0.00 2858.16 0.00
WD3848 165.510 168.040 2.53 1.206 0.00 2461.15 0.00
WD3849 152.950 155.200 2.25 0.593 0.00 499.60 0.00
WD4111 75.220 77.110 1.89 0.878 0.00 980.95 0.00
WD4111 108.510 124.970 16.46 0.774 0.00 482.11 0.00
WD4118 97.320 101.710 4.39 1.317 0.00 1832.35 0.00
WD4124 132.280 138.070 5.79 1.152 0.00 1179.15 0.00
WD4128 131.670 145.690 14.02 0.763 0.00 762.25 0.00
WD4130 142.650 145.690 3.04 0.278 0.00 178.29 0.00
WD4132 146.730 153.620 6.89 0.937 0.00 574.46 0.00
WD4132 169.650 174.190 4.54 0.792 0.00 589.27 0.00
WD4135 101.500 103.580 2.08 0.293 0.00 348.00 0.00
WD4140 177.090 179.530 2.44 0.000 0.00 0.00 0.00
WD4140 198.880 200.990 2.11 0.000 0.00 0.00 0.00
WD4141 124.360 132.340 7.98 0.870 0.00 469.27 0.00
WD4144 161.240 167.120 5.88 1.019 0.00 2919.05 0.00
WD4145 204.220 208.480 4.26 0.832 0.00 501.92 0.00
WD4149 59.440 64.770 5.33 1.850 0.00 2306.90 0.00
WD4460 7.620 47.240 39.62 0.880 0.00 183.97 0.00
WD4460 56.390 62.480 6.09 0.398 0.00 110.03 0.00
WD4473 18.290 25.910 7.62 0.723 0.00 316.46 0.00
WD4474 15.240 45.720 30.48 0.638 0.00 205.66 0.00
WD4738 18.290 19.810 1.52 0.390 0.00 80.00 0.00
WD4739 15.240 22.860 7.62 0.669 0.00 80.00 0.00
WD4740 15.240 22.860 7.62 0.333 0.00 73.33 0.00
WD4750 18.290 33.530 15.24 0.611 0.00 173.64 0.00
WD4794 18.290 22.860 4.57 0.890 0.00 185.00 0.00
WD4798 18.290 19.810 1.52 1.110 0.00 20.00 0.00
WD4978 39.620 48.770 9.15 0.948 0.00 1114.07 0.00
WD4986 9.140 33.530 24.39 0.106 0.00 136.87 0.00
WD5119 32.000 38.100 6.10 0.646 0.00 637.18 0.00
WD5164 6.100 28.960 22.86 0.119 0.00 202.11 0.00
WD5302 45.720 54.860 9.14 0.928 0.00 1704.86 0.00
For
per
sona
l use
onl
y
Hole_ID From To Width Ni_pct As_ppm Cu_ppm Co_ppm
WD5304 149.410 150.420 1.01 1.241 0.00 3339.11 0.00
WD5304 178.610 197.390 18.78 0.933 0.00 480.12 0.00
WD5310 209.850 212.600 2.75 0.256 0.00 214.98 0.00
WD5312 275.840 287.180 11.34 1.108 0.00 642.44 0.00
WD5313 217.320 226.160 8.84 1.252 0.00 1482.87 0.00
WD5315 77.720 81.780 4.06 1.095 0.00 527.07 0.00
WD5318 272.310 274.930 2.62 0.670 0.00 826.34 0.00
WD5321 302.060 304.140 2.08 0.425 0.00 245.00 0.00
WD5323 62.790 75.900 13.11 1.009 0.00 1289.26 0.00
WD5325 233.170 241.400 8.23 1.931 0.00 1877.21 0.00
WD5329 77.720 85.340 7.62 1.379 0.00 736.54 0.00
WD5330 257.860 274.320 16.46 0.000 0.00 0.00 0.00
WD5337 375.510 377.040 1.53 1.580 0.00 2520.00 0.00
WD5338 149.570 149.990 0.42 0.045 0.00 190.00 0.00
WD5341 335.130 339.000 3.87 0.121 0.00 732.61 0.00
WD5342 358.750 363.630 4.88 0.591 0.00 383.73 0.00
WD5343 161.850 169.770 7.92 2.560 0.00 1861.48 0.00
WD5343 174.040 184.100 10.06 1.475 0.00 1201.11 0.00
WD5344 345.950 351.740 5.79 1.044 0.00 1055.92 0.00
WD5466 12.190 21.340 9.15 0.763 0.00 116.61 0.00
WD5467 10.670 25.910 15.24 0.716 0.00 89.99 0.00
WD5493 27.430 32.000 4.57 0.341 0.00 243.22 0.00
WD5494 44.200 46.330 2.13 0.554 0.00 515.82 0.00
WD5496 1.520 7.620 6.10 0.950 0.00 1732.34 0.00
WD5803 321.870 324.700 2.83 1.692 0.00 674.42 0.00
WD5804 180.290 185.470 5.18 0.061 0.00 149.66 0.00
WD5804 220.830 231.650 10.82 0.903 0.00 667.26 0.00
WD5810 275.540 278.590 3.05 0.000 0.00 0.00 0.00
WD5813 69.190 76.810 7.62 0.712 0.00 423.99 0.00
WD5813 98.760 102.410 3.65 1.072 0.00 742.60 0.00
WD5818 176.170 197.510 21.34 0.000 0.00 0.00 0.00
WD5819 287.580 292.520 4.94 2.738 0.00 2233.60 0.00
WD5820 57.910 60.350 2.44 0.401 0.00 363.11 0.00
WD5821 249.630 252.680 3.05 0.362 0.00 269.31 0.00
WD5822 67.670 71.320 3.65 0.000 0.00 0.00 0.00
WD5824 307.420 311.350 3.93 0.766 0.00 508.42 0.00
WD5826 86.870 89.920 3.05 1.711 0.00 1074.62 0.00
WD5830 464.450 465.340 0.89 2.350 0.00 2520.00 0.00
WD5832 143.840 148.740 4.90 0.848 0.00 616.04 0.00
WD6052 1.520 7.620 6.10 0.581 0.00 1519.90 0.00
WD6053 3.050 6.100 3.05 0.530 0.00 3920.66 0.00
WD6054 1.520 7.620 6.10 1.063 0.00 2122.36 0.00
WD6055 1.520 7.620 6.10 0.546 0.00 1145.64 0.00
WD6262 4.570 35.050 30.48 0.766 0.00 1326.74 0.00
For
per
sona
l use
onl
y
Hole_ID From To Width Ni_pct As_ppm Cu_ppm Co_ppm
WD6262 57.910 83.820 25.91 0.857 0.00 756.75 0.00
WD6513 22.860 28.960 6.10 0.928 0.00 677.54 0.00
WD6519 32.000 45.720 13.72 0.650 0.00 914.46 0.00
WD6522 4.570 10.670 6.10 0.775 0.00 1101.85 0.00
WD6522 53.340 57.910 4.57 0.860 0.00 533.04 0.00
WD6523 3.050 6.100 3.05 0.250 0.00 90.00 0.00
WD6524 1.520 7.620 6.10 0.440 0.00 922.25 0.00
WD8016 33.530 39.620 6.09 0.800 0.00 1445.22 0.00
WD8017 3.050 33.530 30.48 1.134 0.00 1851.75 0.00
WD8020 10.670 24.380 13.71 0.913 0.00 1149.38 0.00
WD8130 380.090 382.220 2.13 3.269 0.00 2643.38 0.00
WD8133 147.070 149.050 1.98 0.100 0.00 685.45 0.00
WD8137W1 367.890 377.190 9.30 2.531 0.00 2097.17 0.00
WD8138 82.450 90.530 8.08 0.922 0.00 559.90 0.00
WD8142 151.760 154.720 2.96 0.000 0.00 0.00 0.00
WD8142 175.870 178.670 2.80 0.000 0.00 0.00 0.00
WD8143 145.390 150.420 5.03 0.804 0.00 1047.24 0.00
WD8143 183.400 194.160 10.76 0.625 0.00 538.09 0.00
WD8148 112.620 114.910 2.29 1.148 0.00 644.80 0.00
WD8149 208.760 212.050 3.29 3.557 0.00 5646.29 0.00
WD8150 157.120 159.930 2.81 0.300 0.00 131.10 0.00
WD8152 283.830 285.900 2.07 0.182 0.00 210.10 0.00
WD8156 174.650 179.830 5.18 0.863 0.00 481.58 0.00
WD8159 367.590 370.330 2.74 1.463 0.00 1174.01 0.00
WD8159 380.240 382.710 2.47 1.300 0.00 1251.74 0.00
WD8160 473.350 481.430 8.08 0.738 0.00 554.05 0.00
WD8162 250.240 274.260 24.02 0.759 0.00 539.08 0.00
WD8163 125.580 128.020 2.44 0.949 0.00 1352.17 0.00
WD8163 163.220 165.200 1.98 0.153 0.00 107.78 0.00
WD8164 380.090 382.520 2.43 0.878 0.00 600.41 0.00
WD8165 506.940 509.320 2.38 1.123 0.00 665.29 0.00
WD8166 332.230 335.040 2.81 1.508 0.00 1091.74 0.00
WD8167 109.060 115.490 6.43 1.266 0.00 1190.33 0.00
WD8167 121.430 126.800 5.37 1.969 0.00 2248.31 0.00
WD8167 149.660 156.970 7.31 0.962 0.00 1005.91 0.00
WD8168 231.650 238.810 7.16 0.983 0.00 684.43 0.00
WD8172 353.930 366.520 12.59 0.857 0.00 610.27 0.00
WD8174 312.690 314.860 2.17 0.915 0.00 653.73 0.00
WD8175 124.970 131.310 6.34 0.867 0.00 1061.58 0.00
WD8175 140.210 142.950 2.74 0.928 0.00 814.60 0.00
WD8176 115.920 118.480 2.56 0.966 0.00 1105.66 0.00
WD8176 128.990 130.760 1.77 0.345 0.00 561.02 0.00
WD8177 260.600 265.330 4.73 1.053 0.00 748.31 0.00
WD8178 199.340 211.840 12.50 1.331 0.00 2080.45 0.00
For
per
sona
l use
onl
y
Hole_ID From To Width Ni_pct As_ppm Cu_ppm Co_ppm
WD8178 220.280 226.280 6.00 1.498 0.00 1869.68 0.00
WD8179 124.360 127.040 2.68 0.855 0.00 265.04 0.00
WD8179 203.420 205.740 2.32 1.888 0.00 3857.20 0.00
WD8180 353.260 355.270 2.01 0.179 0.00 175.12 0.00
WD8181 135.580 140.510 4.93 0.731 0.00 580.43 0.00
WD8182 275.940 278.680 2.74 0.571 0.00 472.52 0.00
WD8183 469.540 471.740 2.20 0.792 0.00 549.45 0.00
WD8183 476.920 479.540 2.62 0.434 0.00 349.12 0.00
WD8186 199.890 201.350 1.46 0.480 0.00 560.00 0.00
WD8189 87.480 89.640 2.16 0.370 0.00 342.13 0.00
WD8192 202.080 210.620 8.54 1.082 0.00 1379.39 0.00
WD8199 308.760 322.330 13.57 1.323 0.00 1509.28 0.00
WD8199 346.310 348.570 2.26 0.655 0.00 1180.58 0.00
WD9697 16.460 32.920 16.46 0.732 0.00 630.02 0.00
WD10709 343.200 347.930 4.73 1.144 0.00 1480.95 0.00
WD10709 356.310 359.970 3.66 0.609 0.00 733.28 0.00
WD10714 289.010 294.130 5.12 0.683 0.00 1359.84 0.00
WD10728 296.880 304.190 7.31 0.923 0.00 803.34 0.00
WD10728 308.310 309.680 1.37 0.213 0.00 130.00 0.00
WD10731 201.170 204.220 3.05 0.372 0.00 704.79 0.00
WDC019 68.000 70.000 2.00 0.824 1385.00 1119.00 359.50
WDC020 71.000 78.000 7.00 1.529 9.14 1748.57 460.00
WDC020 83.000 88.000 5.00 1.986 12.40 1988.80 539.20
WDC020 95.000 99.000 4.00 0.528 16.25 395.00 166.00
WDC022 183.000 190.000 7.00 0.733 5.43 759.86 278.71
WDC022 196.000 199.000 3.00 0.274 41.00 293.67 135.33
WDC022 220.000 222.000 2.00 0.433 28.50 440.00 167.00
WDC024 112.000 115.000 3.00 0.000 0.00 0.00 0.00
WDC026 180.000 186.000 6.00 0.599 19.17 662.17 235.33
WDC026 202.000 204.000 2.00 0.908 2530.00 865.00 257.00
WDC027 175.000 181.000 6.00 0.956 6.00 1141.33 325.17
WDC028 178.000 183.000 5.00 2.424 138.40 2918.60 666.00
WDC033 86.000 91.000 5.00 1.090 456.60 272.40 398.80
WDC035 160.000 161.000 1.00 0.273 ‐5.00 484.00 176.00
WDC036 8.000 28.000 20.00 0.726 262.75 1740.33 377.50
WDC037 53.000 68.000 15.00 0.796 0.47 1007.20 292.93
WDC038 4.000 8.000 4.00 0.014 14.75 127.75 47.00
WDC039 139.000 145.000 6.00 1.354 4.50 1770.33 444.33
WDC039 149.000 156.000 7.00 1.396 10.29 1658.00 425.14
WDC039 163.000 167.000 4.00 0.552 123.25 685.00 202.00
WDC041 92.000 95.000 3.00 0.926 16.00 1237.00 361.67
WDC043 52.000 56.000 4.00 0.530 380.00 431.00 226.00
WDC047 80.000 82.000 2.00 0.000 0.00 0.00 0.00
WDC049 109.000 112.000 3.00 0.976 7.67 1101.33 331.67
For
per
sona
l use
onl
y
Hole_ID From To Width Ni_pct As_ppm Cu_ppm Co_ppm
WDC050 99.000 103.000 4.00 1.103 141.00 1560.00 382.25
WDC051 63.000 66.000 3.00 1.462 171.00 1857.67 566.33
WDC052 120.000 122.000 2.00 0.940 0.50 1459.00 312.50
WDC053 164.000 173.000 9.00 2.248 990.22 3452.11 678.89
WDC088 155.000 159.000 4.00 1.017 3422.00 862.25 292.25
WDC089 178.000 184.000 6.00 2.000 227.83 2959.83 594.67
WDC090 164.000 167.000 3.00 4.637 8423.33 6016.67 1602.33
WDC091 172.000 175.000 3.00 0.468 191.00 487.33 187.33
WDC095 194.000 199.000 5.00 1.077 14.60 1324.60 377.60
WDC095 204.000 206.000 2.00 1.658 3876.50 778.00 684.50
WDC096 149.000 155.000 6.00 1.113 7.00 1077.33 374.00
WDC096 168.000 170.000 2.00 0.797 711.00 786.50 219.00
WDC101 137.000 140.000 3.00 0.289 328.87 329.73 138.33
WDC102 178.000 180.000 2.00 0.401 337.50 348.50 154.00
WDC104 105.000 107.000 2.00 2.375 723.50 5825.25 377.50
WDC106 127.000 131.000 4.00 3.967 3306.25 4000.50 1346.25
WDC119 58.000 66.000 8.00 1.042 140.00 1054.63 266.63
WDC120 80.000 87.000 7.00 2.365 560.00 2848.57 746.00
WDC121 38.000 45.000 7.00 1.066 132.71 1701.43 208.00
WDC122 85.000 87.000 2.00 1.466 1540.00 765.50 652.00
WDC123 99.000 102.000 3.00 0.445 59.00 283.00 192.00
WDC124 111.000 113.000 2.00 1.240 17.50 1980.00 382.00
WDC125 51.000 59.000 8.00 0.688 301.63 856.00 365.38
WDC126 103.000 104.000 1.00 1.610 46.00 4820.00 478.00
WDC127 148.000 150.000 2.00 1.283 21.50 9190.00 446.00
WDC128 164.000 168.000 4.00 0.011 ‐5.00 94.00 46.00
WDC130 36.000 56.000 20.00 0.624 37.10 291.95 319.40
WDC132 36.000 62.000 26.00 0.833 291.77 222.46 603.77
WDC144 200.000 206.000 6.00 1.334 18.00 1566.17 414.83
WDC144 211.000 212.000 1.00 0.686 17.00 630.00 234.00
WDC182 128.000 131.000 3.00 0.044 29.33 130.33 57.33
WDC183 118.000 120.000 2.00 1.487 119.50 2187.50 397.50
WDC186 152.000 154.000 2.00 0.833 0.50 1223.00 290.00
WDC189 120.000 121.000 1.00 0.184 24.00 458.00 132.00
WDD016 147.650 150.100 2.45 0.219 402.86 218.35 104.18
WDD020 253.000 266.000 13.00 1.117 12.54 1667.23 393.77
WDD020 272.000 280.000 8.00 1.372 254.75 1619.13 458.50
WDD020 318.000 321.000 3.00 0.830 22.67 1246.67 307.33
WDD021 185.000 188.000 3.00 0.548 7.00 488.00 193.33
WDD022 262.000 269.000 7.00 0.926 6.86 1170.14 341.71
WDD029 229.000 232.000 3.00 0.478 2776.33 416.00 229.67
WDD030 147.000 148.000 1.00 1.366 619.00 816.80 520.20
WDD033 123.000 125.100 2.10 2.118 2090.62 2615.38 662.86
WDD035 134.000 136.000 2.00 0.341 8.50 357.50 151.50
For
per
sona
l use
onl
y
Hole_ID From To Width Ni_pct As_ppm Cu_ppm Co_ppm
WDD036 90.600 93.000 2.40 4.726 1933.00 5015.96 1278.00
WDD037 147.900 151.000 3.10 0.384 942.13 525.48 192.77
WDD039 195.000 197.400 2.40 0.816 8.33 1211.08 327.75
WDD040 145.000 146.000 1.00 0.431 ‐5.00 920.00 201.00
WDD041 201.000 202.700 1.70 1.891 230.65 2162.06 556.50
WDD042 207.100 210.200 3.10 5.558 47.35 5577.58 1489.55
WDD043 128.550 131.000 2.45 0.243 150.35 561.43 146.14
WDD044 149.000 152.000 3.00 2.203 26.29 3420.06 633.79
WDD045 188.250 189.000 0.75 0.061 15.00 231.00 67.00
WDD046 112.000 119.000 7.00 0.959 275.42 492.41 387.14
WDD051 182.000 189.300 7.30 1.477 21.23 1516.07 468.16
WDD055 170.000 176.000 6.00 1.225 15.83 1345.30 429.20
WDD055 189.000 190.000 1.00 0.800 3120.00 839.00 276.00
WDD056 163.000 170.000 7.00 0.834 10.83 920.34 329.63
WDD057 190.000 194.000 4.00 1.892 823.08 2167.53 507.83
WDD060 247.500 248.800 1.30 0.069 132.77 169.08 55.00
WDD061 294.000 297.250 3.25 7.053 33.60 7040.71 1929.95
WDD062 313.700 315.100 1.40 0.745 91.71 1016.43 254.57
WDD072 272.000 273.500 1.50 0.557 117.13 261.07 215.93
WDD073 328.000 329.000 1.00 0.950 329.00 1214.00 256.50
WID1328 164.500 164.700 0.20 3.230 100.00 590.00 540.00
WID1337 90.000 92.000 2.00 0.365 0.00 990.00 140.00
WID1339 94.000 98.000 4.00 1.200 755.00 2275.00 265.00
WID1340 66.000 72.000 6.00 1.187 416.67 5053.33 596.67
WID1341 94.000 104.000 10.00 1.843 524.00 1614.00 570.00
WID1342 74.000 80.000 6.00 0.949 96.67 1720.00 403.33
WID1343 36.000 40.000 4.00 1.135 110.00 1750.00 185.00
WID1344 84.000 88.000 4.00 0.600 0.00 125.00 175.00
WID1346 56.000 58.000 2.00 0.385 0.00 430.00 140.00
WID1347 106.000 112.000 6.00 0.697 0.00 1230.00 443.33
WID1348 62.000 68.000 6.00 0.642 0.00 1296.67 276.67
WID1349 16.000 34.000 18.00 0.909 0.00 660.00 577.78
WID1374 60.000 68.000 8.00 0.425 0.00 2427.50 113.75
WID1375 28.000 38.000 10.00 1.044 129.00 1484.00 172.00
WID1376 10.000 30.000 20.00 0.865 138.00 709.50 632.00
WID1376 44.000 48.000 4.00 0.583 0.00 149.50 72.25
WID1380 70.000 72.000 2.00 3.050 0.00 2250.00 800.00
WID1402 216.000 219.000 3.00 1.754 230.00 1867.33 503.00
WID1403 151.000 152.000 1.00 0.063 0.00 50.00 70.00
WID1479 449.700 451.500 1.80 1.227 1427.78 1068.89 283.33
WID1479 494.700 499.100 4.40 1.368 12.27 1747.95 462.05
WID1480 426.000 429.000 3.00 0.665 741.67 393.33 178.33
WID1481 394.000 396.400 2.40 1.435 943.33 939.17 227.50
WID1482 354.000 359.000 5.00 1.477 474.60 1075.40 340.40
For
per
sona
l use
onl
y
Hole_ID From To Width Ni_pct As_ppm Cu_ppm Co_ppm
WID1544 84.000 86.000 2.00 0.850 600.00 1010.00 300.00
WID1545 72.000 73.000 1.00 0.296 100.00 470.00 130.00
WID1546 46.000 51.000 5.00 1.080 100.00 1328.00 314.00
WID1546 63.000 65.000 2.00 0.188 100.00 180.00 120.00
WID1547 20.000 22.000 2.00 0.545 150.00 465.00 225.00
WID1547 37.000 45.000 8.00 0.993 387.50 1485.00 322.50
WID1548 33.000 35.000 2.00 0.679 150.00 295.00 175.00
WID1550 46.000 56.000 10.00 0.725 120.00 1278.00 262.00
WID1551 46.000 62.000 16.00 0.944 0.00 1188.75 298.75
WID1552 36.000 50.000 14.00 0.960 0.00 1208.57 312.86
WID1553 14.000 18.000 4.00 0.530 0.00 570.00 300.00
WID1553 36.000 46.000 10.00 0.603 0.00 702.00 236.00
WID1554 24.000 30.000 6.00 0.990 0.00 1236.67 450.00
WID1568 202.000 203.500 1.50 0.317 100.00 363.33 170.00
WID1569 162.000 171.000 9.00 0.771 417.22 1200.83 334.83
WID1570 133.050 134.100 1.05 0.512 1676.19 940.48 309.05
WID1724 299.000 299.650 0.65 1.320 10600.00 110.00 230.00
WID1783 200.000 203.000 3.00 2.063 175.00 3439.00 649.83
WID1784 178.650 180.000 1.35 0.844 100.00 886.67 286.30
WID1805 190.400 193.750 3.35 2.483 110.45 2466.87 581.94
WID1806 196.600 198.350 1.75 0.253 100.00 1099.71 129.14
WID1807 215.500 216.300 0.80 0.737 100.00 395.63 261.25
WID1818 231.850 233.850 2.00 1.151 13.75 3390.50 400.50
WID1819 188.700 190.150 1.45 2.756 17.59 4430.69 754.14
WID1820A 131.800 134.600 2.80 0.664 732.14 501.50 213.79
WID1822 136.950 137.950 1.00 0.281 150.00 230.00 140.00
WID1848 88.000 90.000 2.00 1.070 0.00 1080.00 340.00
WID1867 86.000 88.000 2.00 1.610 0.00 1690.00 440.00
WID1869 126.000 128.000 2.00 0.383 0.00 540.00 160.00
WID1898 263.800 266.000 2.20 0.882 100.00 1068.64 302.95
WID1899 257.400 259.800 2.40 3.864 100.00 6160.79 999.50
WID1900 229.950 232.700 2.75 2.864 5592.73 4998.73 579.45
WID1902 249.500 251.000 1.50 0.454 100.00 588.67 185.33
For
per
sona
l use
onl
y
Appendix 5 – JORC Code (2012 Edition) Table 1
132N deposit: Section 1 Sampling Techniques and Data
Criteria JORC Code explanation Commentary
Sampling techniques
Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.
Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.
Aspects of the determination of mineralisation that are material to the Public Report.
In cases where ‘industry standard’ work has been done this would be relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information.
132N has been drilled by percussion, diamond drilling and RC drilling. Accurate drilling data exists for 317 drill holes for 31669.57 metres in the area. This does not include blast holes from mining. The pre‐mining database contained 83 drill holes with 233 intercepts of 1% Ni or greater with widths of at least 1 metre. In the remnant resource a total of 31 holes had one or more composite intercepts over 1% Ni. There was a total of 191 composite intercepts greater than 1% Ni with a width of 0.90 metre or greater.
The holes have been drilled on irregular spacing as tight as 15m by 20m in the central zone of the mineralisation and up to 50m by 30m towards the extremities and down plunge.
Diamond holes were selectively sampled through the visible mineralised zone on a nominal 1m sample length, adjusted to geological and domain boundaries. Sample lengths vary from 0.05m to 4.2m.
Diamond core samples have been sampled by a combination of quarter core and half core cut samples and a combination of BQ, NQ and HQ diameter.
RC drill holes were sampled by 1m riffle split composites. RC drilling was 5 ¼ inch in diameter.
Sample representivity for diamond core was ensured by the sampling of an average length of 1m of core, which was then cut to quarter or half, depending on the company operating at the time, for laboratory analysis.
RC sampling was riffle split from 1m composite bulk samples, producing a nominal 3kg – 5kg representative sample.
Sample lengths for diamond drilling range from 0.05 to 4.2 m and average approximately 1.0m. RC samples sample were all 1m in length.
Mineralised intervals are determined by visual inspection and logging prior to any sampling. Laboratory assays are then compared to the visual estimates and logging to determine if any adjustments are required.
Mineralisation is identified pyrrhotite and pentlandite with minor chalcopyrite hosted in talc‐ carbonate ultramafics.
For Titan and Consmin drilling, representative samples from RC and diamond drilling were collected and sent to accredited laboratories for analysis. Accredited laboratories in Kalgoorlie and Perth crushed and pulverised the samples in entirety, and took a 50g pulp for analysis. This process cannot be established for drilling completed before 2005.
For Titan and Consmin samples, analysis was performed by 4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques. Gold and PGEs were determined by a fire assay fusion followed by aqua regia digest and atomic absorption spectrometer (AAS) finish. Analysis techniques were not established for samples taken before 2005, but the results generally correlate well with newer data. Minor copper, cobalt and arsenic occur in the mineralisation.
Drilling techniques Drill type (e.g. core, reverse circulation, open‐ hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (e.g. core diameter, triple or standard tube, depth of diamond tails, face‐ sampling bit or other type, whether core is oriented and if so, by what method, etc.).
The data used in the remnant Mineral Resource is comprised of diamond drilling samples.
(162) and RC drilling samples (32).
Diamond drilling included NQ, HQ and BQ diameter core.
For
per
sona
l use
onl
y
Drill sample recovery
Method of recording and assessing core and chip sample recoveries and results assessed.
Measures taken to maximise sample recovery and ensure representative nature of the samples.
Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.
Core recoveries were recorded for all resource database diamond core collected by Titan and Consmin. Handwritten geotechnical logging sheets were kept of all drilling activities. Core recoveries are recorded in the database. Diamond core recoveries averaged 96% where core recoveries were recorded.
RC samples recoveries or weights were not recorded.
No relationship could be established between sample recovery and reported grade.
Logging Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.
Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc.) photography.
The total length and percentage of the relevant intersections logged
Detailed drill hole logs (all drilling), geotechnical and structural logs (core only) are available for the drilling.
Separate sample logging sheets were kept including samples numbers for duplicates, standards and blanks taken for QA/QC purposes.
The logging is of a detailed nature, and of sufficient detail to support the current Mineral Resource estimate categories.
The total length of drill intersections used in the remnant Mineral Resource estimate is 180.05m and 100% of those intersections are logged.
Sub‐sampling techniques and sample preparation
If core, whether cut or sawn and whether quarter, half or all core taken.
If non‐core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry.
For all sample types, the nature, quality and appropriateness of the sample preparation technique.
Quality control procedures adopted for all sub‐ sampling stages to maximise representivity of samples.
Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second‐half sampling.
Whether sample sizes are appropriate to the grain size of the material being sampled.
The core was halved or quartered, depending on which company and phase of work, by sawing before sampling
RC drilling was riffle split directly from the sample collection cyclone on the drilling rig.
Sample condition field to record moisture and sample recovery is included in the sampling log sheet and populates the assay table of the database. Unfortunately only a very small percentage of the logs have captured this information so no determination can be made about the quality of the RC samples.
Sample preparation is considered to be appropriate for RC and diamond drilling as per industry standard practices for managing RC samples and diamond core.
Quality control procedures included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis. 4892 QAQC samples have been analysed over the life of this project. No bias or major analytical errors have been found.
Host rock is a talc‐chlorite‐carbonate ultramafic with thin lenses of disseminated and massive Ni sulphides. Samples of diamond core and RC samples produce appropriate size samples to be representative for the style of mineralisation and rock type encountered.
Quality of assay data and laboratory tests
For geophysical tools, spectrometers, handheld XRF instruments, etc., the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.
Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.
Quality control procedures included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis.
One standard, blank and field duplicate were inserted into the sample stream every 20 samples. These were offset through the sampling stream and placed in areas of interest i.e. high grade standards and blanks in the ore zone where possible.
Overall, standards used reported values within 2 standard deviations of the expected values with a few exceptions. These were usually found to be sample miss labelling in the field and were largely able to be rectified in the database.
No geophysical methods or hand‐held XRF units have been used for determination of grades in the Mineral Resource estimate.
For
per
sona
l use
onl
y
Verification of sampling and assaying
The verification of significant intersections by either independent or alternative company personnel.
The use of twinned holes.
Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.
Discuss any adjustment to assay data
Intersections reported have been checked back to original logs and assay data.
4 twinned drill holes were completed. (Cervoj, 2007). These were designed to test the historical high grades. The four holes, WDD153, WDD161, WDD147 and WDC303 confirmed grades from earlier drill holes WID1962, WID1281A, WID1561, WID1280, WID1959, WDC289, WID1317, WID1317A, WID1566, WID1564 and WID1565.
Drill hole data were sourced from digital sources and original hard‐ copy sampling and assay records, and imported into a central electronic database. Datashed software was used to validate and manage the data.
Assays were composited to 1m lengths and where necessary top cuts applied for resource estimation.
Location of data points
Accuracy and quality of surveys used to locate drill holes (collar and down‐hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.
Specification of the grid system used. Quality and adequacy of topographic control.
Surface topography is derived from a detailed topographic survey completed by Spectrum Surveys in 2006.
Collar co‐ordinates were picked up by Spectrum Surveys during the 2006 topographic survey.
A majority of the drill holes were downhole surveyed with gyroscopic survey tool. The remaining holes were surveyed by single shot tool and by collar measurement with a clinometer and compass. Significant magnetic interference is present at 132N, reducing the reliability of single shot surveys.
Original surveying was undertaken in MGA94 zone 51.
Topographic control is considered more than adequate for the current Mineral Resource estimate as it was completed by a licenced surveyor using a RTDGPS.
Data spacing and distribution
Data spacing for reporting of Exploration Results. The resource area has been drilled on an irregular pattern and spacing by several different companies over an extended period. The average spacing is estimated to be approximately 40m by 20m within the remnant Mineral Resource.
Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.
Whether sample compositing has been applied
The drill data spacing and sampling is adequate to establish the geological and grade continuity required for the current Mineral Resource estimate.
Diamond drill hole samples were composited to 1.0 m down‐hole intervals for resource modelling. RC Samples used in the estimate were composited to 1m intervals already.
Orientation of data in relation to geological structure
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.
The drill line and drill hole orientation is oriented as close as practicable to perpendicular to the orientation of the general mineralised orientation.
A majority of the drilling intersects the mineralisation at close to 90 degrees ensuring intersections are representative of true widths. Several historic holes are drilled at a low angle to the mineralisation, the reasons for which are unclear.
Sample security The measures taken to ensure sample security. Reports and original log files indicate at a thorough process of logging, recording, sample storage and dispatch to labs was followed at the time of drilling.
Sample security measures adopted include the daily movement of core samples in trays to the Kalgoorlie Office, where core was kept in a secure area before cutting and sampling.
RC split samples were transported from site daily and delivered to the accredited laboratory depot in Kalgoorlie for preparation and analysis.
Audits or reviews The results of any audits or reviews of sampling techniques and data.
Sample data reviews have included an inspection and investigation of all available paper and digital geological logs to ensure correct entry into the drill hole database.
Visualisation of drilling data in three dimensional software (Micromine and Surpac) and QA/QC sampling review using Maxwell Geoservices QAQCR Software was undertaken. Although these reviews are not definitive, they provide confidence in the general reliability of the data. F
or p
erso
nal u
se o
nly
132N deposit: Section 2 Reporting of Exploration Results
Criteria JORC Code explanation Commentary
Mineral tenement and land tenure status
Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.
The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.
Apollo Phoenix Resources Pty Ltd (Apollo) holds a 100% interest the nickel and base metal rights to the project. Neometals has entered a binding agreement to acquire the tenure, subject to the satisfaction of conditions precedent.
There are no known impediments to operate in the area.
Exploration done by other parties
Acknowledgment and appraisal of exploration by other parties.
Exploration has been undertaken by previous holders, but predominantly Western Mining Corporation (WMC) during the 1980s and Titan Resources Limited from 2001. Consolidated Minerals Ltd took over Titan Resources Limited in 2006. Further exploration was completed and 132N was mined by open pit methods by Australian Nickel Mines NL (Consolidated Minerals Ltd).
Geology Deposit type, geological setting and style of mineralisation. The geology at 132N consists of a thin steeply west dipping raft of ultramafic within a much greater volume of basalt. The ultramafic strikes at between 340° ‐ 345° and appears to pinch out at depth. The ultramafic has been interpreted by past workers (Hellman & Schofield, 2005) to form a synformal structure underlain by basalt. This interpretation has been questioned by Cervoj (2007) who states that detailed mapping and field inspections have identified pillow basalts on either side of the supposed fold axis, which face to the west indicating that the major structural feature is a fault (either wrench or thrust).
There is evidence in the geological and geophysical data for both strike parallel and cross cutting structures. The cross cutting structures are the most important in terms of the mineralisation and appear to have a sinistral sense of movement. The mineralisation at 132N consists of structurally modified or emplaced thin anastomosing lenses of disseminated and massive Ni sulphides hosted by talc‐chlorite‐carbonate ultramafic. Overall the Ni mineralisation strikes about 340° ‐ 345° and dips approximately 65° to the west. Individual lenses however do mimic the basalt ultramafic boundary and are found on both the eastern and western contacts. Nickel mineralisation within the overall zone can vary in dip from 25°E to 70°W. The overall plunge of the mineralisation is ‐30° to the north but can vary from being flat to 50°.
Although the overall mineralised envelope has a strike of over 600 metres individual lenses at a 1% Ni cut off tend to have short strike lengths and rarely exceed 50 metres. Down dip extents vary from 10 metres to up to 100 metres but more typically they are only 25 – 30 metres.
Depth of complete oxidation varies from 10 to 80 metres below the natural surface but is typically around 40 metres
Drill hole Information
A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: easting and northing of the drill hole collar elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar dip and azimuth of the hole down hole length and interception depth hole length. If the exclusion of this information is justified on
See Drilling Information, appendix 3.
No information is excluded.
For
per
sona
l use
onl
y
the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.
Data aggregation methods
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. cutting of high grades) and cut‐off grades are usually Material and should be stated.
Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.
The assumptions used for any reporting of metal equivalent values should be clearly stated.
Drill hole summary results are included in this release. The results reported include all intersections included in the estimation of the resource.
A nominal cut‐off of 1.0% Ni was used to define the drill intersections composites. A 2m maximum internal dilution was used.
Appendix 4 above contains all weighted composites included in the remnant Mineral Resource estimate. Higher grade intersections within the composites are included in the table.
No metal equivalents are used in this Mineral Resource estimate.
Relationship between mineralisation widths and intercept lengths
These relationships are particularly important in the reporting of Exploration Results.
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.
If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g. ‘down hole length, true width not known’).
The drill line and drill hole orientation is oriented as close to 90 degrees to the orientation of the anticipated mineralised orientation as practicable.
The majority of the drilling intersects the mineralisation at close to 90 degrees. The following holes were drilled at a low angle to the mineralisation and therefore intercept widths are wider than true widths; WD3323, WD3330, WD4971, WDD102.
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.
Appropriate maps and tables are included in the body of the announcement.
Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.
All drill intercepts used in the estimation of the resource envelope irrespective of grade are reported in Appendix 4 above. The resource envelope is constructed using a nominal 1.0% Ni cut‐off and a maximum drilled internal dilution of 2m.
All drill hole collars are reported in Appendix 3 above.
Other substantive exploration data
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and
method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.
Mineral Resources were estimated from drill hole assay data, with geological logging used to aid interpretation of mineralised contact positions.
Geological observations are included in the report. All core drilled at 132N is available for review and is stored at the Fisher mine offices in Kambalda.
Metallurgical test work is out of the scope of this report.
Multi‐element assay suites have been analysed and arsenic has been identified as a potentially deleterious element.
Bulk density measurements have been taken and analysed. SGs were assigned to the block model using the formula (Ni% x For
per
sona
l use
onl
y
0.0725) + 2.8023.
A bulk density of 2.5 was assigned to completely weathered waste blocks; 2.7 to moderately weathered waste blocks; 2.9 to fresh waste.
Further work The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large‐scale step‐out drilling).
Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.
No further work is planned at this stage.
There is potential for possible extensions in the down plunge position to the current Mineral Resource, but the grades are considered far too low to be economic at those depths.
Drill spacing is currently considered adequate to undertake limited high level economic evaluations on the project. Infill drilling would be required if more detailed feasibility studies were to be undertaken.
132N deposit: Section 3 Estimation and Reporting of Mineral Resources
Criteria JORC Code explanation Commentary
Database integrity Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes.
Data validation procedures used.
The drill hole database was sourced from original hard‐copy sampling and assay records.
Validation measures included spot checking between database and hard copy drill logs and sections and plans in historic reports.
The database is an extract from an Industry Standard SQL Server database using a normalised assay data model produced by Datashed Software.
Site visits Comment on any site visits undertaken by the Competent Person and the outcome of those visits.
If no site visits have been undertaken indicate why this is the case.
Mr. Marshall visited 132N numerous times between 2005 and 2007 and was intimately involved in the planning and implementation of drilling programs completed during that time. Mr Marshall was also directly involved in the historic data compilation and validation for the project.
Geological interpretation
Confidence in (or conversely, the uncertainty of) the geological interpretation of the mineral deposit.
Nature of the data used and of any assumptions made.
The effect, if any, of alternative interpretations on Mineral Resource estimation.
The use of geology in guiding and controlling Mineral Resource estimation.
The factors affecting continuity both of grade and geology.
132N was discovered in the 1969 by International Nickel Australia Limited (INAL). INAL entered into a joint venture with BHP in 1969 and explored the area from 1969 to 1979. WMC acquired the ground in 1981, continuing with exploration and conducted open pit mining activities during 1990. As a result an extensive body of knowledge exists for the project and therefore confidence in interpretations is relatively high.
Historical data as well as recent data collected by Titan and Consmin were used in the interpretations. The data from different companies and time periods correlated very well.
For this Mineral Resource estimate a 1% Ni cut‐off was used, with the interpretation based on structural and stratigraphic controls. The only valid departure from this interpretation would be to apply a different grade cut‐off.
Wireframe boundaries were “snapped” to drilling intercepts using the sample positions, with the use of geological logging being used as a guide when considering the interpretation of the mineralised wireframe. Interpretations were prepared on 20m section spacing’s cut at bearing 90 degrees on the MGA94 zone 51 grid.
The drill spacing is relatively wide and introduces sufficient uncertainty for the short range variability and continuity in the deposit. The mineralisation is hosted in a high strain environment which can adversely affect the continuity of the mineralisation and mine reconciliations back to the resource model. F
or p
erso
nal u
se o
nly
Given the current wide drill spacing, pinching, swelling and truncation of the mineralisation is possible between the drill holes, as observed in many of the nickel mining operations in the area.
The boundaries of the broader mineralised zone are consistent, but within these zones, higher/ lower grade and thicker/ thinner zones occur. It is expected that additional drilling will define the distribution and nature of this variability.
Dimensions The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource.
The Mineral Resources extend over a strike length of approximately 600 m. The resource models extend to 340 m depth below surface.
The open pit Mineral Resource is mined.
Estimation and modelling techniques
The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used.
The availability of check estimates, previous estimates and/or mine production records and whether the Mineral Resource estimate takes appropriate account of such data.
The assumptions made regarding recovery of by‐products.
Estimation of deleterious elements or other non‐grade variables of economic significance (e.g. sulphur for acid mine drainage characterisation).
In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed.
Any assumptions behind modelling of selective mining units.
Any assumptions about correlation between variables.
Description of how the geological interpretation was used to control the resource estimates.
Discussion of basis for using or not using grade cutting or capping.
The process of validation, the checking process used, the comparison of model data to drill hole data, and use of reconciliation data if available.
Grades were estimated predominantly by Inverse Distance Squared estimation of 1.0m down‐hole composited Nickel, arsenic, cobalt and copper assay grades from diamond and RC holes within mineralised domain wireframes.
Surpac software was used for data compilation, domain wire‐framing, and coding of composite values , statistics, geostatistics and resource estimation.
Previous Mineral Resource estimates have been made by several companies from 1969 onwards. The resources vary considerably depending on the domaining of the Ni grades and depletion by mining;
2000 WMC 282,000 tonnes @ 3.5% Ni
2002 WMC 116,000 tonnes @ 2.1% Ni
2005 Titan Resources 396,000 tonnes @ 1.5% Ni
2005 BM Geological services 136,000 tonnes @ 4.35% Ni
2007 CNPL 282,000 tonnes @ 2.2% Ni
2008 CNPL 200,000 tonnes @ 3.1% Ni
1990s WMC Production 32,174tonnes @ 3.53% Ni
2007 – 2008 CNPL Production 29,485 tonnes @ 2.9% Ni
No consideration has been made for the recovery of by‐products. Arsenic is a significant deleterious element.
No consideration has been made with regard to sulphur levels in the waste material but the assays are available. This is due to the preliminary nature of economic evaluation to date.
Resources were estimated into 5m by 1.25m x 2.5m parent blocks (strike, vertical, cross strike) aligned N‐S on MGA94 zone 51.
For precise volume representation, sub‐blocking was allowed to 2.5m x0.3125m x 0.625m.
The modelling included used an anisotropic search ellipsoid with minimum data requirements of 3 data points and a minimum of two holes in the centre of the deposit. Down plunge depth extremities of the wireframe model required a minimum of one point and one drill hole, although these blocks were not included in this Mineral Resource.
The estimates are not intended to reflect a fixed mining method but could be amenable to several mining techniques.
Details of potential mining parameters have been considered but reflect the early stage of the project evaluation.
Correlations exist in the assay data between Ni and the other elements. The following regressions were used where attributes did not fill after 3 expanding passes: F
or p
erso
nal u
se o
nly
The geology and grade information was used in the creation of the mineralised domain wireframes. A nominal 1.0% Ni cut‐off was used to define the outline within geological units. The selection of this cut‐ off is an economic boundary and matches the mining process used in the past.
No grade cutting or capping has been used. Grades are relatively uniform within a defined range, with no order of magnitude outlying high grades that would materially affect the resource.
Model validation included visual comparison of model estimates and composite grades using section analysis with the raw drilling data and the composite data.
There is no detailed production information to reconcile against the model. CNPL produced 82,153 tonnes @ 1.65% Ni from 2007 to 2008 but this was from the Armstrong and 132N open pits. There was no way to differentiate production in the data supplied.
Moisture Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content.
Tonnages are estimated on a dry tonnage basis.
Cut‐off parameters The basis of the adopted cut‐off grade(s) or quality parameters applied.
The cut off grades reflect Neometals’ perception of the potential range of operating costs and prices of nickel.
The mineralised envelope is modelled using a 1.0% Ni cut‐off grade
Mining factors or assumptions
Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be
Neometals has considered the possibility of both open cut and underground mining on the project. The maximum depth of the open pit is 80 ‐ 90 metres below the natural land surface. Further open pit mining would involve high waste to ore ratios.
Given the nature of the geometry of the mineralisation underground mining of the remnant Mineral Resource would appear to be appropriate. No feasibility studies have yet been completed.
Dependant on the cost parameters used and the nickel price, Mineral Resource, or part thereof, is potentially amenable to underground mining.
For
per
sona
l use
onl
y
reported with an explanation of the basis of the mining assumptions made.
Metallurgical factors or assumptions
The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made.
There were no metallurgical test work results available for this report, however all ore delivered to the NickelWest Concentrator met specifications under the offtake agreement in place at the time.
Recoveries for Widgiemooltha Ni ore from the NickelWest Smelter during 2008 varied from 72% to 87% with an overall average Ni recovery of 80%.
Environmental factors or assumptions
Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfields project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made.
Mine waste is stored locally in waste dumps while process waste is stored in tailings dams by NickelWest.
High talc and carbonate content and low sulphide content the waste rock suggest that ARD should not be a problem.
Bulk density Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples.
The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc.), moisture and differences between rock and alteration zones within the deposit.
Discuss assumptions for bulk density estimates used in the evaluation process of the different materials.
192 samples were determined by weight in air weight in water technique. Cervoj (2007) completed statistics and a regression between nickel and specific gravity measurements. That work was also used as the basis for specific gravity measurements in the current block model. A regression line was determined for fresh mineralised samples of (Ni * 0.0725) + 2.8023 =SG.
SGs of 2.5 for completely weathered, 2.7 for moderately weathered, and 2.9 for fresh were assigned to waste blocks.
Classification The basis for the classification of the Mineral Resources into varying confidence categories.
Whether appropriate account has been taken of all relevant factors (i.e. relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the
Resource classification was assigned on the basis of geological continuity and confidence, the number of drill hole intersections, and average distance to samples.
The resource classification accounts for all relevant factors in the opinion of the Competent Person.
Classification of the estimates reflects the Competent Person’s views of the deposit.
For
per
sona
l use
onl
y
data).
Whether the result appropriately reflects the Competent Person’s view of the deposit.
Audits or reviews The results of any audits or reviews of Mineral Resource estimates.
A detailed audit was completed on the Mineral Resource estimate to prepare this JORC 2012 statement.
Discussion of relative accuracy/ confidence
Where appropriate a statement of the relative accuracy and confidence level in the Mineral Resource estimate using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the resource within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate.
The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used.
These statements of relative accuracy and confidence of the estimate should be compared with production data, where available
Confidence in the relative accuracy of the estimates is reflected by the classifications assigned in the block model.
The geostatistical procedures used to estimate, quantify and qualify the block model were completed to a high standard.
No blocks have been assigned a Measured Mineral Resource category which reflects the relative confidence, or lack thereof, in the accuracy of the interpretations.
Significant doubts about the validity of the wireframe interpretations exist as the Mineral Resource is located in a structurally complex and highly strained environment. This has been demonstrated by mining of the 132N open pit.
There is a high level of confidence in the spatial accuracy of the datasets used in the Mineral Resource estimate as the survey control is very good.
No detailed production data are available for reconciliation as the historical data could not be located.
For
per
sona
l use
onl
y
Armstrong deposit: Section 1 Sampling Techniques and Data
Criteria JORC Code explanation Commentary
Sampling techniques
Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.
Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.
Aspects of the determination of mineralisation that are material to the Public Report.
In cases where ‘industry standard’ work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (eg submarine nodules) may warrant disclosure of detailed information
The Armstrong Mineral Resource has been drilled by percussion, diamond drilling and RC drilling. Accurate drilling data exists for 789 drill holes for 57,700.83 metres. A total of 69 holes had one or more intercepts over 1% Ni.
The holes have been drilled on irregular spacing as tight as 20m by 20m in the central high grade part of the mineralisation and up to 100m by 50m towards the extremities and low grade areas.
Diamond holes were selectively sampled through the visible mineralised zone on a nominal 1m sample length, adjusted to geological and domain boundaries. Sample lengths vary from 0.05m to about 1.2m.
Diamond core samples have been sampled by a combination of quarter core and half core cut samples and a combination of BQ, NQ and HQ diameter.
RC drill holes were sampled by 1m riffle split composites. RC drilling was 5 ¼ inch in diameter.
Sample representivity for diamond core was ensured by the sampling of an average length of 1m of core, which was then cut to quarter or half, depending on the company operating at the time, for laboratory analysis. RC sampling was riffle split from 1m composite bulk samples, producing a nominal 3kg – 5kg representative sample.
Sample lengths for diamond drilling range from 0.2 to 1.2 m and average approximately 1.0m. RC samples sample were all 1m in length.
Mineralised intervals are determined by visual inspection and logging prior to any sampling. Laboratory assays are then compared to the visual estimates and logging to determine if any adjustments are required.
Mineralisation is identified pyrrhotite and pentlandite with minor chalcopyrite hosted in talc‐ carbonate ultramafics.
For Titan and Consmin drilling, representative samples from RC and diamond drilling were collected and sent to accredited laboratories for analysis. Accredited laboratories in Kalgoorlie and Perth crushed and pulverised the samples in entirety, and took a 50g pulp for analysis. This process cannot be established for drilling completed before 2005.
For Titan and Consmin samples, analysis was performed by 4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques. Gold and PGEs were determined by a fire assay fusion followed by aqua regia digest and atomic absorption spectrometer (AAS) finish. Analysis techniques were not established for samples taken before 2005, but the results generally correlate well with newer data.
Minor copper, cobalt and arsenic occur in the mineralisation.
Drilling techniques Drill type (eg core, reverse circulation, open‐hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (eg core diameter, triple or standard tube, depth of diamond tails, face‐ sampling bit or other type, whether core is oriented and if so, by what method, etc.).
The database used in the area of the Mineral Resource is comprised of diamond drilling samples (12219), RC drilling samples (3943), Percussion (1317), RAB (847), Aircore (693).
Only diamond and RC holes were used in the estimation of the resource. Diamond drilling included NQ, HQ and BQ diameter core.
Drill sample recovery
Method of recording and assessing core and chip sample recoveries and results assessed.
Measures taken to maximise sample recovery and ensure representative nature of the samples.
Whether a relationship exists between sample recovery and
Core recoveries were recorded for all resource database diamond core collected by Titan and Consmin. Handwritten geotechnical logging sheets were kept of all drilling activities. Core recoveries are recorded in the database.
RC samples recoveries or weights were not recorded.
No relationship could be established between sample recovery and reported grade. RC samples report a lower average grade than core samples overall which is related their being drilled as RC pre‐collars intersecting lower grades portions outside of F
or p
erso
nal u
se o
nly
grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.
main body of the mineralisation, and diamond drilling focusing on higher grade portions of the orebody.
Logging Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.
Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc.) photography.
The total length and percentage of the relevant intersections logged.
Detailed drill hole logs (all drilling), geotechnical and structural logs (core only) are available for the drilling.
Separate sample logging sheets were kept including samples numbers for duplicates, standards and blanks taken for QA/QC purposes.
The logging is of a detailed nature, and of sufficient detail to support the current Mineral Resource estimate categories.
The total length of drill intersections used in the Mineral Resource estimate is 444.88m and 100% of those intersections are logged.
Sub‐sampling techniques and sample preparation
If core, whether cut or sawn and whether quarter, half or all core taken.
If non‐core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry.
For all sample types, the nature, quality and appropriateness of the sample preparation technique.
Quality control procedures adopted for all sub‐ sampling stages to maximise representivity of samples.
Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second‐half sampling.
Whether sample sizes are appropriate to the grain size of the material being sampled.
The core was halved or quartered, depending on which company and phase of work, by sawing before sampling RC drilling was riffle split directly from the sample collection cyclone on the drilling rig.
Sample condition field to record moisture and sample recovery is included in the sampling log sheet and populates the assay table of the database. Unfortunately only a very small percentage of the logs have captured this information so no determination can be made about the quality of the RC samples.
Sample preparation is considered to be appropriate for RC and diamond drilling as per industry standard practices for managing RC samples and diamond core.
Quality control procedures included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis. 857 QAQC samples are included in the dataset used for this Mineral Resource estimate.
Host rock is mainly a talc‐carbonate ultramafic with minor interflow sediments (black shales). Samples of diamond core and RC samples produce appropriate size samples to be representative for the style of mineralisation and rock type encountered.
Quality of assay data and laboratory tests
For geophysical tools, spectrometers, handheld XRF instruments, etc., the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.
Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) and precision have been established.
Quality control procedures included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis.
One standard, blank and field duplicate were inserted into the sample stream every 20 samples. These were offset through the sampling stream and placed in areas of interest i.e. high grade standards and blanks in the ore zone where possible.
Overall, standards used reported values within 2 standard deviations of the expected values with a few exceptions. These were usually found to be sample miss labelling in the field and were largely able to be rectified in the database.
No geophysical methods or hand‐held XRF units have been used for determination of grades in the Mineral Resource estimate.
Verification of sampling and assaying
The verification of significant intersections by either independent or alternative company personnel.
The use of twinned holes.
Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.
Discuss any adjustment to assay data.
Intersections reported have been checked back to original logs and assay data.
No twin holes have been drilled.
Drill hole data were sourced from digital sources and original hard‐copy sampling and assay records, and imported into a central electronic database. Datashed software was used to validate and manage the data.
Assays were composited to 1m lengths and where necessary top cuts applied for resource estimation. For
per
sona
l use
onl
y
Location of data points
Accuracy and quality of surveys used to locate drill holes (collar and down‐hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.
Specification of the grid system used.
Quality and adequacy of topographic control.
The Armstrong open pit and waste dumps were surveyed on a regular basis by Spectrum Surveys for Titan Resources and Consolidated Minerals during mining by RTDGPS.
Collar co‐ordinates were picked up by Spectrum Surveys.
A majority of the drillholes were downhole surveyed with gyroscopic survey tool. The remaining holes were surveyed by single shot tool and by collar measurement with a clinometer and compass.
Original surveying was undertaken in GDA94 grid.
Topographic control is considered more than adequate for the current Mineral Resource estimate as it was completed by a licenced surveyor using a RTDGPS.
Data spacing and distribution
Data spacing for reporting of Exploration Results.
Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.
Whether sample compositing has been applied.
The resource area has been drilled on an irregular pattern and spacing by several different companies over an extended period. The average spacing is estimated to be approximately 20m by 20m within the Mineral Resource.
The drill data spacing and sampling is adequate to establish the geological and grade continuity required for the current Mineral Resource estimate.
Diamond drill hole samples were composited to 1.0 m down‐hole intervals for resource modelling. RC Samples used in the estimate were composited to 1m intervals already.
Orientation of data in relation to geological structure
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.
If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.
The drill line and drill hole orientation is oriented as close as practicable to perpendicular to the orientation of the general mineralised orientation.
A majority of the drilling intersects the mineralisation at close to 90 degrees ensuring intersections are representative of true widths.
Sample security The measures taken to ensure sample security. Sample security measures adopted include the daily movement of core samples in trays to the Kalgoorlie Office, where core was kept in a secure area before cutting and sampling.
RC split samples were transported from site daily and delivered to the accredited laboratory depot in Kalgoorlie for preparation and analysis.
Reports and original log files indicate at a thorough process of logging, recording, sample storage and dispatch to labs was followed at the time of drilling.
Audits or reviews The results of any audits or reviews of sampling techniques and data.
Sample data reviews have included an inspection and investigation of all available paper and digital geological logs to ensure correct entry into the drill hole database.
Visualisation of drilling data in three dimensional software (Micromine and Surpac) and QA/QC sampling review using Maxwell Geoservices QAQCR Software was undertaken. Although these reviews are not definitive, they provide confidence in the general reliability of the data.
For
per
sona
l use
onl
y
Armstrong deposit: Section 2 Reporting of Exploration Results
Criteria JORC Code explanation Commentary
Mineral tenement and land tenure status
Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.
The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.
Apollo holds a 100% interest the nickel and base metal rights to the project. Neometals has entered a binding agreement to acquire the tenure, subject to the satisfaction of considtions precedent.
There are no known impediments to operate in the area.
Exploration done by other parties
Acknowledgment and appraisal of exploration by other parties.
Exploration has been undertaken by previous holders, but predominantly Western Mining Corporation (WMC) during the 1980s.
Programs of diamond drilling were undertaken by WMC as well as resource estimates, metallurgical test work and economic evaluations.
Geology Deposit type, geological setting and style of mineralisation. Nickel mineralisation is hosted by serpentine‐talc‐chlorite‐carbonate altered ultramafics and typically has a pyrrhotite + pentlandite + pyrite +/‐ chalcopyrite assemblage. There is a combination of disseminated and massive sulphides in thin, discontinuous, steeply dipping lenses within a larger body of diffusely mineralised serpentinite. The Armstrong deposit strikes between 320 – 330 degrees, has a strike length of approximately 450 metres and is truncated at depth by a granitic intrusive. The mineralisation has an average width of 3 metres, dips at about ‐45 degrees west and plunges to the northwest at approximately ‐25 degrees.
A number of arsenic rich shear zones cut obliquely through the mineralisation. These structures strike around 345 degrees and dip at approximately 50 degrees to the west.
The stratigraphy at a deposit scale consists of the Archaean Mt Edwards basalt overlain by the Widgiemooltha Komatiite. The ultramafic succession consists of a series of flows with intercalated sediments. It is approximately 250m thick and displays carbonate alteration and serpentinisation. The mineral assemblages are talc‐ antigorite‐chlorite‐magnetite and talc‐magnesite‐amphibolite‐ magnetite. Stronger carbonate –chlorite alteration is noted around the
mineralised lenses.
Depth of complete oxidation is up to 50 metres, with a further ~10‐ 25m of supergene zone below the base of oxidation.
Drill hole Information
A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:
easting and northing of the drill hole collar
elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar dip and azimuth of the hole down hole length and interception depth hole length.
If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not
See Appendix 3 above for drilling information.
No information is excluded.
For
per
sona
l use
onl
y
detract from the understanding of the report, the Competent Person should clearly explain why this is the case.
Data aggregation methods
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut‐off grades are usually Material and should be stated.
Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.
The assumptions used for any reporting of metal equivalent values should be clearly stated.
Drill hole summary results are included in this release. The results reported include all intersections included in the estimation of the resource.
A nominal cut off of 1.0% Ni was used to define the drill intersections composites. A 2m maximum internal dilution was used. Appendix 4 in the report contains all weighted composites included in the Mineral Resource estimate. Higher grade intersections within the composites are included in the table.
No metal equivalents are used in this Mineral Resource estimate.
Relationship between mineralisation widths and intercept lengths
These relationships are particularly important in the reporting of Exploration Results.
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.
If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg ‘down hole length, true width not known’).
The drill line and drill hole orientation is oriented as close to 90 degrees to the orientation of the anticipated mineralised orientation as practicable.
The majority of the drilling intersects the mineralisation at close to 90 degrees.
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.
Appropriate maps and tables are included in the body of the Announcement.
Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.
All drill intercepts used in the estimation of the resource envelope irrespective of grade are reported in Appendix 43. The resource envelope is constructed using a nominal 1.0% Ni cut‐off and a maximum drilled internal dilution of 2m. All drill hole collars are reported in Appendix 4 above.
Other substantive exploration data
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.
Mineral Resources were estimated from drill hole assay data, with geological logging used to aid interpretation of mineralised contact positions.
Geological observations are included in the report. All core drilled at Armstrong is available for review and is stored at the Fisher mine offices in Kambalda.
Multi‐element assay suites have been analysed and arsenic has been identified as a potentially deleterious element.
Bulk density measurements have been taken and analysed. SGs were assigned to the block model using the formula (Ni% x 0.0533) + 2.7878.
Waste bulk density was assigned on the basis of weathering. Completely weathered waste was assigned 2.5. Moderately For
per
sona
l use
onl
y
weathered waste was assigned 2.7. Fresh rock waste was assigned 2.9.
Further work The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large‐scale step‐out drilling).
Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.
No further work is planned at this stage.
There is potential for possible extensions in the down plunge position to the current Mineral Resource, but the grades are considered far too low to be economic at those depths. Granite is also interpreted at depth that may truncate the mineralisation.
Drill spacing is currently considered adequate to undertake limited high level economic evaluations on the project.
Armstrong deposit: Section 3 Estimation and Reporting of Mineral Resources
Criteria JORC Code explanation Commentary
Database integrity Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes.
Data validation procedures used.
The drill hole database was sourced from original hard‐copy sampling and assay records.
Validation measures included spot checking between database and hard copy drill logs and sections and plans in historic reports.
The database is an extract from an Industry Standard SQL Server database using a normalised assay data model produced by Datashed Software.
Site visits Comment on any site visits undertaken by the Competent Person and the outcome of those visits.
If no site visits have been undertaken indicate why this is the case.
Mr. Marshall visited Armstrong numerous times between 2005 and 2007 and was intimately involved in the planning and implementation of drilling programs completed during that time. Mr Marshall was also directly involved in the historic data compilation and validation for the project.
Geological interpretation
Confidence in (or conversely, the uncertainty of) the geological interpretation of the mineral deposit.
Nature of the data used and of any assumptions made.
The effect, if any, of alternative interpretations on Mineral Resource estimation.
The use of geology in guiding and controlling Mineral Resource estimation.
The factors affecting continuity both of grade and geology.
The Armstrong deposit (formerly named Moore) was discovered in the 1980’s and evaluated by WMC Resources. Titan Resources acquired the deposit in 2004. Mining commenced in 2005. As a result of extensive exploration and mining there is a high degree of confidence in the geology.
Historical data as well as recent data collected by Titan and Consmin were used in the interpretations. The data from different companies and time periods correlated very well.
For this Mineral Resource estimate a 1% Ni cut‐off was used, with the interpretation based on structural and stratigraphic controls. The only valid departure from this interpretation would be to apply a different grade cut‐off.
Wireframe boundaries were “snapped” to drilling intercepts using the sample positions, with the use of geological logging being used as a guide when considering the interpretation of the mineralised wireframe. Interpretations were prepared on 20m section spacings cut at bearing 90 degrees on MGA94 zone 51.
Given the drill spacing, pinching, swelling and truncation of the mineralisation is possible between the drillholes, as observed in many of the other nickel mining operations in the area.
The boundaries of the broader mineralised zone are consistent, but within these zones, higher/ lower grade and thicker/ thinner zones occur.
For
per
sona
l use
onl
y
Dimensions The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource.
The Mineral Resources extend over a strike length of approximately 400 m. The resource models extend to 250 m depth below surface.
The near surface Mineral Resource is mined
Estimation and modelling techniques
The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used.
The availability of check estimates, previous estimates and/or mine production records and whether the Mineral Resource estimate takes appropriate account of such data.
The assumptions made regarding recovery of by‐products.
Estimation of deleterious elements or other non‐grade variables of economic significance (eg sulphur for acid mine drainage characterisation).
In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed.
Any assumptions behind modelling of selective mining units.
Any assumptions about correlation between variables.
Description of how the geological interpretation was used to control the resource estimates.
Discussion of basis for using or not using grade cutting or capping.
The process of validation, the checking process used, the comparison of model data to drill hole data, and use of reconciliation data if available.
Grades were estimated predominantly by Inverse Distance Squared estimation of 1.0m down‐hole composited nickel assay grades from diamond and RC holes within mineralised domain wireframes.
Surpac software was used for data compilation, domain wire‐framing, and coding of composite values, statistics, geostatistics and resource estimation.
Previous Mineral Resource estimates have been made by several companies from 1987 onwards. The more recent estimates compare well with the current one as follows;
301Kt @ 3.1% Ni in Feb 2004 by Golder Associates
102Kt @ 2.0% Ni (primary) and 55.9Kt @ 1.17% Ni (oxide) in sept 2004 Hellman & Schofield
104.6Kt @ 1.72% Ni (primary) in Nov 2004 Hellman & Schofield
54.9Kt @ 1.7% Ni (transitional) and 6.7Kt @ 2.09% Ni (supergene) in Jul 2006 by Consolidated Minerals
440.1Kt @ 2.19% Ni (transitional/fresh) and 5.0Kt @ 1.86% Ni(supergene) in Nov 2006 by Consolidated Minerals
363.6Kt @ 2.56% Ni (fresh) and 20.4Kt @ 1.53% Ni (transitional) in April 2008 by Consolidated Minerals.
Armstrong Open Pit Reconciliation figures from July 2007 ‐ February 2008
Armstrong Open Reconciliation figures from March ‐ May 2008
No consideration has been made for the recovery of by‐products.
Arsenic is a significant deleterious element.
Fe:MgO ratio. Under the Central Widgie off‐take agreement WMC quote their minimum acceptable limit as 0.8. A typical batch For
per
sona
l use
onl
y
of Armstrong ore has a Fe:MgO ratio of 0.4. As Fe:MgO was a key factor in the 2004 closure it is vital to understand the variability within the deposit.
No consideration has been made with regard to sulphur levels in the waste material but the assays are available. This is due to the preliminary nature of economic evaluation to date.
Resources were estimated into 5m by 2.5m x 2.5m parent blocks (strike, vertical, cross strike) aligned N‐S on MGA94 zone 51.
For precise volume representation, sub‐blocking was allowed to 1.25m x0.625m x 0.625m.
The modelling included used an anisotropic search ellipsoid with minimum data requirements of 3 data points and a minimum of two holes in the centre of the deposit. At the east and west and depth.
extremities of the wireframe model a minimum of one point and one drillhole, although these blocks were not included in this Mineral Resource estimate.
The estimates are not intended to reflect a fixed mining method but could be amenable to several mining techniques. Details of potential mining parameters have been considered but reflect the early stage of the project evaluation.
A number of correlations between the elements and attributes of the modelled mineralisation exist at the Armstrong deposit. Where mineralised domains were not filled after 3 expanding passes the following regressions were used;
The geology and grade information was used in the creation of the mineralised domain wireframes. A nominal 1.0% Ni cut‐off was used to define the outline within geological units. The selection of this cut‐ off is an economic boundary as it matched mining practices from 2007 ‐ 2008.
No grade cutting or capping has been used. Grades are relatively uniform within a defined range, with no order of magnitude outlying high grades that would materially affect the resource.
Model validation included visual comparison of model estimates and composite grades using section analysis with the raw drilling data and the composite data.
Reconciliation data is shown above. The modelling was improving against the tonnes and grades mined in 2008 and was overcalling tonnes by 4% and Ni grade by 8% and As grade by 7%. To gain greater confidence in the remnant resource a resource model incorporating all mined mineralisation should be completed. This should be reconciled against all previous production.
For
per
sona
l use
onl
y
Moisture Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content.
Tonnages are estimated on a dry tonnage basis.
Cut‐off parameters The basis of the adopted cut‐off grade(s) or quality parameters applied.
The cut off grades reflect Neometals’ perception of the potential range of operating costs and prices of nickel.
The mineralised envelope is modelled using a 1.0% Ni cut‐off grade
Mining factors or assumptions
Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the mining assumptions made.
Neometals has considered the possibility of both open cut and underground mining on the project. Only open pit designs currently exist for the project but it would be expected that the remnant resource would be exploited via underground methods.
Dependant on the cost parameters used and the nickel price, Mineral Resource, or part thereof, is potentially amenable to open cut or underground mining.
Metallurgical factors or assumptions
The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous.
Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made.
There were no metallurgical test work results available for this report however the ore delivered by Consolidated Minerals to the NickelWest concentrator met specifications under the offtake agreement in place during the time of open pit mining. The high arsenic levels need to be controlled with greater understanding on the controls of its distribution.
Fe:MgO ratio. Under the Central Widgie off‐take agreement WMC quote their minimum acceptable limit as 0.8. A typical batch of Armstrong ore has a Fe:MgO ratio of 0.4.
Recoveries for Widgiemooltha Ni ore from the NickelWest Smelter during 2008 varied from 72% to 87% with an overall average Ni recovery of 80%.
Environmental factors or assumptions
Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfields project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made.
Mine waste is currently held in an above ground waste dump. It would be expected that this practice was continued when mining recommences.
High talc and carbonate content and low sulphide content the waste rock suggest that ARD should not be a problem.
For
per
sona
l use
onl
y
Bulk density Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples.
The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc.), moisture and differences between rock and alteration zones within the deposit.
Discuss assumptions for bulk density estimates used in the evaluation process of the different materials.
62 samples were determined by weight in air weight in water technique. Thompson (2008) completed statistics and a regression between nickel and specific gravity measurements. That work was also used as the basis for specific gravity measurements in the current block model. A regression line was determined for fresh mineralised samples of (Ni * 0.0533) + 2.7878 =SG.
SGs of 2.5 for completely weathered, 2.7 for moderately weathered, and 2.9 for fresh were assigned to waste blocks.
Classification The basis for the classification of the Mineral Resources into varying confidence categories.
Whether appropriate account has been taken of all relevant factors (ie relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the data).
Whether the result appropriately reflects the Competent Person’s view of the deposit.
Resource classification was assigned on the basis of geological continuity and confidence, the number of drill hole intersections, and average distance to samples.
The resource classification accounts for all relevant factors in the opinion of the Competent Person.
Classification of the estimates reflects the Competent Person’s views of the deposit
Audits or reviews The results of any audits or reviews of Mineral Resource estimates.
A detailed audit was completed on the Mineral Resource estimate to prepare this JORC 2012 statement.
Discussion of relative accuracy/ confidence
Where appropriate a statement of the relative accuracy and confidence level in the Mineral Resource estimate using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the resource within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate.
The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used.
These statements of relative accuracy and confidence of the estimate should be compared with production data, where available.
Confidence in the relative accuracy of the estimates is reflected by the classifications assigned in the block model.
The geostatistical procedures used to estimate, quantify and qualify the block model were completed to a high standard. There is a high level of confidence in the spatial accuracy of the datasets used in the Mineral Resource estimate as the survey control is very good.
Significant production data is available for the Armstrong deposit that would feed back in an economic evaluation of the deposit.
For
per
sona
l use
onl
y
Cooke deposit: Section 1 Sampling Techniques and Data
Criteria JORC Code explanation Commentary
Sampling techniques
Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.
Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.
Aspects of the determination of mineralisation that are material to the Public Report.
In cases where ‘industry standard’ work has been done this would be relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information.
The Cooke are has been drilled by Aircore, percussion, diamond drilling and RC drilling. Accurate drilling data exists for 147 drill holes for 18,888.48 metres. A total of 58 holes had one or more intercepts over 1% Ni.
The holes have been drilled on irregular spacing as tight as 30m by 15m in the central high grade part of the mineralisation.
Diamond holes were selectively sampled through the visible mineralised zone on a nominal 1.5m sample length for historic drilling, and 1m for Titan Resources drilling, adjusted to geological and domain boundaries. Sample lengths vary from 0.2m to 5.3m.
Diamond core samples have been sampled by a combination of quarter core and half core cut samples and a combination of BQ, NQ and HQ diameter.
For Titan Resources drilling RC drill holes were sampled by 1m riffle split composites. RC drilling was 5 ¼ inch in diameter. Samples were composited over 4 metre intervals in waste and 1 metre in mineralisation. For historic drilling RC sampling techniques were not confirmed.
Sample representivity for diamond core was ensured by the sampling of an average length of 1m or 1.5m of core, which was then cut to quarter or half, depending on the company operating at the time, for laboratory analysis.
RC sampling was riffle split from 1m composite bulk samples, producing a nominal 3kg – 5kg representative sample for Titan drilling.
Sample lengths for diamond drilling range from 0.05 to 5.3 m and average approximately 1.5 m from historical drilling. Titan drilling was sampled on a nominal 1m length, adjusted to geological domains.
Mineralised intervals were determined by visual inspection and logging prior to any sampling. Laboratory assays are then compared to the visual estimates and logging to determine if any adjustments were required.
Mineralisation is identified pyrrhotite, pentlandite, violarite and pyrite with minor chalcopyrite hosted in talc‐carbonate ultramafics.
For Titan, representative samples from RC and diamond drilling were collected and sent to accredited laboratories for analysis. Accredited laboratories in Kalgoorlie and Perth crushed and pulverised the samples in entirety, and took a 50g pulp for analysis. This process cannot be established for drilling completed before the acquisition by Titan in 2001.
For Titan samples, analysis was performed by 4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques. Gold and PGEs were determined by a fire assay fusion followed by aqua regia digest and atomic absorption spectrometer (AAS) finish. Analysis techniques were not established for samples taken before 2001, but the results generally correlate well with newer data.
Minor copper, cobalt and arsenic occur in the mineralisation.
International Nickel Australia Limited (INAL) and WMC Resources sampling and assay techniques are unknown. These companies completed the majority of the exploration and drilling work in the 1960’s and 1990’s respectively.
For
per
sona
l use
onl
y
Drilling techniques Drill type (e.g. core, reverse circulation, open‐ hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (e.g. core diameter, triple or standard tube, depth of diamond tails, face‐ sampling bit or other type, whether core is oriented and if so, by what method, etc.).
The database used in the Mineral Resource is comprised of diamond drilling samples (11253), RC drilling samples (4768), Percussion (904), Auger (64). Most of the unspecified samples are actually historic diamond drilling drilled predominantly by Western Mining during the early 1990s. Diamond drilling included NQ, HQ and BQ diameter core.
Drill sample recovery
Method of recording and assessing core and chip sample recoveries and results assessed.
Measures taken to maximise sample recovery and ensure representative nature of the samples.
Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.
Core recoveries were recorded for all resource database diamond core collected by Titan. Handwritten geotechnical logging sheets were kept of all drilling activities. Core recoveries are recorded in the database, however no information on the Cooke deposit could be located.
RC samples recoveries or weights were not recorded.
No relationship could be established between sample recovery and reported grade. RC samples report a lower average grade than core samples overall which is related their being drilled as RC pre‐collars intersecting lower grades portions outside of main body of the mineralisation, and diamond drilling focusing on higher grade portions of the orebody.
Logging Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.
Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc.) photography.
The total length and percentage of the relevant intersections logged.
Detailed drill hole logs (all drilling), geotechnical and structural logs (core only) are available for the drilling completed by Titan Resources Limited.
Separate sample logging sheets were kept including samples numbers for duplicates, standards and blanks taken for QA/QC purposes.
The logging is of a detailed nature, and of sufficient detail to support the current Mineral Resource estimate categories.
The total length of drill intersections used in the Mineral Resource estimate is 14,104.50m and 100% of those intersections are logged.
Sub‐sampling techniques and sample preparation
If core, whether cut or sawn and whether quarter, half or all core taken.
If non‐core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry.
For all sample types, the nature, quality and appropriateness of the sample preparation technique.
Quality control procedures adopted for all sub‐ sampling stages to maximise representivity of samples.
Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second‐half sampling.
Whether sample sizes are appropriate to the grain size of the material being sampled.
The core was halved or quartered, depending on which company and phase of work, by sawing before sampling. For Titan Resources, RC drilling was riffle split directly from the sample collection cyclone on the drilling rig.
For Titan Resources, Sample condition field to record moisture and sample recovery is included in the sampling log sheet and populates the assay table of the database. Unfortunately, only a very small percentage of the logs have captured this information so no determination can be made about the quality of the RC samples.
Sample preparation is considered to be appropriate for RC and diamond drilling as per industry standard practices for managing RC samples and diamond core.
For Titan Resources, quality control procedures included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis. 32 QAQC samples are included in the dataset used for this Mineral Resource estimate.
Host rock is mainly a talc‐carbonate ultramafic with minor interflow sediments (black shales). Samples of diamond core and RC samples produce appropriate size samples to be representative for the style of mineralisation and rock type encountered.
International Nickel Australia Limited (INAL) and WMC Resources sampling and assay techniques are unknown. These companies completed the majority of the exploration and drilling work in the 1960’s and 1990’s respectively.
Quality of assay data and laboratory tests
For geophysical tools, spectrometers, handheld XRF instruments, etc., the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.
For Titan Resources, quality control procedures included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis.
For Titan Resources, one standard, blank and field duplicate were inserted into the sample stream every 20 samples. These were offset through the sampling stream and placed in areas of interest i.e. high grade standards and blanks in the ore zone F
or p
erso
nal u
se o
nly
Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.
where possible.
For Titan Resources, overall, standards used reported values within 2 standard deviations of the expected values with a few exceptions. These were usually found to be sample miss labelling in the field and were largely able to be rectified in the database.
It is unknown whether INAL or WMC used QAQC procedures.
No geophysical methods or hand‐held XRF units have been used for determination of grades in the Mineral Resource estimate.
Verification of sampling and assaying
The verification of significant intersections by either independent or alternative company personnel.
The use of twinned holes.
Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.
Discuss any adjustment to assay data.
Intersections reported have been checked back to original logs and assay data.
No twin holes have been drilled.
Drill hole data were sourced from digital sources and original hard‐ copy sampling and assay records, and imported into a central electronic database. Datashed software was used to validate and manage the data.
Assays were composited to 1.5m lengths for resource estimation.
Location of data points
Accuracy and quality of surveys used to locate drill holes (collar and down‐hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.
Specification of the grid system used. Quality and adequacy of topographic control.
Surface topography appears to be derived from the surface position of drill holes.
Collar co‐ordinates were picked up by Spectrum Surveys in 2006.
A majority of the drill holes were downhole surveyed with gyroscopic survey tool. The remaining holes were surveyed by single shot tool and by collar measurement with a clinometer and compass.
Original surveying was undertaken in MGA94.
Topographic control is considered adequate for the current Mineral Resource estimate as it was completed by a licenced surveyor using a RTDGPS.
Data spacing and distribution
Data spacing for reporting of Exploration Results.
Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.
Whether sample compositing has been applied.
The resource area has been drilled on a regular pattern and spacing by different companies over an extended period. The average spacing is estimated to be approximately 30m by 15m within the Mineral Resource.
The drill data spacing and sampling is adequate to establish the geological and grade continuity required for the current Mineral Resource estimate.
Diamond drill hole samples were composited to 1.5 m down‐hole intervals for resource modelling.
Orientation of data in relation to geological structure
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.
If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.
The drill line and drill hole orientation is oriented as close as practicable to perpendicular to the orientation of the general mineralised orientation.
A majority of the drilling intersects the mineralisation at close to 60 ‐ 90 degrees ensuring intersections are representative of true widths.
Sample security The measures taken to ensure sample security. Reports and original log files indicate at a thorough process of logging, recording, sample storage and dispatch to labs was followed at the time of drilling.
For Titan Resources, sample security measures adopted include the daily movement of core samples in trays to the Kalgoorlie Office, where core was kept in a secure area before cutting and sampling.
For Titan Resources, RC split samples were transported from site.
daily and delivered to the accredited laboratory depot in Kalgoorlie for preparation and analysis.
For Titan Resources, Reports and original log files indicate at a thorough process of logging, recording, sample storage and For
per
sona
l use
onl
y
dispatch to labs was followed at the time of drilling.
The measures taken by INAL and WMC are unknown.
Audits or reviews The results of any audits or reviews of sampling techniques and data.
Sample data reviews have included an inspection and investigation of all available paper and digital geological logs to ensure correct entry into the drill hole database.
Visualisation of drilling data in three dimensional software (Micromine) and QA/QC sampling review using Maxwell Geoservices QAQCR Software was undertaken. Although these reviews are not definitive, they provide confidence in the general reliability of the data.
Cooke deposit: Section 2 Reporting of Exploration Results
Criteria JORC Code explanation Commentary
Mineral tenement and land tenure status
Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.
The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.
Apollo holds a 100% interest in the nickel and base metal rights to the project under M15/101. Neometals has entered a binding agreement to acquire the tenure, subject to the satisfaction of considtions precedent.
There are no known impediments to operate in the area.
Exploration done by other parties
Acknowledgment and appraisal of exploration by other parties.
Exploration has been undertaken by previous holders, but predominantly Western Mining Corporation (WMC) during the 1980s and early 1990s.
Programs of diamond and RC drilling were undertaken by WMC as well as resource estimates, metallurgical test work and economic evaluations.
Geology Deposit type, geological setting and style of mineralisation. The Widgiemooltha area lies within the southern part of the Norseman‐Wiluna greenstone belt.
The stratigraphy at a deposit scale consists of the Archaean Mt Edwards basalt overlain by the Widgiemooltha Komatiite. The ultramafic succession consists of a series of flows with intercalated sediments. It is approximately 250m thick and displays carbonate alteration and serpentinisation. The mineral assemblages are talc‐ antigorite‐chlorite‐magnetite and talc‐magnesite‐amphibolite‐ magnetite. Stronger carbonate –chlorite alteration is noted around the mineralised lenses.
The nickel mineralisation at Cooke occurs on or above the ultramafic/mafic contact and is associated with a steep northerly plunging synclinal structure. The syncline plunges at about 50 degrees to the north and dips steeply to the east.
WMC geologists recognised three mineralised surfaces;
• Western inner synclinal contact, within which mineralisation is variable, from heavy matrix contact mineralisation in the synclinal keel, to lower tenor disseminated mineralisation in the north.
• Eastern inner contact, which consists of high grade low tonnage mineralised zone that has limited strike and down dip potential.
• Southern outer contact, which is typically heavy matrix in character, with minor massive mineralisation.
The nickel mineralisation has been defined over a strike of 180 metres and to a depth of 350 metres below the surface. True For
per
sona
l use
onl
y
thickness of mineralisation varies from 2 metres to up to 10 metres.
Depth of oxidation is up to 40 metres.
Drill hole Information
A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:
easting and northing of the drill hole collar, elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar, dip and azimuth of the hole down hole length and interception depth hole length.
If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.
See Appendix 3 above.
Data aggregation methods
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut‐off grades are usually Material and should be stated.
Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.
The assumptions used for any reporting of metal equivalent values should be clearly stated.
Drill hole summary results are included in this release. The results reported include all intersections included in the estimation of the resource.
A nominal cut off of 1.0% Ni was used to define the drill intersections composites. A 2m maximum internal dilution was used.
No metal equivalents are used in this Mineral Resource estimate.
Relationship between mineralisation widths and intercept lengths
These relationships are particularly important in the reporting of Exploration Results.
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.
If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg ‘down hole length, true width not known’).
The drill line and drill hole orientation is oriented as close to 90 degrees to the orientation of the anticipated mineralised orientation as practicable.
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.
See figures above.
Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high
All drill intercepts used in the estimation of the resource envelope irrespective of grade are reported above. The Resource envelope is constructed using a nominal 1.0% Ni cut‐off and a maximum drilled internal dilution of 2m. F
or p
erso
nal u
se o
nly
grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.
Other substantive exploration data
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.
Mineral Resources were estimated from drill hole assay data, with geological logging used to aid interpretation of mineralised contact positions.
Geological observations are included in the report. All core drilled at Cooke is available for review and is stored at the Fisher mine offices in Kambalda.
Multi‐element assay suites have been analysed and arsenic has been identified as a potentially deleterious element.
Bulk density measurements have been taken and analysed. SGs were assigned to the block model using the formula Bulk density (t/m3) = 167.0654/ (57.6714 – Ni %).
Further work The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large‐scale step‐out drilling).
Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.
No further work is planned at this stage.
There is potential for possible extensions in the down plunge position to the current Mineral Resource, but the grades are considered far too low to be economic at those depths.
Drill spacing is currently considered adequate to undertake limited high level economic evaluations on the project. Infill drilling would be required if more detailed feasibility studies were to be undertaken
Cooke deposit: Section 3 Estimation and Reporting of Mineral Resources
Criteria JORC Code explanation Commentary
Database integrity Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes.
Data validation procedures used.
The drill hole database was sourced from original hard‐copy sampling and assay records.
Validation measures included spot checking between database and hard copy drill logs and sections and plans in historic reports.
The database is an extract from an Industry Standard SQL Server database using a normalised assay data model produced by Datashed Software.
Site visits Comment on any site visits undertaken by the Competent Person and the outcome of those visits.
If no site visits have been undertaken indicate why this is the case.
Mr. Marshall visited Cooke numerous times between 2005 and 2007 and was intimately involved in the planning and implementation of drilling programs completed during that time. Mr Marshall was also directly involved in the historic data compilation and validation for the project.
Geological interpretation
Confidence in (or conversely, the uncertainty of) the geological interpretation of the mineral deposit.
Nature of the data used and of any assumptions made.
The effect, if any, of alternative interpretations on Mineral Resource estimation.
The use of geology in guiding and controlling Mineral Resource estimation.
The factors affecting continuity both of grade and geology.
The Cooke deposit was discovered in the 1960’s. The project was acquired by WMC in 1979 and actively explored until the 1990’s. The project was acquired by Titan Resources Limited in 2001 as part of the acquisition of the Widgiemooltha North tenement package. Titan Resources were subsequently taken over by Consolidated Minerals (Consmin) in 2006. Consmin do not appear to have completed any meaningful work. As a result, an extensive body of knowledge exists for the project and therefore confidence in in terpretations is relatively high.
Historical data as well as recent data collected by Titan were used in the interpretations. The data from different companies and time periods correlated very well.
For this Mineral Resource estimate a 1% Ni cut‐off was used, with the interpretation based on structural and stratigraphic For
per
sona
l use
onl
y
controls. The only valid departure from this interpretation would be to apply a different grade cut‐off.
Wireframe boundaries do not appear to be “snapped” to drilling intercepts using the sample positions. Interpretations were prepared on 30m section spacing cut at bearing 90 degrees on the MGA94 grid zone 51 grid.
The drill spacing is relatively wide and introduces sufficient uncertainty for the short range variability and continuity in the deposit. The mineralisation is hosted in a high strain environment which can adversely affect the continuity of the mineralisation and mine reconciliations back to the resource model.
Given the current wide drill spacing, pinching, swelling and truncation of the mineralisation is possible between the drill holes, as observed in many of the nickel mining operations in the area.
The boundaries of the broader mineralised zone are consistent, but within these zones, higher/ lower grade and thicker/ thinner zones occur. It is expected that additional drilling will define the distribution and nature of this variability.
Dimensions The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource.
The Mineral Resources extend over a strike length of approximately 180 m. The resource models extend to 350 m depth below surface.
The Mineral Resource is unmined.
Estimation and modelling techniques
The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used.
The availability of check estimates, previous estimates and/or mine production records and whether the Mineral Resource estimate takes appropriate account of such data.
The assumptions made regarding recovery of by‐products.
Estimation of deleterious elements or other non‐grade variables of economic significance (eg sulphur for acid mine drainage characterisation).
In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed.
Any assumptions behind modelling of selective mining units.
Any assumptions about correlation between variables.
Description of how the geological interpretation was used to control the resource estimates.
Discussion of basis for using or not using grade cutting or capping.
The process of validation, the checking process used, the
Grades were estimated by ordinary kriging estimation of 1.5m down‐ hole composited nickel and inverse distance squared for arsenic assay grades from diamond and RC holes within mineralised domain wireframes.
Micromine software was used for data compilation, domain wire‐ framing, and coding of composite values, statistics, geostatistics and resource estimation.
Previous Mineral Resource estimates have been made by several companies from 1990’s onwards. The more recent estimates compare well with the current one as follows;
126,0000 tonnes @ 1.85% Ni (WMC circa 1990’s)
163,989 tonnes @ 1.62% Ni (Titan Resources 2004)
No consideration has been made for the recovery of by‐products.
Arsenic is a significant deleterious element.
No consideration has been made with regard to sulphur levels in the waste material but the assays are available. This is due to the preliminary nature of economic evaluation to date.
Resources were estimated into 10m by 10m x 2.5m parent blocks (strike, vertical, cross strike) aligned around N‐S on MGA94.
For precise volume representation, sub‐blocking was allowed to 2.5m x2.5m x 0.3125m.
The nickel modelling included used an anisotropic search ellipsoid with minimum data requirements of 8 data points and a maximum of 32 points for pass 1 & 2. On the third pass the number of samples was reduced to a minimum of 4 samples and a maximum of 24. The starting search ellipse was 30m (Y) by 30m (Z) by 10m (X). This was increased to 60m (Y) by 60m (Z) by 20m (X) on the second pass and 90m (Y) by 90m (Z) by 30m (X) on the third pass.
For
per
sona
l use
onl
y
comparison of model data to drill hole data, and use of reconciliation data if available.
The estimates are not intended to reflect a fixed mining method but could be amenable to several mining techniques.
Details of potential mining parameters have been considered but reflect the early stage of the project evaluation.
There is a strong correlation between Nickel and Copper; Nickel and Cobalt; and Nickel and Sulphur (fresh rock). Further there is strong evidence that there is a good correlation between Nickel mineralisation and bulk density.
The geology and grade information was used in the creation of the mineralised domain wireframes. A nominal 1.0% Ni cut‐off was used to define the outline within geological units. The selection of this cut‐ off is natural and corresponds with relatively “hard” mineralisation boundaries.
No grade cutting or capping has been used. Grades are relatively uniform within a defined range, with no order of magnitude outlying high grades that would materially affect the resource.
The block model was validated by viewing in vertical section and plan and comparing to the samples. Declustered sample grades were compared to the resource model block grades.
There is no production information to reconcile against the model.
Moisture Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content.
Tonnages are estimated on a dry tonnage basis.
Cut‐off parameters The basis of the adopted cut‐off grade(s) or quality parameters applied.
The cut off grades reflect Neometals’ perception of the potential range of operating costs and prices of nickel.
The mineralised envelope is modelled using a 1.0% Ni cut‐off grade.
Mining factors or assumptions
Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the mining assumptions made.
Neometals has considered the possibility of both open cut and underground mining on the project.
High level scoping studies have been completed by Titan Resources in 2006. Cooke was found to be sub economic at the time.
Dependant on the cost parameters used and the nickel price, Mineral Resource, or part thereof, is potentially amenable to open cut or underground mining.
For
per
sona
l use
onl
y
Metallurgical factors or assumptions
The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous.
Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made.
Metallurgical test work was conducted by Western Mining in 1998 from nearby deposits such as Widgiemooltha Townsite. The study indicated a nickel recovery of 90% producing a concentrate grade of 8% Ni, 5% MgO and 5000ppm As from a head grade of 2.5% to 2.6% Ni.
Bond Work index was low at 7.8KWhr/t which would result in lower processing costs.
Talc content is approximately 45% in the mineralisation so suppression of talc would be of utmost importance.
The high arsenic levels would present a problem of the concentrate was to feed the NickelWest Smelter.
Iron rich areas lead to high S to Ni ratios of 3.8 resulting in low Ni concentrate grade.
Environmental factors or assumptions
Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfields project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made.
Precise details of potential waste and process residue disposal options are unclear reflecting the early stage of project evaluation.
High talc and carbonate content and low sulphide content the waste rock suggest that ARD should not be a problem.
Bulk density Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples.
The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc.), moisture and differences between rock and alteration zones within the deposit.
Discuss assumptions for bulk density estimates used in the evaluation process of the different materials.
Bulk density was derived from WMC’s historical regression where Bulk density (t/m3) = 167.0654/ (57.6714 – Ni %).
Bulk density is quoted on a dry basis.
Waste bulk density was not estimated (reason not known).
Classification The basis for the classification of the Mineral Resources into varying confidence categories.
Whether appropriate account has been taken of all relevant factors (ie relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the data).
Resource classification was assigned on the basis of geological continuity and confidence and the number of drill hole intersections.
The resource classification accounts for all relevant factors in the opinion of the Competent Person.
Classification of the estimates reflects the Competent Person’s views of the deposit.
For
per
sona
l use
onl
y
Whether the result appropriately reflects the Competent Person’s view of the deposit.
Audits or reviews The results of any audits or reviews of Mineral Resource estimates.
A detailed audit was completed on the Mineral Resource estimate to prepare this JORC 2012 statement.
Discussion of relative accuracy/ confidence
Where appropriate a statement of the relative accuracy and confidence level in the Mineral Resource estimate using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the resource within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate.
The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used.
These statements of relative accuracy and confidence of the estimate should be compared with production data, where available.
Confidence in the relative accuracy of the estimates is reflected by the classifications assigned in the block model.
The geostatistical procedures used to estimate, quantify and qualify the block model were completed to a reasonable standard. Usually a nickel estimate will include other attributes including non‐sulphide nickel, copper, cobalt, MgO, iron and sulphur. It is unknown why these were not estimated.
No blocks have been assigned an Indicated Mineral Resource or Measured Mineral Resource category which reflects the relative confidence, or lack thereof, in the accuracy of the interpretations.
Significant doubts about the validity of the wireframe interpretations exist as the Mineral Resource is located in a structurally complex and highly strained environment. This has been demonstrated by mining activity on other similar deposits in the Widgiemooltha area.
There is a low ‐ moderate level of confidence in the spatial accuracy of the datasets used in the Mineral Resource estimate as the survey control is unknown.
No production data are available for reconciliation as no mining has been undertaken on the project.
For
per
sona
l use
onl
y
Zabel deposit and McEwen and McEwen Hangingwall deposit: Section 1 Sampling Techniques and Data
Criteria JORC Code explanation Commentary
Sampling techniques
Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.
Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.
Aspects of the determination of mineralisation that are material to the Public Report.
In cases where ‘industry standard’ work has been done this would be relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information.
Zabel and McEwen have been drilled by percussion, diamond drilling and RC drilling. Accurate drilling data exists for 1423 drillholes for 130620 metres in the Zabel McEwen dataset. A total of 225 holes had one or more intercepts over 1% Ni. Of these no intercepts were rejected due to inconsistent spatial positioning.
Assay data were missing from the following holes which intersect the mineralised wireframe interpretations at the time of this report; WD5810, WD5330, WD5818, WD4140, WD8142, WD5327, WDC047, WDC024, WD5822, WD8195. These holes are included in the mineralisation interpretations, and they have assay intervals, so the assay data would exist.
The holes have been drilled on irregular spacing as tight as 10m by 10m in the central higher grade parts of the mineralisation and up to 100m by 50m towards the extremities and low grade areas.
Diamond holes were selectively sampled through the visible mineralised zone on a nominal 1m sample length, adjusted to geological and domain boundaries. Sample lengths vary from 0.03m to 18.29m.
Diamond core samples have been sampled by a combination of quarter core and half core cut samples and a combination of BQ, NQ and HQ diameter.
Sample representivity for diamond core was ensured by the sampling of an average length of 1m of core, which was then cut to quarter or half, depending on the company operating at the time, for laboratory analysis.
RC sampling was riffle split from 1m composite bulk samples, producing a nominal 3kg – 5kg representative sample. RC drillholes were sampled by 1m riffle split composites. RC drilling was 5 ¼ inch in diameter.
Sample lengths for diamond drilling range from 0.03 to 18.29 m and average approximately 1.3 m. RC samples lengths used in the Mineral Resource estimate were all 1m in length.
Mineralised intervals are determined by visual inspection and logging prior to any sampling. Laboratory assays are then compared to the visual estimates and logging to determine if any adjustments are required.
Mineralisation is identified pyrrhotite and pentlandite with minor chalcopyrite hosted in talc‐ carbonate ultramafics.
For Titan and Consmin drilling, representative samples from RC and diamond drilling were collected and sent to accredited laboratories for analysis. Accredited laboratories in Kalgoorlie and Perth crushed and pulverised the samples in entirety, and took a 50g pulp for analysis. This process cannot be established for drilling completed before 2005.
For Titan and Consmin samples, analysis was performed by 4 acid digest and a combination of ICP‐MS and ICP‐OES multi element analysis techniques. Gold and PGEs were determined by a fire assay fusion followed by aqua regia digest with atomic absorption spectrometer (AAS) and ICP‐MS finish. Analysis techniques were not established for samples taken before 2005, but the results generally correlate well with newer data.
Minor copper, cobalt and arsenic occur in the mineralisation.
Drilling techniques Drill type (e.g. core, reverse circulation, open‐ hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (e.g. core diameter, triple or standard tube, depth of diamond tails, face‐ sampling bit or other type, whether core is oriented and if so, by what method, etc.).
The database used in the Mineral Resource is comprised of diamond drilling samples (27803), RC drilling samples (7380), Unspecified (24084). Most of the unspecified samples are actually historic diamond drilling drilled predominantly by Western Mining during the early 1980s.
Diamond drilling included NQ, HQ and BQ diameter core.
For
per
sona
l use
onl
y
Drill sample recovery
Method of recording and assessing core and chip sample recoveries and results assessed.
Measures taken to maximise sample recovery and ensure representative nature of the samples.
Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.
Core recoveries were only recorded for five drillholes completed by Titan. Therefor no meaningful determination can be made with respect to core recoveries.
RC samples recoveries or weights were not recorded. The lack of sample recovery information downgrades the confidence in the Mineral Resource estimate.
No relationship could be established between sample recovery and reported grade. RC samples report a lower average grade than core samples overall which is related their being drilled as RC pre‐collars intersecting lower grades portions outside of main body of the mineralisation, and diamond drilling focusing on higher grade portions of the orebody.
Logging Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.
Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc.) photography.
The total length and percentage of the relevant intersections logged
Detailed drill hole logs (all drilling), geotechnical and structural logs (core only) are available for the drilling.
Separate sample logging sheets are kept including samples numbers for duplicates, standards and blanks taken for QA/QC purposes.
The logging is of a reasonably detailed nature, and of sufficient detail to support the current Inferred Mineral Resource estimate category.
The total length of drill intersections used in the Mineral Resource estimate is 1662.68 and a majority of those intersections are logged.
Sub‐sampling techniques and sample preparation
If core, whether cut or sawn and whether quarter, half or all core taken.
If non‐core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry.
For all sample types, the nature, quality and appropriateness of the sample preparation technique.
Quality control procedures adopted for all sub‐ sampling stages to maximise representivity of samples.
Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second‐half sampling.
Whether sample sizes are appropriate to the grain size of the material being sampled.
The core was halved or quartered, depending on which company and phase of work, by sawing before sampling
RC drilling was riffle split directly from the sample collection cyclone on the drilling rig.
Sample condition field to record moisture and sample recovery is included in the sampling log sheet and populates the assay table of the database. Unfortunately only a very small percentage of the logs have captured this information so no determination can be made about the quality of the RC samples.
Sample preparation is considered to be appropriate for RC and diamond drilling as per industry standard practices for managing RC samples and diamond core.
Quality control procedures for Titan drilling included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis. At the time of writing no QAQC samples were included in the dataset used for the Mineral Resource estimate. This downgrades confidence in the data.
Host rock is mainly a talc‐carbonate ultramafic with minor interflow sediments (black shales).
Samples of diamond core and RC samples produce appropriate size samples to be representative for the style of mineralisation and rock type encountered.
Quality of assay data and laboratory tests
For geophysical tools, spectrometers, handheld XRF instruments, etc., the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.
Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.
Quality control procedures included the inclusion of field duplicates, standard samples and blank samples into the sampling stream for laboratory analysis.
One standard, blank and field duplicate were inserted into the sample stream every 20 samples. These were offset through the sampling stream and placed in areas of interest i.e. high grade standards and blanks in the ore zone where possible.
No assessment could be made regarding QAQC as no QAQC samples were included in the dataset used in the Mineral Resource estimate.
No geophysical methods or hand‐held XRF units have been used for determination of grades in the Mineral Resource estimate.
For
per
sona
l use
onl
y
Verification of sampling and assaying
The verification of significant intersections by either independent or alternative company personnel.
The use of twinned holes.
Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.
Discuss any adjustment to assay data.
Intersections reported have been checked back to original logs and assay data.
No twin holes have been drilled.
Drill hole data were sourced from digital sources and original hard‐ copy sampling and assay records, and imported into a central electronic database. Datashed software was used to validate and manage the data.
Assays were composited to 1m lengths and where necessary top cuts applied for resource estimation.
Location of data points
Accuracy and quality of surveys used to locate drill holes (collar and down‐hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.
Specification of the grid system used. Quality and adequacy of topographic control.
Quality of the surface topography data could not be confirmed.
Collar co‐ordinates were either by handheld GPS or unconfirmed.
A majority of the drillholes were downhole surveyed with gyroscopic survey tool. The remaining holes were surveyed by single shot tool and by collar measurement with a clinometer and compass. Significant magnetic interference is present at Zabel and McEwen, reducing the reliability of single shot surveys.
Original surveying was undertaken in Kambalda Nickel Operations Grid (KNO).
Topographic control is considered adequate for the current Mineral Resource estimate, but it is strongly recommended that a surface survey be completed by a licenced surveyor before any further drilling or economic evaluations are completed.
Data spacing and distribution
Data spacing for reporting of Exploration Results.
Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.
Whether sample compositing has been applied
The resource area has been drilled on an irregular pattern and spacing by several different companies over an extended period. The average spacing is estimated to be approximately 30m by 30m for Zabel and McEwen and 50m by 50m for McEwen Hangingwall.
The drill data spacing and sampling is adequate to establish the geological and grade continuity required for the current Mineral Resource estimate.
Diamond drill hole samples were composited to 1.5 m down‐hole intervals for resource modelling. RC Samples used in the estimate were composited to 1m intervals already.
Orientation of data in relation to geological structure
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.
If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.
The drill line and drill hole orientation is oriented as close as practicable to perpendicular to the orientation of the general mineralised orientation.
A majority of the drilling intersects the mineralisation at close to 90 degrees ensuring intersections are representative of true widths. Several holes are drilled at a low angle to the mineralisation, the reasons for which are unclear.
Sample security The measures taken to ensure sample security. Reports and original log files indicate at a thorough process of logging, recording, sample storage and dispatch to labs was followed at the time of drilling.
For Titan drilling, sample security measures adopted include the daily movement of core samples in trays to the Kalgoorlie Office, where core was kept in a secure area before cutting and sampling.
RC split samples were transported from site daily and delivered to the accredited laboratory depot in Kalgoorlie for preparation and analysis.
Reports and original log files indicate at a thorough process of logging, recording, sample storage and dispatch to labs was followed at the time of drilling.
Security could not be confirmed for drilling completed before 2005.
For
per
sona
l use
onl
y
Audits or reviews The results of any audits or reviews of sampling techniques and data.
Sample data reviews have included an inspection and investigation of all available paper and digital geological logs to ensure correct entry into the drillhole database.
Visualisation of drilling data in three dimensional software (Micromine and Surpac) was Although these reviews are not definitive, they provide confidence in the general reliability of the data.
Zabel deposit and McEwen and McEwen Hangingwall deposit: Section 2 Reporting of Exploration Results
Criteria JORC Code explanation Commentary
Mineral tenement and land tenure status
Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.
The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.
Apollo holds a 100% interest the nickel and base metal rights to the project. Neometals has entered a binding agreement to acquire the tenure, subject to the satisfaction of considtions precedent.
There are no known impediments to operate in the area.
Exploration done by other parties
Acknowledgment and appraisal of exploration by other parties.
Exploration has been undertaken by previous holders, but predominantly Western Mining Corporation (WMC) during the 1980s.
Programs of diamond drilling were undertaken by WMC as well as resource estimates, metallurgical test work and economic evaluations.
Geology Deposit type, geological setting and style of mineralisation. Zabel and McEwen ware interpreted to be structurally and hydrothermally modified and remobilised Kambalda style nickel occurrences.
At prospect scale the major structural feature is the Widgiemooltha North Anticline, an isoclinal fold striking at 337 and plunging shallowly to the north. The Widgiemooltha North Anticline is the dominant control on the geometry of the mineralisation.
The Zabel deposit is dominated by basal contact and footwall stringer ore. It is poddy and structurally modified. The thickest, highest grade ore tends to be associated with serpentinite hangingwall although most of the ultramafic is completely altered to talc carbonate with minor tremolite. The orebody is bounded to the south by the presence of shale on the contact and is as yet not closed off sufficiently at depth. Zabel tends to be of higher tenor than McEwen with massive ore averaging around 6.5%. Continuity between sections has been assumed at Zabel although not proven. The overall plunge at Zabel is 30 degrees to the north, but the high grade pristine parts of the ore plunge steeply to the south. Much of the ore is sheared. The structural evolution at Zabel is not adequately understood.
The McEwen deposit contains both disseminated hanging wall ore and basal contact massive ore towards the southern end. The southern portion of McEwen is dominated by serpentinite which grades into talc carbonate assemblages to the north. This corresponds with the disappearance of high grade contact ore. Most of the hanging wall ore occurs north of the contact ore but some occurs at the south end of the deposit as well. Felsic intrusives and metasediments are common in the hangingwall sequence at McEwen. Continuity could be assumed with more confidence at McEwen although grades tended to be low. Less structural modification has occurred at McEwen. F
or p
erso
nal u
se o
nly
Depth of complete oxidation is up to 60 metres, with a further ~30‐ 50m of supergene zone below the base of oxidation.
Drill hole Information
A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:
easting and northing of the drill hole collar elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar dip and azimuth of the hole down hole length and interception depth, and hole length.
If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.
Drill infromation in Appendix 3 above. No information is excluded.
Data aggregation methods
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut‐off grades are usually Material and should be stated.
Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.
The assumptions used for any reporting of metal equivalent values should be clearly stated.
Drill hole summary results are included in this release. The results reported include all intersections included in the estimation of the resource.
A nominal cut‐off of 1.0% Ni was used to define the drill intersections composites. A 2m maximum internal dilution was used.
Appendix 4 this announcement contains all weighted composites included in the Mineral Resource estimate. Higher grade intersections within the composites are included in the table.
No metal equivalents are used in this Mineral Resource estimate.
Relationship between mineralisation widths and intercept lengths
These relationships are particularly important in the reporting of Exploration Results.
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.
If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg ‘down hole length, true width not known’).
The drill line and drill hole orientation is oriented as close to 90 degrees to the orientation of the anticipated mineralised orientation as practicable.
The majority of the drilling intersects the mineralisation at close to 90 degrees. The following holes were drilled at a low angle to the mineralisation and therefore intercept widths are wider than true widths; WD3831, WD3837, WD3839.
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.
Appropriate maps and tables are included in the body of the Anniuncement.
For
per
sona
l use
onl
y
Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades
and/or widths should be practiced to avoid misleading reporting of Exploration Results.
All drill intercepts used in the estimation of the resource envelope irrespective of grade are reported in Appendix 4. The resource envelope is constructed using a nominal 1.0% Ni cut‐off and a maximum drilled internal dilution of 2m.
All drillhole collars are reported in Appendix 3.
Other substantive exploration data
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.
Mineral Resources were estimated from drill hole assay data, with geological logging used to aid interpretation of mineralised contact positions.
Geological observations are included in the report. All core drilled at Zabel and McEwen is available for review and is stored at the Fisher mine offices in Kambalda.
Metallurgical testwork is out of the scope of this announcement.
Multi‐element assay suites have been analysed and arsenic has been identified as a potentially deleterious element.
Bulk density measurements have been taken and analysed. A regression line was determined for fresh mineralised samples of (Ni * 0.152) + 2.911 =SG.
Further work The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large‐scale step‐out drilling).
Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.
No further work is planned at this stage.
There is potential for possible extensions in the down plunge position to the current Mineral Resources, but the grades are considered far too low and widths too narrow to be economic at those depths.
Drill spacing is currently considered adequate to undertake limited high level economic evaluations on the project. Infill drilling would be required if more detailed feasibility studies were to be undertaken.
Zabel deposit and McEwen and McEwen Hangingwall desposit: Section 3 Estimation and Reporting of Mineral Resources
Criteria JORC Code explanation Commentary
Database integrity Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes.
Data validation procedures used.
The drill hole database was sourced from original hard‐copy and digital sampling and assay records.
Validation measures included spot checking between database and hard copy drill logs and sections and plans in historic reports.
The database is an extract from an Industry Standard SQL Server database using a normalised assay data model produced by Datashed Software.
Site visits Comment on any site visits undertaken by the Competent Person and the outcome of those visits.
If no site visits have been undertaken indicate why this is the case.
Mr. Marshall visited Zabel and McEwen numerous times between 2005 and 2007 and was intimately involved in the planning and implementation of drilling programs completed during that time. Mr Marshall was also directly involved in the historic data compilation and validation for the project.
Geological interpretation
Confidence in (or conversely, the uncertainty of) the geological interpretation of the Mineral deposit.
Nature of the data used and of any assumptions made.
The effect, if any, of alternative interpretations on Mineral
Zabel and McEwen were discovered in the 1970’s and evaluated intermittently by several companies since. Most of the data for the project was collected by WMC during the 1980s. As a result an extensive body of knowledge exists for the project and therefore confidence in interpretations is relatively high.
Historical data as well as recent data collected by Titan and Consmin were used in the interpretations. The data from different For
per
sona
l use
onl
y
Resource estimation.
The use of geology in guiding and controlling Mineral Resource estimation.
The factors affecting continuity both of grade and geology.
companies and time periods correlated very well.
For this Mineral Resource estimate a 1% Ni cut‐off was used, with the interpretation based on structural and stratigraphic controls. The only valid departure from this interpretation would be to apply a different grade cut‐off.
Wireframe boundaries were “snapped” to drilling intercepts using the sample positions, with the use of geological logging being used as a guide when considering the interpretation of the mineralised wireframe. Interpretations were prepared on 20m section spacings cut at bearing 90 degrees on the AMG84 grid.
The drill spacing is relatively wide and introduces sufficient uncertainty for the short range variability and continuity in the deposit. The mineralisation is hosted in a high strain environment which can adversely affect the continuity of the mineralisation and mine reconciliations back to the resource model.
Given the current wide drill spacing, pinching, swelling and truncation of the mineralisation is possible between the drillholes, as observed in many of the nickel mining operations in the area.
The boundaries of the broader mineralised zone are consistent, but within these zones, higher/ lower grade and thicker/ thinner zones occur. It is expected that additional drilling will define the distribution and nature of this variability.
Dimensions The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource.
The Mineral Resources extend over a strike length of approximately 2900 m. The resource models extend to 425 m depth below surface.
The Mineral Resource is unmined.
Estimation and modelling techniques
The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used.
The availability of check estimates, previous estimates and/or mine production records and whether the Mineral Resource estimate takes appropriate account of such data.
The assumptions made regarding recovery of by‐products.
Estimation of deleterious elements or other non‐grade variables of economic significance (eg sulphur for acid mine drainage characterisation).
In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed.
Any assumptions behind modelling of selective mining units.
Any assumptions about correlation between variables.
Description of how the geological interpretation was used to control the resource estimates.
Grades were estimated predominantly by Ordinary Kriging estimation of 1.5m down‐hole composited nickel, cobalt and copper assay grades from diamond and RC holes within mineralised domain wireframes.
Surpac software was used for data compilation, domain wire‐framing, and coding of composite values , statistics, geostatistics and resource estimation.
Previous Mineral Resource estimates have been made by several companies from 1987: 8.24Mt at 0.98% Ni (Titan 2004 reported at 0.5% Ni cut‐ off).
No consideration has been made for the recovery of by‐products.
Arsenic is a significant deleterious element. It is quoted in the Mineral Resource table.
No consideration has been made with regard to sulphur levels in the waste material but the assays are available. This is due to the preliminary nature of economic evaluation to date.
Resources were estimated into 10m by 10m x 5m parent blocks (strike, vertical, cross strike) aligned to 340 azimuths on AMG84 grid.
For precise volume representation, sub‐blocking was allowed to 2.5m x1.25m x 0.3125m.
The modelling included used an anisotropic search ellipsoid with minimum data requirements of 4 data points and a minimum of two holes.
The estimates are not intended to reflect a fixed mining method but could be amenable to several mining techniques.
Details of potential mining parameters have been considered but reflect the early stage of the project evaluation.
Block maths for specific gravity (SG) = nickel grade X 0.152 + 2.911. The correlation for SG was defined by Cervoj (2007) due to the fact not all samples had SG measurements.
No correlation was able to be established between nickel and arsenic. Arsenic is interpreted to be controlled by stratigraphy For
per
sona
l use
onl
y
Discussion of basis for using or not using grade cutting or capping.
The process of validation, the checking process used, the comparison of model data to drill hole data, and use of reconciliation data if available.
faults and shears within the greenstone sequence.
The geology and grade information was used in the creation of the mineralised domain wireframes. A nominal 1.0% Ni cut‐off was used to define the outline within geological units. The selection of this cut‐ off is natural and corresponds with relatively “hard” mineralisation boundaries.
Grade top cutting has been applied as follows; Zabel Ni 5%, McEwen Hangingwall Ni 3.5%, As 1500ppm, McEwen East Ni 2.5%, As 1000ppm, McEwen West Ni 3.5%, As 4000ppm.
This approach might be reconsidered for future Mineral Resource estimates given the lack of any real nugget effect in the nickel environment.
Model validation included visual comparison of model estimates and composite grades using section analysis with the raw drilling data and the composite data.
There is no production information to reconcile against the model.
Moisture Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content.
Tonnages are estimated on a dry tonnage basis.
Cut‐off parameters The basis of the adopted cut‐off grade(s) or quality parameters applied.
The cut off grades reflect Neometals’ perception of the potential range of operating costs and prices of nickel.
The mineralised envelope is modelled using a 1.0% Ni cut‐off grade.
Mining factors or assumptions
Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the mining assumptions made.
Neometals has considered the possibility of both open cut and underground mining on the project. No detailed design work has been completed.
No reportable economic evaluations have been completed to the knowledge of the author.
Dependant on the cost parameters used and the nickel price, Mineral Resource, or part thereof, is potentially amenable to open cut or underground mining.
Metallurgical factors or assumptions
The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous.
Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made.
No metallurgical testwork information was available at the time of reporting.
For
per
sona
l use
onl
y
Environmental factors or assumptions
Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfields project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made.
Precise details of potential waste and process residue disposal options are unclear reflecting the early stage of project evaluation.
High talc and carbonate content and low sulphide content the waste rock suggest that ARD should not be a problem.
Bulk density Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples.
The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc.), moisture and differences between rock and alteration zones within the deposit.
Discuss assumptions for bulk density estimates used in the evaluation process of the different materials.
535 samples were determined by weight in air weight in water technique. Cervoj (2007) completed statistics and a regression between nickel and specific gravity measurements. That work was also used as the basis for specific gravity measurements in the current block model. A regression line was determined for fresh mineralised samples of (Ni * 0.152) + 2.911 =SG.
No allowance was made for the effect of weathering in the model.
Classification The basis for the classification of the Mineral Resources into varying confidence categories.
Whether appropriate account has been taken of all relevant factors (ie relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the data).
Whether the result appropriately reflects the Competent Person’s view of the deposit.
Resource classification was assigned on the basis of geological continuity and confidence, the number of drill hole intersections, and average distance to samples.
The resource classification accounts for all relevant factors in the opinion of the Competent Person.
Classification of the estimates reflects the Competent Person’s views of the mineralisation.
Audits or reviews The results of any audits or reviews of Mineral Resource estimates.
A detailed audit was completed on the Mineral Resource estimate to prepare this JORC 2012 statement.
Discussion of relative accuracy/ confidence
Where appropriate a statement of the relative accuracy and confidence level in the Mineral Resource estimate using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the resource within stated confidence limits, or, if such an
Confidence in the relative accuracy of the estimates is reflected by the classifications assigned in the block model
The geostatistical procedures used to estimate, quantify and qualify the block model were completed to a high standard
No blocks have been assigned a Measured Mineral Resource or Indicated Mineral Resource category which reflects the relative confidence, or lack thereof, in the accuracy of the interpretations
Significant doubts about the validity of the wireframe interpretations exist as the Mineral Resource is located in a structurally complex and highly strained environment. This has been demonstrated by mining activity on other similar deposits in the F
or p
erso
nal u
se o
nly
approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate.
The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used.
These statements of relative accuracy and confidence of the estimate should be compared with production data, where available.
Widgiemooltha area.
There is a low level of confidence in the spatial accuracy of the datasets used in the Mineral Resource estimate as the survey control is poor (handheld GPS).
No production data are available for reconciliation as no mining has been undertaken on the project.
For
per
sona
l use
onl
y