VLADIMIR SIMIĆ - ICerS · University of Belgrade Faculty of Mining and Geology Department of...
Transcript of VLADIMIR SIMIĆ - ICerS · University of Belgrade Faculty of Mining and Geology Department of...
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University of BelgradeFaculty of Mining and GeologyDepartment of Economic GeologyBelgrade, [email protected]
January 29, 2015Annual Meeting on Raw Materials for Ceramic Tiles 1
VLADIMIR SIMIĆ
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Introduction Serbia Bosnia & Hercegovina◦ Republic of Srpska◦ Federation of BiH
Slovenia Macedonia Croatia Ranking
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Clays made predominantly of kaolinite and/orillite, with variable content of other clayminerals, quartz, feldspar and mica.
Firing colour usually white or near-white(buff, pale grey, beige)
No carbonates
Relatively low Fe content
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JORC, PERC OR NI 14-101 definition
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According to Kužvart, 1984
Small < 0.5 Mt Medium 0.5-1.0 Mt Large 1-5 Mt Very large > 5 Mt
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Country Comm. 2008 2009 2010 2011 2012 2013Serbiae Ceramic clay 150 150 150 130 130 130-Kosovo Clays 20.8 46.4 22.9 38.8 55.3 50.1B&H Kaolin crude 259.3 148.4 41.8 232.1 149.5Croatiae Ceramic clay 300 300 NA NA NAFYROM Clays,
bentonite22.9 15.3 12.8 14.5 6.9
Slovenia Ceramic clay,crude
32.2 9.5 12.3 10.1 12.0
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Serbia – my estimation of average production of ceramic clays
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ALAS ZORKA-KERAMIKA d.o.o. – www.zorka-keramika.rs
Quartzwerke Gmbh–Kopovi Ub –www.kopoviub.co.rs
ŠAMOT Aranđelovac – www.samot.co.rs (notprivatised yet)
KERAMIKA AD MLADENOVAC (in the processof liquidation)
KAOLIN AD Valjevo, www.kaolin.co.rs
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Basin Primary rock Typical deposit
Main clay minerals
Other clay minerals
Non-clay mineralsMain Other
Aranđelovac Granite Vrbica, Lazine Kaolinite Illite, tr. Al-smectite Quartz Feldspar,
mica
Brajkovac Schists, sub. metaclastics Dren Kaolinite, illite Low Al-
smectite Quartz Feldspar, low mica
Kolubara
Dacite-andesite, pyroclastics Rudovci Kaolinite Low illite, Al-
smectite Quartz
Schists Baroševac Kaolinite, illite Low Al-smectite Quartz Feldspar,
low mica
Vlašić Metaclastics, sub. schists
Bele vode, Jovanovića
brdo, DokmirKaolinite, illite I-S,
Al-smectite Quartz Low feldspar
Jadarska Lešnica Metaklastics, granite Savića mala Kaolinite, illite Low Al-
smectite Quartz Low feldspar
Štubik (East. Serbia) Gneiss Metriš Kaolinite Illite Quartz Mica
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Deposit Owner Explo-red
Partiallyexplored
In operation Out ofoperation
Exausted or almostexausted
Vrbica Šamot + + +Bukovik Šamot + +Ćirinac Šamot + + +Lazine Šamot + +Krušik Šamot + + +Košarno Keramika + +Bukovik-Partizani Šamot + +Kapetanovo Polje Šamot + +Rudovci Šamot + + +Prkosava Šamot + +Baroševac None + +Dren Kolubara + +Dokmir Kopovi + +Jovanovića Brdo Zorka + + +Bele Vode Zorka + +Stare Kuće Zorka + +Burovica Zorka + +Zbegovi Zorka + +Miličinica Kaolin + +Kranjani Kaolin + +Brezaci ? + +Slatina Kopovi + +Savića Mala Zorka + +
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Deposit Owner Clay type Deposit tonnage RemarkSmall Medium Large
Bukovik Šamot Refractory + Thick overburdenLazine Šamot Refractory + Plastic and
carbonaceous clayKošarno Keramika Refractory
Ceramic+
+Thin layersSandy
Prkosava Šamot Refractory + Not explored enough, occasionally thickoverburden, OM
Dren Kolubara Ceramic + Variable gradeDokmir Kopovi Ceramic + Different gradesSlatina Kopovi Ceramic + Exploitation depends
on market foroverlying sands
Bele Vode Zorka Ceramic + Partially exploitedStare Kuće Zorka Ceramic +Burovica Zorka Ceramic +Zbegovi Zorka Ceramic +Brezaci Zorka Ceramic + SandySavića Mala Zorka Refractory
Ceramic+
+Alternation of twoclay grades, coallayers inside clay
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Mostly excavated
Not excavatedBukovik deposit
Vrbica deposit
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Mostly excavated
Blue – kaolinitic clay (carbonaceous and grey)Green – greenish clay, more feldsparBlack – coal
LAZINE DEPOSIT
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Blue – kaolinitic clay K1 & K2Red – kaolinitic clay K5
KOŠARNO DEPOSIT
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Bukovik Ćirinac Lazine OM
Lazine grey
KošarnoK1
KošarnoK5
SiO2 54,13 55,24 48,23 52,69 54,99 70,64Al2O3 29,15 28,81 29,31 30,50 28,61 17,28Fe2O3 3,95 2,69 2,50 2,94 2,82 2,12CaO 0,28 0,94 0,87 0,86 0,59 0,86MgO 0,40 0,23 0,19 0,39 0,63 0,52K2O 1,20 1,26 1,15 1,37 1,56 2,15Na2O 0,31 0,30 0,25 0,13 0,81 0,35LOI 10,53 10,58 17,48 11,45 9,90 5,97PCE (SC) 30/31 31 29/30 28
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Ćirinac deposit, refractory kaolinitic clay
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Parent rock – metaclastic sediments of Upper Paleozoic age
Mineralogy – K and I, IS, Sm, Q Industrial types of clay – Ceramic clays Tectonics – almost no influence Deposits – small to medium
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Dren Dren sandy
DokmirD2
SlatinaPKG-2S
SlatinaPKG-2V
SiO2 61,79 68,01 63.00-67.00 60,00-65,00 49,00-52,00
TiO2 1,03 1,11 0,50-1,00 0,50-1,00 0,50-1,00
Al2O3 23,63 19,01 19,00-23,00 21,00-24,00 28,00-31,00
Fe2O3 2,30 1,77 1,80-2,50 2,00-3,00 2,00-3,00
CaO 0,69 0,57
MgO 0,42 0,32
K2O3,38
2,41
Na2O 0,30
LOI 6,61 7,00 6,00-8,00 6,00-8,00 10,00-12,00
OM na na Max. 2,00 5,00-8,00 10,00-20,00
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Bele vode
Stare kuće
Buro-vica
Reka-ve
Breza-ci
Savićamala-r
Savićamala-c
SiO2 64,28 62,85 59,59 64,84 69,04 53,87 67,49
TiO2 0,66 0,86 0,74 na 0,5 0,92 0,85
Al2O3 21,72 22,23 25,60 21,58 17,27 27,36 19,75
Fe2O3 1,90 1,90 2,21 2,16 1,57 1,68 1,71
CaO 0,52 0,27 0,48 1,24 0,60 0,60 0,39
MgO 0,71 0,86 0,19 1,03 0,64 0,49 0,38
K2O 2,49 3,15 2,62 2,80 2,78 2,16 2,21
Na2O 0,21 0,04 0,18 0,15 0,10 0,11 0,41
LOI 7,52 7,70 8,53 6,64 6,72 12,72 6,40
r-refractoryc-ceramic
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Resources of all clays in Kosovo were 2,5 Mt in 2002 (source:http://enrin.grida.no/htmls/kosovo/SoE/mining.htm)
Resources for ceramic industry in Kosovo weremostly kaolins from the Karačevo deposit(eastern part of Kosovo area)
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Potential basinsaround Bujanovac granite complexKriva reka basin(Kosovo territory)Vranje basin(Serbian territory)
Karačevo kaolin deposit
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REPUBLIKA SRPSKA Deposits in basins:◦ Prijedor◦ Banja Luka◦ Bratunac◦ Laktaši◦ Spreča
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Ceramic Tiles 23
FEDERATION OF BIH: Deposits in basins:◦ Sarajevo-Zenica◦ Sana
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Source rocks:Metamorphicrocks ofPalezoic age Mineralogy:Kaolinite, illite, smectite, quartz, feldsparDeposits:
Crna dolina
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Deposit Measuredresources
Indicatedresources
Inferredresources
As of date
Crna Dolina 7,000 450 2006Krpeljevo 2,300 1,600 1970Puharska 105 1957Rizvanovići 1,000 1976Čelopek 80.5 92.5 1968Carevine 124 315 1969Jezero 1,000 1969Buvač 3,000 1969Rakelići 40 95 1966Kurteš 260 1965
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However, Cvijić (2004) stated that measured & indicated resources in Prijedor basin are around 34.5 Mt, but without giving data for particular deposits
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The most important deposit in Prijedor basin, as well in Republika Srpska
Until several months ago belonged to NEMETALI a.d., now sold to private investor
Not well explored! Thus all resources, not reserves!
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Ceramic clay K1 Ceramic clay K2SiO2 59.82 58.17Al2O3 23.89 23.58Fe2O3 2.05 3.61CaO 0.67 0.82MgO 0.93 1.31K2O 2.67 2.39Na2O 0.56 0.66LOI 9.12 9.15
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K1 <2.5 % Fe K2 2.5-5% Fe
Coal, carbonaceous clay
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Deposit Measuredresources
Indicatedresources
Inferredresources
As of date
Milosavci, Laktaši
100 60 2003
Jelovci 2, Bratunac
260 50 1979
Sočkovac, NE B&H
6,000 2012
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White clay Grey claySiO2 60.59 64.09Al2O3 18.02 21.32Fe2O3 2.95 0.55TiO2 0.80 0.95CaO 0.32 0.28MgO 0.69 0.51K2O 2.32 2.41Na2O 0.33 0.39LOI 4.14 4.91
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Deposit Measuredresources
Indicatedresources
Inferredresources
As of date
Kruhari 1,550 10 2003Čardačište-Kruhari
4,500 3,960 2002
Demiševci 85 94 1970
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Not precisely defined what is ceramic and what common brick clay! Mostly used for brickclays!
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Ten clay deposits;Three in exploitation - Rapajlo, Golo brdo andČavka (all brick clay quality)Other seven deposits that were previouslyexplored and exploited - Zenik, Kobiljača, Bilalovac, Klokot, Pirići, Šljivčica and Jardol are today abandoned, without clear conception andpolicy for further exploration and exploitation (
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Ceramic clay deposits located in 3 basins:Katlanovo Veles Pehčevo
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Pehčevo total resources ofclays ~ 8.2 Mt
Biggest single deposit Elatawith 2,5 Mt ofresources
Basin potentialfor furtherexploration
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Mostly common clays used for brick clayindustry, but previously also used for tiles.
Para Niva deposit – 6 Mt resources, mineralogy: quartz, chlorite, illite, feldspar
Gorna Vrca deposit (used by brick factory) –3.5 Mt resources, 5 % carbonates, mineralogy:quartz, illite, organic matter, chemistry – over6 % of Fe2O3
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4 deposits ofceramic claysin operation:1.Globoko2. Okroglica 13. Šmiklavž4. Hom 1
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2
43
1
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Deposit Clay type Used for Firing colour ResourcesM m3
Globoko GI+II (K, I) Electr. Porc. rose1-5
Globoko GIII (K, I) Pottery whiteOkroglica 1 K, I Wall&floor tiles red ~ 1Šmiklavž K Clinker tiles Brown-red 1-5Hom 1 I, Chl Wall&floor tiles red < 1
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Total ceramic clay resources in Slovenia in 2011 – 4.2 Mt
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Large potential deposit of ceramic clays ILIRSKA BISTRICA
Mineralogy: Illite/mica 35-41%, chlorite 25%, quartz 20-25%, siderite 5-10%, carbonates <0.5%
Geology: up to 60 m thick clay horizon with sand layers
Firing colour: pale to dark brown
Resources: 33 Mt (explored in 1986)
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INKER dd Zaprešić – sanitary ceramics KERAMIKA MODUS, Orahovica – tile producer
Deposits in general medium-sized, no data on exact resources/reserves per single deposit
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2007 2008 2009 2010 2011 2012 2013Resources 5,707 7,533 10,742 8,783 6,461 3,327 2,871Production 88 7.6 35.8 34 18.3 0 0
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11 exploitation fields in Croatia for ceramic and refractory clays
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2 ceramic claydeposits, severalother alreadyexcavated.Mineralogy:Smectite, illite, kaolinite, quartz
Used by INKER d.d. and small localproducers ofhouseholdceramics
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Several ceramic claydeposits, several alreadyexcavated.Mineralogy:Kaolinite, illite, smectite, quartz
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SiO2 68.92-79.08Al2O3 14.30-28.20Fe2O3 0.95-3.31TiO2 0.11-1.61CaO 0.20-1.75MgO 0.10-2.20K2O 0.20-2.72Na2O 0.08-0.51LOI 3.30-15.98
Avanić et al, 2006
Several clay lenses, averagethickness 3.9 m, variablequality
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Loess without carbonate, average thickness 11 mMineralogy:Kaolinite, illite, smectite, quartzReserves:4 Mt (2010)
Orahovica deposit
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Serbia: KošarnoBrezaci
B&H – RS: Prijedor basin (further explorationnecessary for quality contol andexploitation!)
FYROM: Pehčevo basin
Slovenia: Ilirska Bistrica deposit
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To my colleagues who helped me with data collection:
Dr. Duška Rokavec, Geological Survey of Slovenia, Ljubljana, Slovenia [email protected]
Prof. Dr. Orce Spasovski, University Goce Delčev, Štip, FYROM [email protected]
Rade Milićević, Geosfera Belgrade, Serbia, [email protected]
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THANK YOU FOR YOUR ATTENTION!
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Ceramic Tiles 47