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Suzdal Mine, Semey, Abai Region, Kazakhstani
| Regional Level Types | |
|---|---|
| Suzdal Mine | Mine |
| Semey | City of Regional Subordination |
| Abai Region | Region |
| Kazakhstan | Country |
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Latitude & Longitude (WGS84):
50° 2' 41'' North , 79° 45' 6'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Owned/operated by:
Sediment-hosted gold deposit.
The Suzdal orogenic gold deposit is situated in the northwestern part of the West Kalba gold belt in Eastern Kazakhstan and belongs to the type of stringer–disseminated mineralized zones hosted in the Lower Carboniferous black-shale volcanic–carbonate–terrigenous sequences. Mineralization is controlled by the NE-trending Suzdal Fault. Mineralization is superposed on the Late Paleozoic complex of metadolerite and quartz porphyry dikes. Ore deposition was a long-term process comprising four stages. The first stage was related to deposition of slightly auriferous pyrite syngenetic to host rocks. The second stage is characterized by formation of the first productive (with invisible gold) fine acicular arsenopyrite mineralization accompanied by sericitization and localized in the tectonic zone. The stockwork ore with pocket–disseminated base metal mineralization and free microscopic native gold of the third stage is hosted in silicified rocks. The ore formation has been completed by quartz–stibnite veins superposed on all preceding types of mineralization.
The antimony mineralization at this deposit consists of nests and veinlets hosted in brecciated mineralized carbonaceous carbonate–terrigenous rocks and
metadolerite dikes and can be traced unchanged to depths of 500–600 m.
The Suzdal deposit is situated on the hanging-wall side of the Charsk–Gornostaev ophiolitic suture and near the intersection of two major tectonic structures: the northwest-trending Gornostaev fault system and the northeast-trending Suzdal fault zone. The Suzdal fault zone can be traced southeastwards from the Semeytau volcanic–plutonic complex. The geological succession comprises Early Carboniferous sedimentary and volcanogenic rocks, younger sedimentary cover, and magmatic rocks representing several tectonomagmatic episodes. Pre-Mesozoic magmatism includes gabbro, dolerite, andesitic dacite, granite, and granite porphyry, whereas the Early Mesozoic Semeytau volcanic–plutonic complex is characterised by a rhyolite–trachyrhyolite–trachybasalt association with monzonite, granite-porphyry, and granosyenite-porphyry intrusions. At the Suzdal deposit, widespread mafic and felsic dykes include metadolerite, granite porphyry, granosyenite porphyry, and quartz porphyry. This juxtaposition of sedimentary sequences, magmatic bodies, and intersecting fault systems provides the principal geological framework within which gold mineralisation and associated hydrothermal alteration developed.
The Suzdal orogenic gold deposit is situated in the northwestern part of the West Kalba gold belt in Eastern Kazakhstan and belongs to the type of stringer–disseminated mineralized zones hosted in the Lower Carboniferous black-shale volcanic–carbonate–terrigenous sequences. Mineralization is controlled by the NE-trending Suzdal Fault. Mineralization is superposed on the Late Paleozoic complex of metadolerite and quartz porphyry dikes. Ore deposition was a long-term process comprising four stages. The first stage was related to deposition of slightly auriferous pyrite syngenetic to host rocks. The second stage is characterized by formation of the first productive (with invisible gold) fine acicular arsenopyrite mineralization accompanied by sericitization and localized in the tectonic zone. The stockwork ore with pocket–disseminated base metal mineralization and free microscopic native gold of the third stage is hosted in silicified rocks. The ore formation has been completed by quartz–stibnite veins superposed on all preceding types of mineralization.
The antimony mineralization at this deposit consists of nests and veinlets hosted in brecciated mineralized carbonaceous carbonate–terrigenous rocks and
metadolerite dikes and can be traced unchanged to depths of 500–600 m.
The Suzdal deposit is situated on the hanging-wall side of the Charsk–Gornostaev ophiolitic suture and near the intersection of two major tectonic structures: the northwest-trending Gornostaev fault system and the northeast-trending Suzdal fault zone. The Suzdal fault zone can be traced southeastwards from the Semeytau volcanic–plutonic complex. The geological succession comprises Early Carboniferous sedimentary and volcanogenic rocks, younger sedimentary cover, and magmatic rocks representing several tectonomagmatic episodes. Pre-Mesozoic magmatism includes gabbro, dolerite, andesitic dacite, granite, and granite porphyry, whereas the Early Mesozoic Semeytau volcanic–plutonic complex is characterised by a rhyolite–trachyrhyolite–trachybasalt association with monzonite, granite-porphyry, and granosyenite-porphyry intrusions. At the Suzdal deposit, widespread mafic and felsic dykes include metadolerite, granite porphyry, granosyenite porphyry, and quartz porphyry. This juxtaposition of sedimentary sequences, magmatic bodies, and intersecting fault systems provides the principal geological framework within which gold mineralisation and associated hydrothermal alteration developed.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
32 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold var. Electrum | 1.AA.05 | (Au,Ag) |
| ⓘ | 1.AA.05 | Au | |
| ⓘ | Native Antimony | 1.CA.05 | Sb |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Nickeline | 2.CC.05 | NiAs |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Cinnabar | 2.CD.15a | HgS |
| ⓘ | Stibnite | 2.DB.05 | Sb2S3 |
| ⓘ | Aurostibite | 2.EB.05a | AuSb2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Marcasite | 2.EB.10a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | Ullmannite | 2.EB.25 | NiSbS |
| ⓘ | Willyamite | 2.EB.25 | CoSbS |
| ⓘ | Berthierite | 2.HA.20 | FeSb2S4 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Spinel | 4.BB.05 | MgAl2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| ⓘ | Goethite | 4.FD.10 | Fe3+O(OH) |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Siderite | 5.AB.05 | FeCO3 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| ⓘ | Scheelite | 7.GA.05 | Ca(WO4) |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Hydroxylapatite | 8.BN.05 | Ca5(PO4)3(OH) |
| ⓘ | Scorodite | 8.CD.10 | Fe3+AsO4 · 2H2O |
| Group 9 - Silicates | |||
| ⓘ | Tremolite | 9.DE.10 | ◻Ca2Mg5(Si8O22)(OH)2 |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Margarite | 9.EC.30 | CaAl2(Al2Si2O10)(OH)2 |
| ⓘ | Kaolinite | 9.ED.05 | Al2(Si2O5)(OH)4 |
| Unclassified | |||
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Lepidolite' ? | - | |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Monazite Group' | - | REE(PO4) |
| ⓘ | 'Wad' | - | |
| ⓘ | 'Chrome-Spinel (of Dana)' | - | |
| ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
| ⓘ | 'Apatite' | - | Ca5(PO4)3A |
| ⓘ | 'Tetrahedrite Group' | - | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| ⓘ | 'Hydromica' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Goethite | Fe3+O(OH) |
| H | ⓘ Hydroxylapatite | Ca5(PO4)3(OH) |
| H | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| H | ⓘ Margarite | CaAl2(Al2Si2O10)(OH)2 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Scorodite | Fe3+AsO4 · 2H2O |
| H | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Siderite | FeCO3 |
| O | Oxygen | |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Goethite | Fe3+O(OH) |
| O | ⓘ Hydroxylapatite | Ca5(PO4)3(OH) |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| O | ⓘ Margarite | CaAl2(Al2Si2O10)(OH)2 |
| O | ⓘ Monazite Group | REE(PO4) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Scheelite | Ca(WO4) |
| O | ⓘ Scorodite | Fe3+AsO4 · 2H2O |
| O | ⓘ Siderite | FeCO3 |
| O | ⓘ Spinel | MgAl2O4 |
| O | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Garnet Group | X3Z2(SiO4)3 |
| O | ⓘ Apatite | Ca5(PO4)3A |
| Mg | Magnesium | |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Mg | ⓘ Spinel | MgAl2O4 |
| Mg | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Al | Aluminium | |
| Al | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Al | ⓘ Margarite | CaAl2(Al2Si2O10)(OH)2 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Spinel | MgAl2O4 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Si | ⓘ Margarite | CaAl2(Al2Si2O10)(OH)2 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
| P | Phosphorus | |
| P | ⓘ Hydroxylapatite | Ca5(PO4)3(OH) |
| P | ⓘ Monazite Group | REE(PO4) |
| P | ⓘ Apatite | Ca5(PO4)3A |
| S | Sulfur | |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Berthierite | FeSb2S4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Cinnabar | HgS |
| S | ⓘ Galena | PbS |
| S | ⓘ Marcasite | FeS2 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Stibnite | Sb2S3 |
| S | ⓘ Ullmannite | NiSbS |
| S | ⓘ Willyamite | CoSbS |
| S | ⓘ Tetrahedrite Group | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| K | Potassium | |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Hydroxylapatite | Ca5(PO4)3(OH) |
| Ca | ⓘ Margarite | CaAl2(Al2Si2O10)(OH)2 |
| Ca | ⓘ Scheelite | Ca(WO4) |
| Ca | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Ca | ⓘ Apatite | Ca5(PO4)3A |
| Ti | Titanium | |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Ti | ⓘ Rutile | TiO2 |
| Fe | Iron | |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Berthierite | FeSb2S4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Goethite | Fe3+O(OH) |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Marcasite | FeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Scorodite | Fe3+AsO4 · 2H2O |
| Fe | ⓘ Siderite | FeCO3 |
| Co | Cobalt | |
| Co | ⓘ Willyamite | CoSbS |
| Ni | Nickel | |
| Ni | ⓘ Nickeline | NiAs |
| Ni | ⓘ Ullmannite | NiSbS |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| As | ⓘ Nickeline | NiAs |
| As | ⓘ Scorodite | Fe3+AsO4 · 2H2O |
| Ag | Silver | |
| Ag | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Sb | Antimony | |
| Sb | ⓘ Native Antimony | Sb |
| Sb | ⓘ Aurostibite | AuSb2 |
| Sb | ⓘ Berthierite | FeSb2S4 |
| Sb | ⓘ Stibnite | Sb2S3 |
| Sb | ⓘ Ullmannite | NiSbS |
| Sb | ⓘ Willyamite | CoSbS |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
| W | Tungsten | |
| W | ⓘ Scheelite | Ca(WO4) |
| Au | Gold | |
| Au | ⓘ Aurostibite | AuSb2 |
| Au | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Au | ⓘ Native Gold | Au |
| Hg | Mercury | |
| Hg | ⓘ Cinnabar | HgS |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
Other Regions, Features and Areas containing this locality
AsiaContinent
Eurasian PlateTectonic Plate
- Central Kazakhstan Folded RegionOrogenic Belt
- Irtysh-Zaisan Fold BeltOrogenic Belt
- Mohe BasinBasin
Soviet Union (1922-1991)Country
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References
Kovalev, K.R.; Kalinin, Y.A.; Naumov, E.A.; Pirajno, F.; Borisenko, A.S. (2009) A mineralogical study of the Suzdal sediment-hosted gold deposit, Eastern Kazakhstan: Implications for ore genesis. Ore Geology Reviews, 35 (2). doi:10.1016/j.oregeorev.2008.11.007
Kovalev, K. R., Kalinin, Yu. A., Polynov, V. I., Kydyrbekov, E. L., Borisenko, A. S., Naumov, E. A., Netesov, M. I., Klimenko, A. G., Kolesnikova, M. K. (2012) The Suzdal gold-sulfide deposit in the black shale of Eastern Kazakhstan. Geology of Ore Deposits, 54 (4) 254-275 doi:10.1134/s1075701512040034
[2]Kalinin, Yu. A., Naumov, E. A., Borisenko, A. S., Kovalev, K. R., Antropova, A. I. (2015) Spatial-temporal and genetic relationships between gold and antimony mineralization at gold-sulfide deposits of the Ob-Zaisan folded zone. Geology of Ore Deposits, 57 (3) 157-171 doi:10.1134/s1075701515030022
D’yachkov, Boris A., Bissatova, Ainel Y., Mizernaya, Marina A., Khromykh, Sergey V., Oitseva, Tatiana A., Kuzmina, Oxana N., Zimanovskaya, Natalya A., Aitbayeva, Saltanat S. (2021) Mineralogical Tracers of Gold and Rare-Metal Mineralization in Eastern Kazakhstan. Minerals, 11 (3) 253 doi:10.3390/min11030253
[1]Naumov, Evgeny, Kalinin, Yuri, Palyanova, Galina, Kryuchkova, Lyudmila, Voitenko, Viacheslav, Abramova, Vera, Pirajno, Franco (2025) Combined study of Au-bearing arsenopyrite of orogenic gold deposits (NE Asia): High resolution 3D X-ray computed tomography, LA-ICP-MS, and EMPA data. Geoscience Frontiers, 16 (1). doi:10.1016/j.gsf.2024.101953
[3]Agaliyeva, Bakytgul; Orazbekova, Gulizat; Apshikur, Baitak; Frolova, Olga; Mukyshev, Damir; Amralinova, Bakytzhan; Mataibaeva, Indira (2026) Integrated Remote Sensing and Geological Analysis for Delineating Prospective Gold-Mineralisation Zones at the Suzdal Deposit, Kazakhstan. Geosciences, 16 (10). doi:10.3390/geosciences16100412