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Zhongshangou Mine, Dongping Au-Te ore field, Shuiquangou Complex, Chongli District, Zhangjiakou, Hebei, Chinai
| Regional Level Types | |
|---|---|
| Zhongshangou Mine | Mine |
| Dongping Au-Te ore field | Ore Field |
| Shuiquangou Complex | Complex |
| Chongli District | District |
| Zhangjiakou | Prefecture-level City |
| Hebei | Province |
| China | Country |
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Latitude & Longitude (WGS84):
40° 54' 12'' North , 115° 6' 10'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Zhangjiakou | 692,602 (2013) | 21.5km |
| Zhangjiakou Shi Xuanhua Qu | 373,422 (2015) | 33.0km |
Name(s) in local language(s):
中山沟金矿, 东坪金碲矿田, 崇礼县, 张家口市, 河北省, 中国
Alkaline igneous rock-hosted gold deposit.
Local geological units of the Zhongshangou mainly include the Devonian Shuiquangou intrusive complex and the Archean Sanggan Group. The Shuiquangou complex in the mining area mainly consists of hornblende monzogranite, pyroxene diorite, and syenite. Mineralization at Zhongshangou was strictly fault-controlled. Ore veins of the deposit mainly developed within the Shuiquangou alkaline complex. At present, more than 40 parallel ore-bearing veins have been identified, and two of them have been confirmed to be of economic significance. Vein No. 1 contains three orebodies, with the maximum ore grade of approximately 50 g/t Au. Vein No. 2, with a gold grade of > 1.6 g/t and a tellurium grade of > 0.5 g/t, is located to the east of Vein No. 1. Individual ore bodies from the two veins generally have a length of < 300 m and a thickness of < 3 m. Three ore types are identified by our and previous researches: the potassic alteration-type ores, auriferous quartz vein-type ores, and breccia-type ores. Three stages of ore deposition: (1) Pre-ore stage. This stage represents an initial potassium stage in which K-feldspar, magnetite, specularite, pyrite, and milky quartz are developed. Pyrite grains are generally coarse and euhedral to subhedral in shape. (2) Main-ore stage. This stage contains abundant sulfides, tellurides, and visible gold. Sulfide minerals are widely developed in this stage. Au- and Te-bearing minerals, which mostly occur as fine mineral inclusions within sulfides, coexist in this stage. Tellurides from this stage are dominated by hessite, altaite, and petzite. (3) Post-ore stage. The ore-barren calcite veins are the result of later hydrothermal activities and they are not major contributors to the Au-Te mineralization.
Magmatic rocks are dominated by the Shuiquangou complex. The intrusive body in the mining district covers an exposed area of about 9 km2 and occurs as a deep-seated composite batholith. It is in intrusive contact with the metamorphic rocks of the Sanggan Group Jiangouhe Formation in the Muchanggou area. The monzonitic complex is the immediate ore-hosting wall rock and is closely related to mineralization. It has been modified by later tectonic and hydrothermal processes to form different types of altered rocks. Dikes in the district are controlled by faults and mainly consist of monzonite, syenite, K-feldspar pegmatite, and diabase, among which K-feldspar pegmatite and fine-grained quartz monzonite are most developed. Wall-rock alterations mainly include K-feldspathization, silicification, sericitization, kaolinization, and carbonatization.
Local geological units of the Zhongshangou mainly include the Devonian Shuiquangou intrusive complex and the Archean Sanggan Group. The Shuiquangou complex in the mining area mainly consists of hornblende monzogranite, pyroxene diorite, and syenite. Mineralization at Zhongshangou was strictly fault-controlled. Ore veins of the deposit mainly developed within the Shuiquangou alkaline complex. At present, more than 40 parallel ore-bearing veins have been identified, and two of them have been confirmed to be of economic significance. Vein No. 1 contains three orebodies, with the maximum ore grade of approximately 50 g/t Au. Vein No. 2, with a gold grade of > 1.6 g/t and a tellurium grade of > 0.5 g/t, is located to the east of Vein No. 1. Individual ore bodies from the two veins generally have a length of < 300 m and a thickness of < 3 m. Three ore types are identified by our and previous researches: the potassic alteration-type ores, auriferous quartz vein-type ores, and breccia-type ores. Three stages of ore deposition: (1) Pre-ore stage. This stage represents an initial potassium stage in which K-feldspar, magnetite, specularite, pyrite, and milky quartz are developed. Pyrite grains are generally coarse and euhedral to subhedral in shape. (2) Main-ore stage. This stage contains abundant sulfides, tellurides, and visible gold. Sulfide minerals are widely developed in this stage. Au- and Te-bearing minerals, which mostly occur as fine mineral inclusions within sulfides, coexist in this stage. Tellurides from this stage are dominated by hessite, altaite, and petzite. (3) Post-ore stage. The ore-barren calcite veins are the result of later hydrothermal activities and they are not major contributors to the Au-Te mineralization.
Magmatic rocks are dominated by the Shuiquangou complex. The intrusive body in the mining district covers an exposed area of about 9 km2 and occurs as a deep-seated composite batholith. It is in intrusive contact with the metamorphic rocks of the Sanggan Group Jiangouhe Formation in the Muchanggou area. The monzonitic complex is the immediate ore-hosting wall rock and is closely related to mineralization. It has been modified by later tectonic and hydrothermal processes to form different types of altered rocks. Dikes in the district are controlled by faults and mainly consist of monzonite, syenite, K-feldspar pegmatite, and diabase, among which K-feldspar pegmatite and fine-grained quartz monzonite are most developed. Wall-rock alterations mainly include K-feldspathization, silicification, sericitization, kaolinization, and carbonatization.
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
40 valid minerals. 1 (TL) - type locality of 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 Silver | 1.AA.05 | Ag |
| ⓘ | var. Küstelite | 1.AA.05 | Ag |
| ⓘ | Native Bismuth | 1.CA.05 | Bi |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Cervelleite | 2.BA.60 | Ag4TeS |
| ⓘ | Hessite | 2.BA.60 | Ag2Te |
| ⓘ | Petzite | 2.BA.75 | Ag3AuTe2 |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Altaite | 2.CD.10 | PbTe |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Bismuthinite | 2.DB.05 | Bi2S3 |
| ⓘ | Tellurobismuthite | 2.DC.05 | Bi2Te3 |
| ⓘ | Tetradymite | 2.DC.05 | Bi2Te2S |
| ⓘ | Calaverite | 2.EA.10 | AuTe2 |
| ⓘ | Molybdenite | 2.EA.30 | MoS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | 'Tennantite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)As4S12S |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| ⓘ | Tennantite-(Zn) | 2.GB.05 | Cu6(Cu4Zn2)As4S12S |
| ⓘ | Tetrahedrite-(Zn) | 2.GB.05 | Cu6(Cu4Zn2)Sb4S12S |
| Group 3 - Halides | |||
| ⓘ | Fluorite | 3.AB.25 | CaF2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | var. Specularite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz var. Chalcedony | 4.DA.05 | SiO2 |
| ⓘ | 4.DA.05 | SiO2 | |
| ⓘ | var. Smoky Quartz | 4.DA.05 | SiO2 |
| ⓘ | var. Milky Quartz | 4.DA.05 | SiO2 |
| ⓘ | Pyrolusite | 4.DB.05 | Mn4+O2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| ⓘ | Anatase | 4.DD.05 | TiO2 |
| ⓘ | Zincospiroffite (TL) | 4.JK.10 | Zn2Te4+3O8 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Ankerite | 5.AB.10 | Ca(Fe2+,Mg)(CO3)2 |
| ⓘ | Cerussite | 5.AB.15 | PbCO3 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Anglesite | 7.AD.35 | PbSO4 |
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| Group 9 - Silicates | |||
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Kaolinite | 9.ED.05 | Al2(Si2O5)(OH)4 |
| ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Orthoclase | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5(T8O22)W2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Feldspar Group' | - | |
| ⓘ | 'Calcium Amphibole Subgroup var. Hornblende' | - | AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'K Feldspar' | - | |
| ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
| ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
| ⓘ | 'Apatite' | - | Ca5(PO4)3A |
| ⓘ | 'Tetrahedrite Group' | - | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| ⓘ | 'Calcium Amphibole Subgroup' | - | AnCa2(C2+5-mC3+m)(Si8-(n+m)Al(n+m))W2 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| H | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Cerussite | PbCO3 |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Amphibole Supergroup | AB2C5(T8O22)W2 |
| O | ⓘ Anatase | TiO2 |
| O | ⓘ Anglesite | PbSO4 |
| O | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Cerussite | PbCO3 |
| O | ⓘ Quartz var. Chalcedony | SiO2 |
| O | ⓘ Diopside | CaMgSi2O6 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| O | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Microcline | K(AlSi3O8) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Orthoclase | K(AlSi3O8) |
| O | ⓘ Pyrolusite | Mn4+O2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Quartz var. Smoky Quartz | SiO2 |
| O | ⓘ Hematite var. Specularite | Fe2O3 |
| O | ⓘ Quartz var. Milky Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Pyroxene Group | ADSi2O6 |
| O | ⓘ Garnet Group | X3Z2(SiO4)3 |
| O | ⓘ Zincospiroffite | Zn2Te34+O8 |
| O | ⓘ Apatite | Ca5(PO4)3A |
| F | Fluorine | |
| F | ⓘ Fluorite | CaF2 |
| F | ⓘ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Mg | ⓘ Diopside | CaMgSi2O6 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Al | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Al | ⓘ Microcline | K(AlSi3O8) |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Orthoclase | K(AlSi3O8) |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Al | ⓘ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Quartz var. Chalcedony | SiO2 |
| Si | ⓘ Diopside | CaMgSi2O6 |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Si | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Si | ⓘ Microcline | K(AlSi3O8) |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Orthoclase | K(AlSi3O8) |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Quartz var. Smoky Quartz | SiO2 |
| Si | ⓘ Quartz var. Milky Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | ⓘ Pyroxene Group | ADSi2O6 |
| Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
| Si | ⓘ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| P | Phosphorus | |
| P | ⓘ Apatite | Ca5(PO4)3A |
| S | Sulfur | |
| S | ⓘ Anglesite | PbSO4 |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Bismuthinite | Bi2S3 |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Cervelleite | Ag4TeS |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Covellite | CuS |
| S | ⓘ Galena | PbS |
| S | ⓘ Molybdenite | MoS2 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| S | ⓘ Tetradymite | Bi2Te2S |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| S | ⓘ Tetrahedrite Group | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| S | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| S | ⓘ Tetrahedrite-(Zn) | Cu6(Cu4Zn2)Sb4S12S |
| Cl | Chlorine | |
| Cl | ⓘ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| K | Potassium | |
| K | ⓘ Microcline | K(AlSi3O8) |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Orthoclase | K(AlSi3O8) |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Diopside | CaMgSi2O6 |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Fluorite | CaF2 |
| Ca | ⓘ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | ⓘ Apatite | Ca5(PO4)3A |
| Ca | ⓘ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Ti | Titanium | |
| Ti | ⓘ Anatase | TiO2 |
| Ti | ⓘ Rutile | TiO2 |
| Mn | Manganese | |
| Mn | ⓘ Pyrolusite | Mn4+O2 |
| Fe | Iron | |
| Fe | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Hematite var. Specularite | Fe2O3 |
| Cu | Copper | |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Covellite | CuS |
| Cu | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Cu | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| Cu | ⓘ Tetrahedrite-(Zn) | Cu6(Cu4Zn2)Sb4S12S |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| Zn | ⓘ Zincospiroffite | Zn2Te34+O8 |
| Zn | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| Zn | ⓘ Tetrahedrite-(Zn) | Cu6(Cu4Zn2)Sb4S12S |
| As | Arsenic | |
| As | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| As | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| Mo | Molybdenum | |
| Mo | ⓘ Molybdenite | MoS2 |
| Ag | Silver | |
| Ag | ⓘ Cervelleite | Ag4TeS |
| Ag | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Ag | ⓘ Hessite | Ag2Te |
| Ag | ⓘ Petzite | Ag3AuTe2 |
| Ag | ⓘ Native Silver | Ag |
| Ag | ⓘ Native Silver var. Küstelite | Ag |
| Sb | Antimony | |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Sb | ⓘ Tetrahedrite-(Zn) | Cu6(Cu4Zn2)Sb4S12S |
| Te | Tellurium | |
| Te | ⓘ Altaite | PbTe |
| Te | ⓘ Calaverite | AuTe2 |
| Te | ⓘ Cervelleite | Ag4TeS |
| Te | ⓘ Hessite | Ag2Te |
| Te | ⓘ Petzite | Ag3AuTe2 |
| Te | ⓘ Tellurobismuthite | Bi2Te3 |
| Te | ⓘ Tetradymite | Bi2Te2S |
| Te | ⓘ Zincospiroffite | Zn2Te34+O8 |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
| Au | Gold | |
| Au | ⓘ Calaverite | AuTe2 |
| Au | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Au | ⓘ Native Gold | Au |
| Au | ⓘ Petzite | Ag3AuTe2 |
| Pb | Lead | |
| Pb | ⓘ Altaite | PbTe |
| Pb | ⓘ Anglesite | PbSO4 |
| Pb | ⓘ Cerussite | PbCO3 |
| Pb | ⓘ Galena | PbS |
| Bi | Bismuth | |
| Bi | ⓘ Native Bismuth | Bi |
| Bi | ⓘ Bismuthinite | Bi2S3 |
| Bi | ⓘ Tellurobismuthite | Bi2Te3 |
| Bi | ⓘ Tetradymite | Bi2Te2S |
Geochronology
Mineralization age: Middle Triassic : 241 MaImportant note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.
| Geologic Time | Rocks, Minerals and Events | ||||||
|---|---|---|---|---|---|---|---|
| Phanerozoic | |||||||
| Mesozoic | |||||||
| Triassic | |||||||
| Middle Triassic |
| ||||||
Other Regions, Features and Areas containing this locality
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References
Hart, Craig J., Goldfarb, Richard J., Qiu, Yumin, Snee, Lawrence, Miller, Lance D., Miller, Marti L. (2002) Gold deposits of the northern margin of the North China Craton: multiple late Paleozoic–Mesozoic mineralizing events. Mineralium Deposita, 37 (3) 326-351 doi:10.1007/s00126-001-0239-2
[1]Wang, Chengyang; Chen, Wei; Jiajia Yu; Zhao, Junkang (2025) Geological characteristics, fluid inclusion, and isotope systematics of the Zhongshangou gold deposit, northern margin of the North China Craton: A comparative study with the Dongping deposit and implications for regional mineralization. Ore Geology Reviews, 182. 106629 doi:10.1016/j.oregeorev.2025.106629
[2]Zhen, Shimin; Wang, Dazhao; Zhang, Yangyang; Zha, Zhongjian; Bai, Haijun; Wang, Jiang; Wang, Chunnv; Xing, Wanli; Liu, Jiajun (2026) Ore-forming mechanism of the Zhongshangou tellurium-rich gold deposit, Zhangjiakou goldfield, North China: Insights from pyrite textures and trace element compositions. Ore Geology Reviews, p.107579. doi:10.1016/j.oregeorev.2026.107579