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Zaozigou Au deposit, Hezuo Co., Gannan, Gansu, Chinai
| Regional Level Types | |
|---|---|
| Zaozigou Au deposit | Deposit |
| Hezuo Co. | County |
| Gannan | Prefecture |
| Gansu | Province |
| China | Country |
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Latitude & Longitude (WGS84):
34° 57' 56'' North , 102° 48' 41'' East
Latitude & Longitude (decimal):
Type:
Age:
238 ± 1.8 Ma
Geologic Time:
Dating method:
U-Pb zircons
Reference for age:
Qiu, K. F., Yu, H. C., Deng, J., McIntire, D., Gou, Z. Y., Geng, J. Z., ... & Goldfarb, R. (2020). The giant Zaozigou Au-Sb deposit in West Qinling, China: magmatic-or metamorphic-hydrothermal origin?. Mineralium Deposita, 1-18.
Köppen climate type:
Name(s) in local language(s):
枣子沟金矿 (早子沟金矿), 合作市, 甘南藏族自治州, 甘肃省, 中国
Disseminated-style (Carlin-like) gold deposit. Free gold occurs as microscopic grains (unlike a typical Carlin deposit, where visible gold is absent). Discovered in 1996. Annual production of 3t of gold per year with cumulative production of 26t.
There are 147 gold orebodies have been found in the Zaozigou gold deposit, of which 17 orebodies are main ore bodies with gold reserves greater than 1 tonne, and the total gold reserves of more than 100 tonnes.
The Zaozigou Au-Sb deposit, with proven reserves of 111 t Au and 0.05 Mt Sb, is located in the western portion of the West Qinling orogen. Ore bodies are mostly hosted in the Triassic Gulangdi Formation, which consists of argillaceous to siliceous slates and subordinate greywacke and limestone. The Zaozigou deposit includes 646 ore bodies, with the orebody Au-1 being the largest and having a proven reserve of 28.7 t Au. Gold mineralization is largely confined by brittle faults, and thus, individual ore bodies are exclusively of vein type.
The two Au mineralization events inferred by U-Pb dating of scheelite at the Zaozigou deposit are consistent with two episodes of Au mineralization in the West Qinling. The older mineralization event (ca. 230 Ma) recorded by scheelite from the steeply-dipping ore body at the Zaozigou deposit reflects a large-scale Au mineralization episode at 249–230 Ma in the West Qinling. The younger mineralization event (ca. 212 Ma) documented by scheelite from the gently dipping quartz-stibnite veins at the Zaozigou deposit reflects the orogenic Au mineralization period spanning from 210 to 195 Ma in the West Qinling.
A total of 523 individual ore bodies have been identified in the Zaozigou gold deposit, of which 18 are classified as major. Based on spatial distribution and structural style, the deposit is subdivided into three sectors: the Eastern, Western, and Gelouang sectors.
The Eastern Sector, the principal mineralized zone at Zaozigou deposit, trends NE (striking 50°–60°), hosting representative ore bodies such as Au1 and Au9. This zone extends for more than 1000 m along strike and exceeds 300 m in width. In shallow levels, the ore bodies dip steeply to the northwest and are locally subvertical, whereas at depth they are displaced by a gently dipping fault, resulting in an apparent southeastward dip. NE-trending veins in this sector are characterized by intense hydrothermal alteration and high gold grades. Both thickness and grade vary markedly along strike and down dip, and the veins commonly branch and merge, indicating a structurally complex mineralizing system. The Zaozigou deposit features four principal ore types: altered slate, altered vein, quartz-stibnite, and altered sandstone. The first two types predominantly occur in steeply dipping ore bodies trending nearly SN and NE, whereas the latter two are mainly hosted in gently dipping NW-trending structures.
The mineralization at Zaozigou can be divided into five paragenetic stages:
Silicification–hematitization stage, characterized by widespread hematitization and biotite alteration (representing potassic alteration).
Quartz–pyrite–arsenopyrite stage, with a mineral sequence of quartz → pyrite → arsenopyrite → gold, commonly associated with bleached alteration halos. This is the primary gold deposition stage.
Quartz–stibnite stage, with the mineral sequence quartz → pyrite → arsenopyrite → gold → stibnite, representing another major gold-forming event.
Quartz–carbonatization stage, characterized by the precipitation of quartz → calcite → kaolinite.
Surface oxidation stage, marked by the oxidation of metal sulfides at shallow depths and formation of limonite and stibiconite.
At Zaozigou, two styles of mineralization have been identified: early disseminated and stockwork ores, and late stibnite–quartz ± dolomite ± native gold veins within altered dacite and slate. In addition to native gold, stibnite is recovered as an ore mineral.
classified as an orogenic gold deposit.
There are 147 gold orebodies have been found in the Zaozigou gold deposit, of which 17 orebodies are main ore bodies with gold reserves greater than 1 tonne, and the total gold reserves of more than 100 tonnes.
The Zaozigou Au-Sb deposit, with proven reserves of 111 t Au and 0.05 Mt Sb, is located in the western portion of the West Qinling orogen. Ore bodies are mostly hosted in the Triassic Gulangdi Formation, which consists of argillaceous to siliceous slates and subordinate greywacke and limestone. The Zaozigou deposit includes 646 ore bodies, with the orebody Au-1 being the largest and having a proven reserve of 28.7 t Au. Gold mineralization is largely confined by brittle faults, and thus, individual ore bodies are exclusively of vein type.
The two Au mineralization events inferred by U-Pb dating of scheelite at the Zaozigou deposit are consistent with two episodes of Au mineralization in the West Qinling. The older mineralization event (ca. 230 Ma) recorded by scheelite from the steeply-dipping ore body at the Zaozigou deposit reflects a large-scale Au mineralization episode at 249–230 Ma in the West Qinling. The younger mineralization event (ca. 212 Ma) documented by scheelite from the gently dipping quartz-stibnite veins at the Zaozigou deposit reflects the orogenic Au mineralization period spanning from 210 to 195 Ma in the West Qinling.
A total of 523 individual ore bodies have been identified in the Zaozigou gold deposit, of which 18 are classified as major. Based on spatial distribution and structural style, the deposit is subdivided into three sectors: the Eastern, Western, and Gelouang sectors.
The Eastern Sector, the principal mineralized zone at Zaozigou deposit, trends NE (striking 50°–60°), hosting representative ore bodies such as Au1 and Au9. This zone extends for more than 1000 m along strike and exceeds 300 m in width. In shallow levels, the ore bodies dip steeply to the northwest and are locally subvertical, whereas at depth they are displaced by a gently dipping fault, resulting in an apparent southeastward dip. NE-trending veins in this sector are characterized by intense hydrothermal alteration and high gold grades. Both thickness and grade vary markedly along strike and down dip, and the veins commonly branch and merge, indicating a structurally complex mineralizing system. The Zaozigou deposit features four principal ore types: altered slate, altered vein, quartz-stibnite, and altered sandstone. The first two types predominantly occur in steeply dipping ore bodies trending nearly SN and NE, whereas the latter two are mainly hosted in gently dipping NW-trending structures.
The mineralization at Zaozigou can be divided into five paragenetic stages:
Silicification–hematitization stage, characterized by widespread hematitization and biotite alteration (representing potassic alteration).
Quartz–pyrite–arsenopyrite stage, with a mineral sequence of quartz → pyrite → arsenopyrite → gold, commonly associated with bleached alteration halos. This is the primary gold deposition stage.
Quartz–stibnite stage, with the mineral sequence quartz → pyrite → arsenopyrite → gold → stibnite, representing another major gold-forming event.
Quartz–carbonatization stage, characterized by the precipitation of quartz → calcite → kaolinite.
Surface oxidation stage, marked by the oxidation of metal sulfides at shallow depths and formation of limonite and stibiconite.
At Zaozigou, two styles of mineralization have been identified: early disseminated and stockwork ores, and late stibnite–quartz ± dolomite ± native gold veins within altered dacite and slate. In addition to native gold, stibnite is recovered as an ore mineral.
classified as an orogenic gold deposit.
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
29 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 | 1.AA.05 | Au |
| ⓘ | Native Antimony | 1.CA.05 | Sb |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Stibnite | 2.DB.05 | Sb2S3 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | var. Arsenic-bearing Pyrite | 2.EB.05a | Fe(S,As)2 |
| ⓘ | Marcasite | 2.EB.10a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Valentinite | 4.CB.55 | Sb2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| ⓘ | Tripuhyite | 4.DB.05 | Fe3+Sb5+O4 |
| ⓘ | Stibiconite | 4.DH.20 | Sb3+Sb5+2O6(OH) |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Ankerite | 5.AB.10 | Ca(Fe2+,Mg)(CO3)2 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| ⓘ | var. Iron-bearing Dolomite | 5.AB.10 | Ca(Mg,Fe)(CO3)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Scheelite | 7.GA.05 | Ca(WO4) |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Scorodite | 8.CD.10 | Fe3+AsO4 · 2H2O |
| Group 9 - Silicates | |||
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Titanite | 9.AG.15 | CaTiO(SiO4) |
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | 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 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Feldspar Group' | - | |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Monazite Group' | - | REE(PO4) |
| ⓘ | 'Hornblende Root Name Group' | - | ◻Ca2(C2+4C3+)(AlSi7O22)W2 |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Apatite' | - | Ca5(PO4)3A |
| ⓘ | 'Micrite' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Scorodite | Fe3+AsO4 · 2H2O |
| H | ⓘ Stibiconite | Sb3+Sb25+O6(OH) |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| 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 | ⓘ Stibiconite | Sb3+Sb25+O6(OH) |
| O | ⓘ Titanite | CaTiO(SiO4) |
| O | ⓘ Tripuhyite | Fe3+Sb5+O4 |
| O | ⓘ Valentinite | Sb2O3 |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| O | ⓘ Apatite | Ca5(PO4)3A |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)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 | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Mg | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Titanite | CaTiO(SiO4) |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| P | Phosphorus | |
| P | ⓘ Monazite Group | REE(PO4) |
| P | ⓘ Apatite | Ca5(PO4)3A |
| S | Sulfur | |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Chalcocite | Cu2S |
| S | ⓘ Covellite | CuS |
| S | ⓘ Galena | PbS |
| S | ⓘ Marcasite | FeS2 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Stibnite | Sb2S3 |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| S | ⓘ Pyrite var. Arsenic-bearing Pyrite | Fe(S,As)2 |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Scheelite | Ca(WO4) |
| Ca | ⓘ Titanite | CaTiO(SiO4) |
| Ca | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| Ca | ⓘ Apatite | Ca5(PO4)3A |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | ⓘ Rutile | TiO2 |
| Ti | ⓘ Titanite | CaTiO(SiO4) |
| Fe | Iron | |
| Fe | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Marcasite | FeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Scorodite | Fe3+AsO4 · 2H2O |
| Fe | ⓘ Tripuhyite | Fe3+Sb5+O4 |
| Fe | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| Fe | ⓘ Pyrite var. Arsenic-bearing Pyrite | Fe(S,As)2 |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chalcocite | Cu2S |
| Cu | ⓘ Covellite | CuS |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| As | ⓘ Scorodite | Fe3+AsO4 · 2H2O |
| As | ⓘ Pyrite var. Arsenic-bearing Pyrite | Fe(S,As)2 |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Sb | Antimony | |
| Sb | ⓘ Native Antimony | Sb |
| Sb | ⓘ Stibiconite | Sb3+Sb25+O6(OH) |
| Sb | ⓘ Stibnite | Sb2S3 |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Sb | ⓘ Tripuhyite | Fe3+Sb5+O4 |
| Sb | ⓘ Valentinite | Sb2O3 |
| W | Tungsten | |
| W | ⓘ Scheelite | Ca(WO4) |
| Au | Gold | |
| Au | ⓘ Native Gold | Au |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
Other Regions, Features and Areas containing this locality
AsiaContinent
- Hindukush Himalayan RegionGroup of Mountain Ranges
- Tibetan PlateauPlateau
China
- Qinghai
- East Kunlun Orogenic BeltMetamorphic belt
- Qinling Metallogenic BeltMineral Belt
Eurasian PlateTectonic Plate
- Kunlun/South Qilian Fold BeltVolcanic Arc
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References
Yu, Hao-Cheng, Guo, Chang-An, Qiu, Kun-Feng, McIntire, Duncan, Jiang, Gui-Peng, Gou, Zong-Yang, Geng, Jian-Zhen, Pang, Yao, Zhu, Rui, Li, Ning-Bo (2019) Geochronological and Geochemical Constraints on the Formation of the Giant Zaozigou Au-Sb Deposit, West Qinling, China. Minerals, 9 (1) 37 doi:10.3390/min9010037
Qiu, Kun-Feng; Yu, Hao-Cheng; Deng, Jun; McIntire, Duncan; Gou, Zong-Yang; Geng, Jian-Zhen; Chang, Zhao-Shan; Zhu, Rui; Li, Kang-Ning; Goldfarb, Richard (2020) The giant Zaozigou Au-Sb deposit in West Qinling, China: magmatic- or metamorphic-hydrothermal origin? Mineralium Deposita, 55 (2). 345-362 doi:10.1007/s00126-019-00937-w
Kong, Yunhui, Chen, Guodong, Liu, Bingli, Xie, Miao, Yu, Zhengbo, Li, Cheng, Wu, Yixiao, Gao, Yaxin, Zha, Shuai, Zhang, Hanyuan, Wang, Lu, Tang, Rui (2022) 3D Mineral Prospectivity Mapping of Zaozigou Gold Deposit, West Qinling, China: Machine Learning-Based Mineral Prediction. Minerals, 12 (11) 1361 doi:10.3390/min12111361
[1]Du, Shi-Guang, Tian, Xiang-Sheng, Ren, Zhe, Jin, Xiao-Ye, Tao, Huan, Luo, Tao, Zhu, Rui, Li, Jian-Wei, Deng, Xiao-Dong (2025) Laser ablation ICP-MS scheelite U-Pb dating constraints on two discrete gold mineralization events of the Zaozigou Au-Sb deposit, West Qinling orogen, China. Ore Geology Reviews, 176. 106437 doi:10.1016/j.oregeorev.2024.106437
[3]Li, Kangning; Gao, Shen; Tang, Qingyan; Zhao, Jichang; Hu, Hao; Liu, Jiajun; Zhai, Degao (2026) Source of giant Au-Sb mineralization in the Xiahe-Hezuo district, western Qinling: Constraints from Pb-S-Sb-Hg isotopes. Ore Geology Reviews, 198. p.107563. doi:10.1016/j.oregeorev.2026.107563
[2]Li, Kangning; Jia, Ruya; Tang, Qingyan; Xue, Jianling; He, Tongtong; Pang, Zhenshan; Cheng, Zhizhong; Yan, Tingjie (2026) Ore-forming age and temperature of the Zaozigou gold deposit, West Qinling Orogen: constraints from arsenopyrite Re-Os isotopes, mineral geochemistry, and fluid inclusion thermometry. Ore Geology Reviews, 193. p.107271. doi:10.1016/j.oregeorev.2026.107271