Lizi Au deposit, Qinzhou District, Tianshui, Gansu, Chinai
| Regional Level Types | |
|---|---|
| Lizi Au deposit | Deposit |
| Qinzhou District | District |
| Tianshui | Prefecture-level City |
| Gansu | Province |
| China | Country |
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Latitude & Longitude (WGS84):
34° 12' 15'' North , 105° 55' 29'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Other/historical names associated with this locality:
Liziyuan Au deposit; Liziyuan gold deposit
Name(s) in local language(s):
李子金矿床, 秦州区, 天水市, 甘肃省, 中国
Altered rock and quartz vein-type gold mineralizations, occurring in amphibolite schists and Indosinian intrusive rocks along a fracture zone. The deposit is worked by three small mines, each of which is centered on particular lithologies and mineralization styles.
The Lizi Gold Deposit is situated in Tianshui City, Gansu Province, People's Republic of China. The exposed strata in the mining area consist predominantly of greenschist-facies metasedimentary and metavolcanic rocks of the Ordovician Liziyuan Group, with minor occurrences of Precambrian Qinling Group migmatite. Magmatic rocks are extensively exposed in the mining district, primarily comprising three porphyry groups and the Tianzishan monzogranite. Among these, the Tianzishan monzogranite represents the largest intrusive body, with a previously reported crystallization age of 236.1 ± 1.9 Ma. The Lizi gold deposit consists of five mining segments: Shenjiagou, Kuangou, Jiancaowan, Liushagou, and Suishizi. The Shenjiagou, Kuangou, Jiancaowan, and Liushagou segments are hosted in schists of the Liziyuan Group and are controlled by NW-trending ductile–brittle shear zones, occurring as parallel lenses and veins. In contrast, the Suishizi gold deposit is hosted within the Tianzishan monzogranite and is controlled by diorite porphyry dikes and NE-trending faults. The goldfield has cumulative proven reserves exceeding 50 tonnes, with an average grade of 10 g/t.
The mineralization process of the Lizi gold deposit is divided into four stages:
(1) Stage I: Quartz-Sericite-Pyrite Stage. This stage is characterized by milky white quartz veins developed within the Liziyuan Group strata, sharp contacts with the host rocks. The alteration assemblage is dominated by sericitization and silicification.
(2) Stage Ⅱ: Pyrite-Gold Stage. Gold-bearing pyrite-pyrrhotite veins crosscut the Stage I quartz veins, with irregular boundaries, and common branching and rejoining. The alteration assemblage consists of chloritization, epidotization, albitization, and pyritization. Native gold occurs mainly in fractures or as inclusions within pyrite, pyrrhotite, galena, tetrahedrite, and quartz. Te–Bi minerals are closely associated with gold.
(3) Stage Ⅲ: Chalcopyrite-Gold Stage. Chalcopyrite-native gold veins crosscut or envelop Stage Ⅱ veins. The alteration assemblage is characterized by carbonatization, and magnetite–hematite alteration. Native gold is found in association with chalcopyrite, galena, galenobismutite, magnetite, and hematite within fractures of pyrite and quartz.
(4) Stage IV: Quartz-Calcite Stage. Quartz-calcite veinlets crosscut veins from the previous three stages. They are either devoid of sulfides or contain minor pyrite, marking the termination of mineralization.
Yuzigou, Liushagou, Jiancaowan, Kuangou, Suishizi, and Yingfang mining camps.
The Liziyuan Au deposit is a typical example hosted in brittle to ductile shear zones developed in greenschist-facies metasedimentary volcanic rocks and Triassic intrusions. The deposit contains three main sections at Shenjiagou, Suishizi, and Jiancaowan.
The Lizi Gold Deposit is situated in Tianshui City, Gansu Province, People's Republic of China. The exposed strata in the mining area consist predominantly of greenschist-facies metasedimentary and metavolcanic rocks of the Ordovician Liziyuan Group, with minor occurrences of Precambrian Qinling Group migmatite. Magmatic rocks are extensively exposed in the mining district, primarily comprising three porphyry groups and the Tianzishan monzogranite. Among these, the Tianzishan monzogranite represents the largest intrusive body, with a previously reported crystallization age of 236.1 ± 1.9 Ma. The Lizi gold deposit consists of five mining segments: Shenjiagou, Kuangou, Jiancaowan, Liushagou, and Suishizi. The Shenjiagou, Kuangou, Jiancaowan, and Liushagou segments are hosted in schists of the Liziyuan Group and are controlled by NW-trending ductile–brittle shear zones, occurring as parallel lenses and veins. In contrast, the Suishizi gold deposit is hosted within the Tianzishan monzogranite and is controlled by diorite porphyry dikes and NE-trending faults. The goldfield has cumulative proven reserves exceeding 50 tonnes, with an average grade of 10 g/t.
The mineralization process of the Lizi gold deposit is divided into four stages:
(1) Stage I: Quartz-Sericite-Pyrite Stage. This stage is characterized by milky white quartz veins developed within the Liziyuan Group strata, sharp contacts with the host rocks. The alteration assemblage is dominated by sericitization and silicification.
(2) Stage Ⅱ: Pyrite-Gold Stage. Gold-bearing pyrite-pyrrhotite veins crosscut the Stage I quartz veins, with irregular boundaries, and common branching and rejoining. The alteration assemblage consists of chloritization, epidotization, albitization, and pyritization. Native gold occurs mainly in fractures or as inclusions within pyrite, pyrrhotite, galena, tetrahedrite, and quartz. Te–Bi minerals are closely associated with gold.
(3) Stage Ⅲ: Chalcopyrite-Gold Stage. Chalcopyrite-native gold veins crosscut or envelop Stage Ⅱ veins. The alteration assemblage is characterized by carbonatization, and magnetite–hematite alteration. Native gold is found in association with chalcopyrite, galena, galenobismutite, magnetite, and hematite within fractures of pyrite and quartz.
(4) Stage IV: Quartz-Calcite Stage. Quartz-calcite veinlets crosscut veins from the previous three stages. They are either devoid of sulfides or contain minor pyrite, marking the termination of mineralization.
Yuzigou, Liushagou, Jiancaowan, Kuangou, Suishizi, and Yingfang mining camps.
The Liziyuan Au deposit is a typical example hosted in brittle to ductile shear zones developed in greenschist-facies metasedimentary volcanic rocks and Triassic intrusions. The deposit contains three main sections at Shenjiagou, Suishizi, and Jiancaowan.
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Rock Types Recorded
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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 | |||
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Digenite | 2.BA.10 | Cu9S5 |
| ⓘ | Acanthite | 2.BA.35 | Ag2S |
| ⓘ | 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 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Altaite | 2.CD.10 | PbTe |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Bismuthinite | 2.DB.05 | Bi2S3 |
| ⓘ | Tellurobismuthite | 2.DC.05 | Bi2Te3 |
| ⓘ | Molybdenite | 2.EA.30 | MoS2 |
| ⓘ | Pyrite var. Gold-bearing Pyrite | 2.EB.05a | FeS2 |
| ⓘ | 2.EB.05a | FeS2 | |
| ⓘ | Marcasite | 2.EB.10a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | 'Tennantite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)As4S12S |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| ⓘ | 'var. Silver-bearing Tetrahedrite' | 2.GB.05 | (Cu,Ag)6[Cu4(Fe,Zn)2]Sb4S13 |
| ⓘ | Chalcostibite | 2.HA.05 | CuSbS2 |
| ⓘ | Galenobismutite | 2.JB.25e | PbBi2S4 |
| ⓘ | Lillianite | 2.JB.40a | Pb3-2xAgxBi2+xS6 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| 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) |
| ⓘ | Actinolite | 9.DE.10 | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| ⓘ | 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 | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5(T8O22)W2 |
| ⓘ | 'Beegerite' | - | Pb6Bi2S9 |
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Hornblende Root Name Group' | - | ◻Ca2(C2+4C3+)(AlSi7O22)W2 |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'K Feldspar' | - | |
| ⓘ | 'Apatite' | - | Ca5(PO4)3A |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| 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 | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Amphibole Supergroup | AB2C5(T8O22)W2 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Titanite | CaTiO(SiO4) |
| 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 | ⓘ 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 | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)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 | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| 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 | ⓘ Apatite | Ca5(PO4)3A |
| S | Sulfur | |
| S | ⓘ Acanthite | Ag2S |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Pyrite var. Gold-bearing Pyrite | FeS2 |
| S | ⓘ Beegerite | Pb6Bi2S9 |
| S | ⓘ Bismuthinite | Bi2S3 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Chalcocite | Cu2S |
| S | ⓘ Chalcostibite | CuSbS2 |
| S | ⓘ Covellite | CuS |
| S | ⓘ Digenite | Cu9S5 |
| S | ⓘ Galena | PbS |
| S | ⓘ Galenobismutite | PbBi2S4 |
| S | ⓘ Lillianite | Pb3-2xAgxBi2+xS6 |
| S | ⓘ Marcasite | FeS2 |
| S | ⓘ Molybdenite | MoS2 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| S | ⓘ Tetrahedrite Subgroup var. Silver-bearing Tetrahedrite | (Cu,Ag)6[Cu4(Fe,Zn)2]Sb4S13 |
| 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 | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Titanite | CaTiO(SiO4) |
| Ca | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| 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 | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Pyrite var. Gold-bearing Pyrite | FeS2 |
| 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 | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Marcasite | FeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Tetrahedrite Subgroup var. Silver-bearing Tetrahedrite | (Cu,Ag)6[Cu4(Fe,Zn)2]Sb4S13 |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chalcocite | Cu2S |
| Cu | ⓘ Chalcostibite | CuSbS2 |
| Cu | ⓘ Covellite | CuS |
| Cu | ⓘ Digenite | Cu9S5 |
| Cu | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Cu | ⓘ Tetrahedrite Subgroup var. Silver-bearing Tetrahedrite | (Cu,Ag)6[Cu4(Fe,Zn)2]Sb4S13 |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| Zn | ⓘ Tetrahedrite Subgroup var. Silver-bearing Tetrahedrite | (Cu,Ag)6[Cu4(Fe,Zn)2]Sb4S13 |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| As | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Mo | Molybdenum | |
| Mo | ⓘ Molybdenite | MoS2 |
| Ag | Silver | |
| Ag | ⓘ Acanthite | Ag2S |
| Ag | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Ag | ⓘ Hessite | Ag2Te |
| Ag | ⓘ Lillianite | Pb3-2xAgxBi2+xS6 |
| Ag | ⓘ Petzite | Ag3AuTe2 |
| Ag | ⓘ Native Silver | Ag |
| Ag | ⓘ Tetrahedrite Subgroup var. Silver-bearing Tetrahedrite | (Cu,Ag)6[Cu4(Fe,Zn)2]Sb4S13 |
| Ag | ⓘ Native Silver var. Küstelite | Ag |
| Sb | Antimony | |
| Sb | ⓘ Chalcostibite | CuSbS2 |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Sb | ⓘ Tetrahedrite Subgroup var. Silver-bearing Tetrahedrite | (Cu,Ag)6[Cu4(Fe,Zn)2]Sb4S13 |
| Te | Tellurium | |
| Te | ⓘ Altaite | PbTe |
| Te | ⓘ Hessite | Ag2Te |
| Te | ⓘ Petzite | Ag3AuTe2 |
| Te | ⓘ Tellurobismuthite | Bi2Te3 |
| Au | Gold | |
| Au | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Au | ⓘ Native Gold | Au |
| Au | ⓘ Petzite | Ag3AuTe2 |
| Pb | Lead | |
| Pb | ⓘ Altaite | PbTe |
| Pb | ⓘ Beegerite | Pb6Bi2S9 |
| Pb | ⓘ Galena | PbS |
| Pb | ⓘ Galenobismutite | PbBi2S4 |
| Pb | ⓘ Lillianite | Pb3-2xAgxBi2+xS6 |
| Bi | Bismuth | |
| Bi | ⓘ Beegerite | Pb6Bi2S9 |
| Bi | ⓘ Native Bismuth | Bi |
| Bi | ⓘ Bismuthinite | Bi2S3 |
| Bi | ⓘ Galenobismutite | PbBi2S4 |
| Bi | ⓘ Lillianite | Pb3-2xAgxBi2+xS6 |
| Bi | ⓘ Tellurobismuthite | Bi2Te3 |
Localities in this Region
- Gansu
- Tianshui
- Qinzhou District
- Tianshui
Other Regions, Features and Areas containing this locality
AsiaContinent
- Hindukush Himalayan RegionGroup of Mountain Ranges
China
- Qinling Metallogenic BeltMineral Belt
Eurasian PlateTectonic Plate
- Kunlun/South Qilian Fold BeltVolcanic Arc
- North China CratonOrogen
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References
He, Chong-Guo; Li, Jian-Wei; Zu, Bo; Liu, Wen-Jiang; Qiu, Hua-Ning; Bai, Xiu-Juan (2021) Sericite 40Ar/39Ar and zircon U-Pb dating of the Liziyuan gold deposit, West Qinling orogen, central China: Implications for ore genesis and tectonic setting. Ore Geology Reviews, 139. 104531 doi:10.1016/j.oregeorev.2021.104531
Wang, Shuo, Liu, Zhanjin, Liu, Yunhua, Deng, Nan, Yang, Benzhao, Tan, Le (2023) Contribution of Triassic Tectonomagmatic Activity to the Mineralization of Liziyuan Orogenic Gold Deposits, West Qinling Orogenic Belt, China. Minerals, 13 (1) 130 doi:10.3390/min13010130
[1]Jin, Kailai; Wang, Yunfeng; Feng, Bo; Gu, Shangyi; Duan, Liuan; Fu, Yong; Chen, Yuanlin (2026) Genesis of the Lizi gold deposit in the western Qinling Orogen, China: Insights from in situ U-Pb dating of rutile, trace elements of pyrite, and S-Pb isotopes. Ore Geology Reviews, p.107392. doi:10.1016/j.oregeorev.2026.107392