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Liwu Cu-Zn deposit, Jiulong County, Garzê Autonomous Prefecture (Ganzi Autonomous Prefecture), Sichuan, Chinai
| Regional Level Types | |
|---|---|
| Liwu Cu-Zn deposit | Deposit |
| Jiulong County | County |
| Garzê Autonomous Prefecture (Ganzi Autonomous Prefecture) | Prefecture |
| Sichuan | Province |
| China | Country |
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Latitude & Longitude (WGS84):
28° 29' 38'' North , 101° 41' 20'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Name(s) in local language(s):
里伍铜矿, 九龙县, 甘孜藏族自治州, 四川省, 中国
VHMS-type copper-zinc deposit.
The exposed strata in the mining area are dominated by the Mesoproterozoic Liwu Group, with minor occurrences of Cenozoic unconsolidated deposits. The Liwu Group represents the main ore-hosting formation. Based on lithological assemblages, it is subdivided into the middle member (Pt1L2) and the upper member (Pt1L3), among which the third lithologic unit of the middle member constitutes the principal ore-bearing horizon. The mineralization type in the study area is mainly structural–hydrothermal filling and metasomatism, characterized by multi-stage and multi-genetic processes, and generally belongs to a medium- to high-temperature hydrothermal system. Mineralization is closely associated with wall-rock alteration, including biotitization, silicification, albitization, chloritization, garnetization, tourmalinization, and sericitization.
The ore bodies in the Heiniudong mining area occur within a structural–stratigraphic unit dominated by quartz schist and quartzite. The ore-bearing zone is located below the staurolite zone within the garnet (coarse-grained) contact metamorphic zone. A total of four economically significant ore bodies have been identified in the Heiniudong mining area, namely II4, I3, I1, and III1 from top to bottom, while the others are striped and disseminated occurrences located above and below the main ore bodies. Ore body II4 is distributed parallel above ore body I3 and is a concealed ore body, with a vertical spacing of generally 40–60 m. The ore body is mostly stratiform, striking northwest and dipping southwest, with dip angles ranging from 30° to 35°. The measured extension along dip is 250 m, and along strike is 150 m, with measured elevations ranging from 3320 m to 3450 m. The copper grades range from 0.41% to 0.83%, with an average of 0.62%, and the zinc grades range from 0.47% to 9.96%, with an average of 1.38%.
The deposit contains more than 0.8 ×106 t of Cu, 0.5 ×106 t of Zn, 133 t of Ag and 1300 t of Co. The deposit has an average Cu grade of 0.51%–2.50%, an average Zn grade of 0.29%–1.64%, an average Ag grade of 10×10−6–46×10−6 and an average Co grade of more than 0.01%. The Liwu copper-rich deposit is composed of several ore blocks, such as Liwu, Heiniudong, Zhongzui, Wajingou, Baixianglin and Sunyelin, which are produced around the Mesoproterozoic dome structure and their distribution is controlled by the dome structure.
The exposed strata in the mining area are dominated by the Mesoproterozoic Liwu Group, with minor occurrences of Cenozoic unconsolidated deposits. The Liwu Group represents the main ore-hosting formation. Based on lithological assemblages, it is subdivided into the middle member (Pt1L2) and the upper member (Pt1L3), among which the third lithologic unit of the middle member constitutes the principal ore-bearing horizon. The mineralization type in the study area is mainly structural–hydrothermal filling and metasomatism, characterized by multi-stage and multi-genetic processes, and generally belongs to a medium- to high-temperature hydrothermal system. Mineralization is closely associated with wall-rock alteration, including biotitization, silicification, albitization, chloritization, garnetization, tourmalinization, and sericitization.
The ore bodies in the Heiniudong mining area occur within a structural–stratigraphic unit dominated by quartz schist and quartzite. The ore-bearing zone is located below the staurolite zone within the garnet (coarse-grained) contact metamorphic zone. A total of four economically significant ore bodies have been identified in the Heiniudong mining area, namely II4, I3, I1, and III1 from top to bottom, while the others are striped and disseminated occurrences located above and below the main ore bodies. Ore body II4 is distributed parallel above ore body I3 and is a concealed ore body, with a vertical spacing of generally 40–60 m. The ore body is mostly stratiform, striking northwest and dipping southwest, with dip angles ranging from 30° to 35°. The measured extension along dip is 250 m, and along strike is 150 m, with measured elevations ranging from 3320 m to 3450 m. The copper grades range from 0.41% to 0.83%, with an average of 0.62%, and the zinc grades range from 0.47% to 9.96%, with an average of 1.38%.
The deposit contains more than 0.8 ×106 t of Cu, 0.5 ×106 t of Zn, 133 t of Ag and 1300 t of Co. The deposit has an average Cu grade of 0.51%–2.50%, an average Zn grade of 0.29%–1.64%, an average Ag grade of 10×10−6–46×10−6 and an average Co grade of more than 0.01%. The Liwu copper-rich deposit is composed of several ore blocks, such as Liwu, Heiniudong, Zhongzui, Wajingou, Baixianglin and Sunyelin, which are produced around the Mesoproterozoic dome structure and their distribution is controlled by the dome structure.
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
26 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 Bismuth | 1.CA.05 | Bi |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Dyscrasite | 2.AA.35 | Ag3Sb |
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Stannite | 2.CB.15a | Cu2FeSnS4 |
| ⓘ | Cubanite | 2.CB.55a | CuFe2S3 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Bismuthinite | 2.DB.05 | Bi2S3 |
| ⓘ | Guanajuatite | 2.DB.05 | Bi2Se3 |
| ⓘ | Pilsenite | 2.DC.05 | Bi4Te3 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 9 - Silicates | |||
| ⓘ | Kyanite | 9.AF.15 | Al2(SiO4)O |
| ⓘ | Staurolite | 9.AF.30 | Fe2+2Al9Si4O23(OH) |
| ⓘ | 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 |
| Unclassified | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5(T8O22)W2 |
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Tourmaline' | - | AD3G6(T6O18)(BO3)3X3Z |
| ⓘ | 'Hornblende Root Name Group' | - | ◻Ca2(C2+4C3+)(AlSi7O22)W2 |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| H | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| B | Boron | |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| C | Carbon | |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | Oxygen | |
| O | ⓘ Amphibole Supergroup | AB2C5(T8O22)W2 |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Kyanite | Al2(SiO4)O |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| 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 | ⓘ Garnet Group | X3Z2(SiO4)3 |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Na | Sodium | |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Al | Aluminium | |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Kyanite | Al2(SiO4)O |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| 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 | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Kyanite | Al2(SiO4)O |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| Si | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| 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 |
| Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
| S | Sulfur | |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Bismuthinite | Bi2S3 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Chalcocite | Cu2S |
| S | ⓘ Covellite | CuS |
| S | ⓘ Cubanite | CuFe2S3 |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Stannite | Cu2FeSnS4 |
| 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 | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Ca | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | Iron | |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Cubanite | CuFe2S3 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Stannite | Cu2FeSnS4 |
| Fe | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| Cu | Copper | |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chalcocite | Cu2S |
| Cu | ⓘ Covellite | CuS |
| Cu | ⓘ Cubanite | CuFe2S3 |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Cu | ⓘ Stannite | Cu2FeSnS4 |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| Se | Selenium | |
| Se | ⓘ Guanajuatite | Bi2Se3 |
| Ag | Silver | |
| Ag | ⓘ Dyscrasite | Ag3Sb |
| Sn | Tin | |
| Sn | ⓘ Stannite | Cu2FeSnS4 |
| Sb | Antimony | |
| Sb | ⓘ Dyscrasite | Ag3Sb |
| Te | Tellurium | |
| Te | ⓘ Pilsenite | Bi4Te3 |
| Au | Gold | |
| Au | ⓘ Native Gold | Au |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
| Bi | Bismuth | |
| Bi | ⓘ Native Bismuth | Bi |
| Bi | ⓘ Bismuthinite | Bi2S3 |
| Bi | ⓘ Guanajuatite | Bi2Se3 |
| Bi | ⓘ Pilsenite | Bi4Te3 |
Other Regions, Features and Areas containing this locality
AsiaContinent
- Emeishan TrapsLarge Igneous Province
- Hindukush Himalayan RegionGroup of Mountain Ranges
- Tibetan PlateauPlateau
China
- Songpan-Ganzi Li Mineral BeltMineral Belt
- ⭔Southwest ChinaRegion
Eurasian PlateTectonic Plate
- Songpan-Ganzi Hoh-Xil TerraneOrogenic Belt
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References
Zaw, Khin; Peters, Stephen G.; Cromie, Paul; Burrett, Clive; Hou, Zengqian (2007) Nature, diversity of deposit types and metallogenic relations of South China. Ore Geology Reviews, 31 (1). doi:10.1016/j.oregeorev.2005.10.006
[1]Guan, Sensen; He, Zhengwei; Wang, Jiaxian; Chen, Xin; He, Li (2026) Geochemical Characteristics and Exploration Implications of Primary Halos in the Liwu Copper Deposit, Western Yangtze Block, China. Minerals, 16 (5). doi:10.3390/min16050496
[2]Yuan, Hua-yun, , , Zhou, Qing, Song, Yuan-bao, Zhang, Wei, Zhang, Hui-hua, Li, Tong-zhu, Yin, Tao, Wang, Chang-nan, Tang, Gao-lin, , , , (2026) Mineralization of the Liwu large-scale stratiform copper deposits in Sichuan Province, China: Constraints from fluid inclusions. China Geology, 6. 1-17 doi:10.31035/cg2023034