Songshan Sn deposit, Lincang, Yunnan, Chinai
Regional Level Types | |
---|---|
Songshan Sn deposit | Deposit |
Lincang | Prefecture-level City |
Yunnan | Province |
China | Country |
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Latitude & Longitude (WGS84):
24° 41' 38'' North , 99° 48' 45'' East
Latitude & Longitude (decimal):
Locality type:
KΓΆppen climate type:
The Upper part of the Songshan Formation is composed of sericite-quartz schist, sericite microcrystalline schist, and Calcareous silicate. They are intercalated with several layers of garnet-actinolite skarn. The Lower part of the Songshan Formation is characteristic of chlorite quartz schist interbedded with sericite quartz schist. The Datianyakou Formation is composed of plagioclase-bearing porphyroblastic schist and granulite. The Pinghejie granitic pluton which is composed of granodiorite, biotite monzogranite, intruded into the Songshan Formation. Tin mineralization occurred as tin-bearing (tourmaline)-quartz veins in the Songshan deposit, which was controlled by NNW-trending and NNE-trending fractures, occurred in the Pinghejie granitic pluton and the Songshan Formation schist.
There are several ores segments that occur in the Songshan deposit, such as Laodiji-Chumadiji, Xiaozhai, Linggangzhai, Zhoujiazhai, Malishu, and Guangshan. Orebodies in the schist occur in the Laodiji-Chumadiji, Zhoujiazhai, and Linggangzhai ores segments with shallow dip angles and lengths of 30β60 m. Tin mineralization mainly occurred as tourmaline-quartz veins within the skarn and filled the fractures in the granite and the schist. The skarn was fragmented seriously, accompanied by silicification and sulfide mineralization.
Orebodies in the Pinghejie biotite monzogranite occur as quartz-tourmaline veins or quartz veins in the Malishu, Xiaozhai, and Guangshan ores segments. The orebodies are controlled by the NNE-trending tension fissures.
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Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
10 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
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Alphabetical List Tree DiagramDetailed Mineral List:
β Actinolite Formula: ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Cassiterite Formula: SnO2 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β 'Chlorite Group' Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Diopside Formula: CaMgSi2O6 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Epidote Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β 'Garnet Group' Formula: X3Z2(SiO4)3 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Hematite Formula: Fe2O3 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Muscovite Formula: KAl2(AlSi3O10)(OH)2 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Pyrite Formula: FeS2 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Pyrrhotite Formula: Fe1-xS Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Quartz Formula: SiO2 Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β 'Tourmaline' Formula: AD3G6 (T6O18)(BO3)3X3Z Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
β Zircon Formula: Zr(SiO4) Reference: Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | Pyrite | 2.EB.05a | FeS2 |
β | Pyrrhotite | 2.CC.10 | Fe1-xS |
Group 4 - Oxides and Hydroxides | |||
β | Cassiterite | 4.DB.05 | SnO2 |
β | Hematite | 4.CB.05 | Fe2O3 |
β | Quartz | 4.DA.05 | SiO2 |
Group 9 - Silicates | |||
β | Actinolite | 9.DE.10 | β»Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
β | Diopside | 9.DA.15 | CaMgSi2O6 |
β | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
β | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | Zircon | 9.AD.30 | Zr(SiO4) |
Unclassified Minerals, Rocks, etc. | |||
β | 'Chlorite Group' | - | |
β | 'Garnet Group' | - | X3Z2(SiO4)3 |
β | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
β | 'Tourmaline' | - | AD3G6 (T6O18)(BO3)3X3Z |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
H | β Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
H | β Muscovite | KAl2(AlSi3O10)(OH)2 |
H | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
B | Boron | |
B | β Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | Oxygen | |
O | β Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
O | β Zircon | Zr(SiO4) |
O | β Cassiterite | SnO2 |
O | β Diopside | CaMgSi2O6 |
O | β Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
O | β Garnet Group | X3Z2(SiO4)3 |
O | β Hematite | Fe2O3 |
O | β Muscovite | KAl2(AlSi3O10)(OH)2 |
O | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
O | β Quartz | SiO2 |
O | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
O | β Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
Na | Sodium | |
Na | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Mg | Magnesium | |
Mg | β Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
Mg | β Diopside | CaMgSi2O6 |
Al | Aluminium | |
Al | β Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
Al | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Al | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
Si | Silicon | |
Si | β Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
Si | β Zircon | Zr(SiO4) |
Si | β Diopside | CaMgSi2O6 |
Si | β Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
Si | β Garnet Group | X3Z2(SiO4)3 |
Si | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | β Quartz | SiO2 |
Si | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
S | Sulfur | |
S | β Pyrite | FeS2 |
S | β Pyrrhotite | Fe1-xS |
K | Potassium | |
K | β Muscovite | KAl2(AlSi3O10)(OH)2 |
K | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
Ca | Calcium | |
Ca | β Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
Ca | β Diopside | CaMgSi2O6 |
Ca | β Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
Ca | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Fe | Iron | |
Fe | β Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
Fe | β Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
Fe | β Hematite | Fe2O3 |
Fe | β Pyrite | FeS2 |
Fe | β Pyrrhotite | Fe1-xS |
Zr | Zirconium | |
Zr | β Zircon | Zr(SiO4) |
Sn | Tin | |
Sn | β Cassiterite | SnO2 |
References
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Year (asc) Year (desc) Author (A-Z) Author (Z-A) In-text Citation No.Zhu, Y., Li, X., & Li, Z. (2022). The fractures-controlled tin mineralization at the end of Late Cretaceous in the Songshan deposit, southwestern China: constraints from UβPb dating of zircon, garnet, and cassiterite. Ore Geology Reviews, 105191.
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