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Yangliuping Cu-Ni-PGE deposit, Yangliuping Cu-Ni-PGE ore field, Danba Co., Garzê Autonomous Prefecture (Ganzi Autonomous Prefecture), Sichuan, Chinai
Regional Level Types
Yangliuping Cu-Ni-PGE depositDeposit
Yangliuping Cu-Ni-PGE ore fieldOre Field
Danba Co.County
Garzê Autonomous Prefecture (Ganzi Autonomous Prefecture)Prefecture
SichuanProvince
ChinaCountry

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Latitude & Longitude (WGS84):
30° 41' 54'' North , 101° 54' 34'' East
Latitude & Longitude (decimal):
30.69861,101.90972
GRN:
N21E63
Type:
Deposit
Köppen climate type:
Cwb : Subtropical highland climate or temperate oceanic climate with dry winters
Mindat Locality ID:
730
Long-form identifier:
mindat:1:2:730:7
GUID (UUID V4):
0
Name(s) in local language(s):
杨柳坪铜镍铂族矿, 杨柳坪铜镍铂族矿田, 丹巴县, 甘孜藏族自治州, 四川省, 中国


Tectonic dome, consisting of Devonian to Triassic strata that underwent Late Triassic greenschist facies metamorphism. These rocks are overlain by Carboniferous calcareous slate and micaschist, Early Permian marble and Late Permian basalts of the Dashibao Formation, which are believed to form part of the Emeishan continental flood basalt system.

Four mafic-ultramafic sills intruding Devonian carbonaceous marble and graphitic schists in the center of the Yangliuping dome are the hosts for PGE-bearing Ni-Cu-sulphide mineralizations (Daqiangyanwo, Xiezuoping, Yangliuping and Zhengziyanwo ore blocks). The sills are believed to have acted as conduits for the overlying Dashibao formation basalts where the magma passed through prior to eruption. The rocks have been modified by hydrothermal activity and now chiefly consist of serpentinite, talc schist, tremolite schist and meta-gabbro. Disseminated Cu-Ni-sulphide mineralization (with 0.2-2 g/t PGE), accounting for more than 95% of the ore reserves, occurs abundantly in the serpentinite in the lower parts of the sill. Massive sulphide minerals (with 1-8 g/t PGE) occur at the base of the sill and in the footwall along fractures beneath the mineralized serpentinite. There also exist independent ore bodies which were formed by hydrothermal replacement and are hosted in limestones and shales instead of magmatic rocks. These ore bodies were preferentially mined because of their high grades of copper and nickel (e.g. Yuhaizi ore block).

Sulphides also occur in small, uneconomic veinlets, with quartz and calcite as gangue minerals. Contact metamorphic minerals, including slender prismatic diopside and granular epidote or garnet, occur locally in marble near the boundaries of the sill.

Located about 30 km south of Danba.

Select Mineral List Type

StandardDetailedGalleryStrunzChemical Elements

Detailed Mineral List:

ⓘActinolite
Formula:◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
ⓘAlbite
Formula:Na(AlSi3O8)
ⓘ'Amphibole Supergroup'
Formula:AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ'Amphibole Supergroup var. Uralite'
Formula:AX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘArsenopyrite
Formula:FeAsS
ⓘ'Biotite'
Formula:K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
ⓘBornite
Formula:Cu5FeS4
ⓘCalcite
Formula:CaCO3
ⓘChalcopyrite
Formula:CuFeS2
ⓘ'Chlorite Group'
ⓘChromferide
Formula:Fe3Cr1-x (x = 0.6)
ⓘChromite
Formula:Fe2+Cr3+2O4
ⓘCobaltite
Formula:CoAsS
ⓘCubanite
Formula:CuFe2S3
ⓘDanbaite (TL)
Formula:CuZn2
Type Locality:
ⓘDiopside
Formula:CaMgSi2O6
ⓘDolomite
Formula:CaMg(CO3)2
ⓘEpidote
Formula:(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘGalena
Formula:PbS
ⓘ'Garnet Group'
Formula:X3Z2(SiO4)3
ⓘGersdorffite
Formula:NiAsS
ⓘGoethite
Formula:Fe3+O(OH)
ⓘHematite
Formula:Fe2O3
ⓘ'Hexatestibiopanickelite'
Formula:(Pd,Ni)(Sb,Te) ?
ⓘIlmenite
Formula:Fe2+TiO3
ⓘKotulskite
Formula:Pd(Te,Bi)2-x (x ≈ 0.4)
Description: Contains significant amounts of bismuth and nickel.
ⓘLaurite
Formula:RuS2
ⓘLepidocrocite
Formula:Fe3+O(OH)
ⓘLinnaeite
Formula:Co2+Co3+2S4
ⓘMackinawite
Formula:FeS
ⓘMagnetite
Formula:Fe2+Fe3+2O4
ⓘMaslovite
Formula:PtBiTe
ⓘMelonite
Formula:NiTe2
ⓘMelonite var. Palladium-bearing Melonite
Formula:(Ni,Pd)Te2
ⓘMerenskyite
Formula:PdTe2
ⓘMichenerite
Formula:PdBiTe
ⓘMillerite
Formula:NiS
ⓘMoncheite
Formula:Pt(Te,Bi)2
ⓘMuscovite
Formula:KAl2(AlSi3O10)(OH)2
ⓘMuscovite var. Sericite
Formula:KAl2(AlSi3O10)(OH)2
ⓘNaldrettite
Formula:Pd2Sb
ⓘNative Chromium
Formula:Cr
ⓘNative Gold
Formula:Au
ⓘNative Gold var. Electrum
Formula:(Au,Ag)
ⓘNative Palladium
Formula:(Pd,Pt)
ⓘNative Platinum
Formula:Pt
ⓘNickeline
Formula:NiAs
ⓘOmeiite (TL)
Formula:(Os,Ru)As2
Type Locality:
ⓘPentlandite
Formula:(NixFey)Σ9S8
ⓘPentlandite var. Silver-bearing Pentlandite
Formula:(Ni,Fe,Ag)9S8
ⓘPyrite
Formula:FeS2
ⓘPyrite var. Bravoite
Formula:(Fe,Ni)S2
ⓘPyrrhotite
Formula:Fe1-xS
ⓘQuartz
Formula:SiO2
ⓘQusongite
Formula:WC
ⓘ'Saussurite'
ⓘ'Serpentine Subgroup'
Formula:D3[Si2O5](OH)4
ⓘSperrylite
Formula:PtAs2
ⓘSphalerite
Formula:ZnS
ⓘStibiopalladinite
Formula:Pd5Sb2
ⓘSudburyite
Formula:PdSb
ⓘTalc
Formula:Mg3Si4O10(OH)2
ⓘTellurobismuthite
Formula:Bi2Te3
ⓘTestibiopalladite
Formula:PdSbTe
ⓘTitanite
Formula:CaTi(SiO4)O
ⓘTremolite
Formula:◻Ca2Mg5(Si8O22)(OH)2
ⓘVavřínite
Formula:Ni2SbTe2
ⓘViolarite
Formula:Fe2+Ni3+2S4
ⓘZoisite
Formula:(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Gold
var. Electrum		1.AA.05(Au,Ag)
ⓘ1.AA.05Au
ⓘDanbaite (TL)1.AB.10bCuZn2
ⓘNative Chromium1.AE.05Cr
ⓘChromferide1.AE.15Fe3Cr1-x (x = 0.6)
ⓘNative Palladium1.AF.10(Pd,Pt)
ⓘNative Platinum1.AF.10Pt
ⓘQusongite1.BA.25WC
Group 2 - Sulphides and Sulfosalts
ⓘStibiopalladinite2.AC.20aPd5Sb2
ⓘNaldrettite2.AC.25dPd2Sb
ⓘBornite2.BA.15Cu5FeS4
ⓘPentlandite2.BB.15(NixFey)Σ9S8
ⓘvar. Silver-bearing Pentlandite2.BB.15(Ni,Fe,Ag)9S8
ⓘSphalerite2.CB.05aZnS
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘCubanite2.CB.55aCuFe2S3
ⓘKotulskite2.CC.05Pd(Te,Bi)2-x (x ≈ 0.4)
ⓘNickeline2.CC.05NiAs
ⓘSudburyite2.CC.05PdSb
ⓘPyrrhotite2.CC.10Fe1-xS
ⓘMillerite2.CC.20NiS
ⓘMackinawite2.CC.25FeS
ⓘ'Hexatestibiopanickelite'2.CC.30(Pd,Ni)(Sb,Te) ?
ⓘVavřínite2.CC.30Ni2SbTe2
ⓘGalena2.CD.10PbS
ⓘLinnaeite2.DA.05Co2+Co3+2S4
ⓘViolarite2.DA.05Fe2+Ni3+2S4
ⓘTellurobismuthite2.DC.05Bi2Te3
ⓘMelonite2.EA.20NiTe2
ⓘMerenskyite2.EA.20PdTe2
ⓘMoncheite2.EA.20Pt(Te,Bi)2
ⓘMelonite
var. Palladium-bearing Melonite		2.EA.20(Ni,Pd)Te2
ⓘPyrite
var. Bravoite		2.EB.05a(Fe,Ni)S2
ⓘLaurite2.EB.05aRuS2
ⓘPyrite2.EB.05aFeS2
ⓘSperrylite2.EB.05aPtAs2
ⓘOmeiite (TL)2.EB.15a(Os,Ru)As2
ⓘArsenopyrite2.EB.20FeAsS
ⓘCobaltite2.EB.25CoAsS
ⓘGersdorffite2.EB.25NiAsS
ⓘMaslovite2.EB.25PtBiTe
ⓘMichenerite2.EB.25PdBiTe
ⓘTestibiopalladite2.EB.25PdSbTe
Group 4 - Oxides and Hydroxides
ⓘGoethite4.00.Fe3+O(OH)
ⓘChromite4.BB.05Fe2+Cr3+2O4
ⓘMagnetite4.BB.05Fe2+Fe3+2O4
ⓘHematite4.CB.05Fe2O3
ⓘIlmenite4.CB.05Fe2+TiO3
ⓘQuartz4.DA.05SiO2
ⓘLepidocrocite4.FE.15Fe3+O(OH)
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
ⓘDolomite5.AB.10CaMg(CO3)2
Group 9 - Silicates
ⓘTitanite9.AG.15CaTi(SiO4)O
ⓘEpidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘZoisite9.BG.10(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
ⓘDiopside9.DA.15CaMgSi2O6
ⓘActinolite9.DE.10◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
ⓘTremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2
ⓘTalc9.EC.05Mg3Si4O10(OH)2
ⓘMuscovite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘvar. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘAlbite9.FA.35Na(AlSi3O8)
Unclassified
ⓘ'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
ⓘ'Chlorite Group'-
ⓘ'Amphibole Supergroup
var. Uralite'		-AX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ'Garnet Group'-X3Z2(SiO4)3
ⓘ'Serpentine Subgroup'-D3[Si2O5](OH)4
ⓘ'Saussurite'-

List of minerals for each chemical element

HHydrogen
HⓘActinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
HⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
HⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
HⓘEpidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
HⓘGoethiteFe3+O(OH)
HⓘLepidocrociteFe3+O(OH)
HⓘMuscoviteKAl2(AlSi3O10)(OH)2
HⓘTalcMg3Si4O10(OH)2
HⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
HⓘAmphibole Supergroup var.UraliteAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
HⓘZoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
HⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
HⓘSerpentine SubgroupD3[Si2O5](OH)4
CCarbon
CⓘCalciteCaCO3
CⓘDolomiteCaMg(CO3)2
CⓘQusongiteWC
OOxygen
OⓘActinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
OⓘAlbiteNa(AlSi3O8)
OⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
OⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
OⓘCalciteCaCO3
OⓘChromiteFe2+Cr23+O4
OⓘDiopsideCaMgSi2O6
OⓘDolomiteCaMg(CO3)2
OⓘEpidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
OⓘGoethiteFe3+O(OH)
OⓘHematiteFe2O3
OⓘIlmeniteFe2+TiO3
OⓘLepidocrociteFe3+O(OH)
OⓘMagnetiteFe2+Fe23+O4
OⓘMuscoviteKAl2(AlSi3O10)(OH)2
OⓘQuartzSiO2
OⓘTalcMg3Si4O10(OH)2
OⓘTitaniteCaTi(SiO4)O
OⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
OⓘAmphibole Supergroup var.UraliteAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
OⓘZoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
OⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
OⓘGarnet GroupX3Z2(SiO4)3
OⓘSerpentine SubgroupD3[Si2O5](OH)4
FFluorine
FⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
FⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FⓘAmphibole Supergroup var.UraliteAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
NaSodium
NaⓘAlbiteNa(AlSi3O8)
MgMagnesium
MgⓘActinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
MgⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MgⓘDiopsideCaMgSi2O6
MgⓘDolomiteCaMg(CO3)2
MgⓘTalcMg3Si4O10(OH)2
MgⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
AlAluminium
AlⓘAlbiteNa(AlSi3O8)
AlⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
AlⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
AlⓘEpidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
AlⓘMuscoviteKAl2(AlSi3O10)(OH)2
AlⓘAmphibole Supergroup var.UraliteAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
AlⓘZoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
AlⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
SiⓘActinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
SiⓘAlbiteNa(AlSi3O8)
SiⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
SiⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
SiⓘDiopsideCaMgSi2O6
SiⓘEpidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
SiⓘMuscoviteKAl2(AlSi3O10)(OH)2
SiⓘQuartzSiO2
SiⓘTalcMg3Si4O10(OH)2
SiⓘTitaniteCaTi(SiO4)O
SiⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
SiⓘAmphibole Supergroup var.UraliteAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
SiⓘZoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
SiⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
SiⓘGarnet GroupX3Z2(SiO4)3
SiⓘSerpentine SubgroupD3[Si2O5](OH)4
SSulfur
SⓘArsenopyriteFeAsS
SⓘBorniteCu5FeS4
SⓘPyrite var.Bravoite(Fe,Ni)S2
SⓘChalcopyriteCuFeS2
SⓘCobaltiteCoAsS
SⓘCubaniteCuFe2S3
SⓘGalenaPbS
SⓘGersdorffiteNiAsS
SⓘLauriteRuS2
SⓘLinnaeiteCo2+Co23+S4
SⓘMackinawiteFeS
SⓘMilleriteNiS
SⓘPentlandite(NixFey)Σ9S8
SⓘPyriteFeS2
SⓘPyrrhotiteFe1-xS
SⓘSphaleriteZnS
SⓘViolariteFe2+Ni23+S4
SⓘPentlandite var.Silver-bearing Pentlandite(Ni,Fe,Ag)9S8
ClChlorine
ClⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ClⓘAmphibole Supergroup var.UraliteAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
KPotassium
KⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
KⓘMuscoviteKAl2(AlSi3O10)(OH)2
KⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
CaⓘActinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
CaⓘCalciteCaCO3
CaⓘDiopsideCaMgSi2O6
CaⓘDolomiteCaMg(CO3)2
CaⓘEpidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
CaⓘTitaniteCaTi(SiO4)O
CaⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
CaⓘZoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
TiTitanium
TiⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
TiⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
TiⓘIlmeniteFe2+TiO3
TiⓘTitaniteCaTi(SiO4)O
TiⓘAmphibole Supergroup var.UraliteAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
CrChromium
CrⓘChromferideFe3Cr1-x (x = 0.6)
CrⓘChromiteFe2+Cr23+O4
CrⓘNative ChromiumCr
FeIron
FeⓘActinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
FeⓘArsenopyriteFeAsS
FeⓘBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FeⓘBorniteCu5FeS4
FeⓘPyrite var.Bravoite(Fe,Ni)S2
FeⓘChalcopyriteCuFeS2
FeⓘChromferideFe3Cr1-x (x = 0.6)
FeⓘChromiteFe2+Cr23+O4
FeⓘCubaniteCuFe2S3
FeⓘEpidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
FeⓘGoethiteFe3+O(OH)
FeⓘHematiteFe2O3
FeⓘIlmeniteFe2+TiO3
FeⓘLepidocrociteFe3+O(OH)
FeⓘMackinawiteFeS
FeⓘMagnetiteFe2+Fe23+O4
FeⓘPentlandite(NixFey)Σ9S8
FeⓘPyriteFeS2
FeⓘPyrrhotiteFe1-xS
FeⓘViolariteFe2+Ni23+S4
FeⓘPentlandite var.Silver-bearing Pentlandite(Ni,Fe,Ag)9S8
CoCobalt
CoⓘCobaltiteCoAsS
CoⓘLinnaeiteCo2+Co23+S4
NiNickel
NiⓘPyrite var.Bravoite(Fe,Ni)S2
NiⓘGersdorffiteNiAsS
NiⓘHexatestibiopanickelite(Pd,Ni)(Sb,Te) ?
NiⓘMeloniteNiTe2
NiⓘMilleriteNiS
NiⓘNickelineNiAs
NiⓘPentlandite(NixFey)Σ9S8
NiⓘViolariteFe2+Ni23+S4
NiⓘMelonite var.Palladium-bearing Melonite(Ni,Pd)Te2
NiⓘPentlandite var.Silver-bearing Pentlandite(Ni,Fe,Ag)9S8
NiⓘVavříniteNi2SbTe2
CuCopper
CuⓘBorniteCu5FeS4
CuⓘChalcopyriteCuFeS2
CuⓘCubaniteCuFe2S3
CuⓘDanbaiteCuZn2
ZnZinc
ZnⓘDanbaiteCuZn2
ZnⓘSphaleriteZnS
AsArsenic
AsⓘArsenopyriteFeAsS
AsⓘCobaltiteCoAsS
AsⓘGersdorffiteNiAsS
AsⓘNickelineNiAs
AsⓘOmeiite(Os,Ru)As2
AsⓘSperrylitePtAs2
RuRuthenium
RuⓘLauriteRuS2
RuⓘOmeiite(Os,Ru)As2
PdPalladium
PdⓘHexatestibiopanickelite(Pd,Ni)(Sb,Te) ?
PdⓘKotulskitePd(Te,Bi)2-x (x ≈ 0.4)
PdⓘMerenskyitePdTe2
PdⓘMicheneritePdBiTe
PdⓘNative Palladium(Pd,Pt)
PdⓘStibiopalladinitePd5Sb2
PdⓘSudburyitePdSb
PdⓘTestibiopalladitePdSbTe
PdⓘMelonite var.Palladium-bearing Melonite(Ni,Pd)Te2
PdⓘNaldrettitePd2Sb
AgSilver
AgⓘNative Gold var.Electrum(Au,Ag)
AgⓘPentlandite var.Silver-bearing Pentlandite(Ni,Fe,Ag)9S8
SbAntimony
SbⓘHexatestibiopanickelite(Pd,Ni)(Sb,Te) ?
SbⓘStibiopalladinitePd5Sb2
SbⓘSudburyitePdSb
SbⓘTestibiopalladitePdSbTe
SbⓘNaldrettitePd2Sb
SbⓘVavříniteNi2SbTe2
TeTellurium
TeⓘHexatestibiopanickelite(Pd,Ni)(Sb,Te) ?
TeⓘKotulskitePd(Te,Bi)2-x (x ≈ 0.4)
TeⓘMaslovitePtBiTe
TeⓘMeloniteNiTe2
TeⓘMerenskyitePdTe2
TeⓘMicheneritePdBiTe
TeⓘMoncheitePt(Te,Bi)2
TeⓘTellurobismuthiteBi2Te3
TeⓘTestibiopalladitePdSbTe
TeⓘMelonite var.Palladium-bearing Melonite(Ni,Pd)Te2
TeⓘVavříniteNi2SbTe2
WTungsten
WⓘQusongiteWC
OsOsmium
OsⓘOmeiite(Os,Ru)As2
PtPlatinum
PtⓘMaslovitePtBiTe
PtⓘMoncheitePt(Te,Bi)2
PtⓘNative Palladium(Pd,Pt)
PtⓘNative PlatinumPt
PtⓘSperrylitePtAs2
AuGold
AuⓘNative Gold var.Electrum(Au,Ag)
AuⓘNative GoldAu
PbLead
PbⓘGalenaPbS
BiBismuth
BiⓘKotulskitePd(Te,Bi)2-x (x ≈ 0.4)
BiⓘMaslovitePtBiTe
BiⓘMicheneritePdBiTe
BiⓘMoncheitePt(Te,Bi)2
BiⓘTellurobismuthiteBi2Te3

Localities in this Region

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Eurasian PlateTectonic Plate

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References

Platinum metal mineral research group, Kweiyang Institute of Geochemistry (1974): Telluro-stibnide of palladium and nickel and other new minerals and varieties of platinum metals. Geochimica 3(3), 169-181.
Dunn, Pete J., Chao, George Y., Fleischer, Michael, Ferraiolo, James A., Langley, Richard H., Pabst, Adolf, Zilczer, Janet A. (1985) New mineral names.American Mineralogist, 70 (1-2) 214-221
Denghong Wang, Yingshi Chu, Fuxun Luo, Zhi'an Lu, and Zhixin Tang (2000): The origin of the Cu-Ni-PGE orebody in Yangliuping, Sichuan Province, and the significance of its discovery. Acta Geoscientia Sinica 21(3), 260-265.
Xiaoqiang Hu, Yunquan Li, and Dequan Shuai (2001) Ore mineral research on Danba Cu-Ni-Pt deposit in Sichuan. Journal of Mineralogy and Petrology 21(1), 14-18 (in Chinese with English abstract).
Xiaoqiang Hu, Yunquan Li, and Dequan Shuai (2001): Ore fabric and metallogenic epoch of the Cu-Ni-Pt deposit in the Danba area, Sichuan. Journal of Chengdu University of Technology 28(1), 48-52 (in Chinese with English abstract).
Deng, H.-L., Campbell, A.J., and Humayun, M. (2002): Platinum Group Elements in sulfides from Yangliuping Cu-Ni-Pt-Pd Deposit in Sichuan, China. Goldschmidt Conference Abstracts 2002, A177.
Yao, Y., and Viljoen, M.J. (2003): Intrusion-hosted PGE mineralization in the Sichuan province, China. Goldschmidt Conference Abstracts 2003, A560.
Song, Xie-Yan; Zhou, Mei-Fu; Cao, Zhi-Min; Sun, Min; Wang, Yun-Liang (2003) Ni-Cu-(PGE) magmatic sulfide deposits in the Yangliuping area, Permian Emeishan igneous province, SW China.Mineralium Deposita, 38 (7). 831-843doi:10.1007/s00126-003-0362-3
Jianbin Zheng, Zhimin Cao, Xieyan Song, Wei An, and Ji Liu (2004): PGE geochemistry of the Yangliuping magmatic Ni-Cu-PGE sulfide deposit. Geology and Prospecting 40(5), 16-20.
Song, X.-Y.; Zhou, M.-F.; Cao, Z.-M. (2004) Genetic relationships between base-metal sulfides and platinum-group minerals in the Yangliuping Ni–Cu–(PGE) sulfide deposit, southwestern China.The Canadian Mineralogist, 42 (2). 469-483doi:10.2113/gscanmin.42.2.469
Song, Xie-Yan, Zhou, Mei-Fu, Keays, Reid R., Cao, Zhi-Min, Sun, Min, Qi, Liang (2006) Geochemistry of the Emeishan flood basalts at Yangliuping, Sichuan, SW China: implications for sulfide segregation.Contributions to Mineralogy and Petrology, 152 (1) 53-74doi:10.1007/s00410-006-0094-3
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