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Panzhihua Fe-V-Ti-(PGE) deposit, Dong District, Panzhihua, Sichuan, Chinai
Regional Level Types
Panzhihua Fe-V-Ti-(PGE) depositDeposit
Dong DistrictDistrict
PanzhihuaPrefecture-level City
SichuanProvince
ChinaCountry

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Latitude & Longitude (WGS84):
26° 35' 49'' North , 101° 45' 40'' East
Latitude & Longitude (decimal):
26.59698,101.76135
GRN:
N18E65
Type:
Deposit
Köppen climate type:
Cwa : Monsoon-influenced humid subtropical climate
Nearest Settlements:
PlacePopulationDistance
Dadukou461,513(2014)7.8km
Mindat Locality ID:
21216
Long-form identifier:
mindat:1:2:21216:7
GUID (UUID V4):
0
Name(s) in local language(s):
攀枝花铁钒钛(铂族元素)矿床, 东区, 攀枝花市, 四川省, 中国


Superlarge Fe-V-Ti and minor Cu-Ni-(PGE) deposit, hosted in a gabbroic layered mafic intrusion. A series of N-S-trending strike faults split the
intrusion into seven blocks from NE to SW, these are named Zhujiabaobao, Lanjiahuoshan, Jianbaobao, Daomakan, Gongshan, Nongnongping, and Nalaqing.
Located in the most southerly part of Pan-Xi rift zone.

The Panzhihua deposit is the one of the largest Fe-Ti oxide deposits in the world and holds 10,000 to 20,000 tons of Co resource with grades varying from 0.01 % to 0.02 %. The Panzhihua intrusion is composed mainly of gabbro and hosts Fe-Ti oxide ore bodies in its lower part. The Fe-Ti oxide ore of the Panzhihua Fe-Ti oxides deposit could be classified based on the structure: massive ores, densely disseminated ores, moderately disseminated ores, sparsely disseminated ores and laminated ores. The massive ores primarily consist of minerals from the titanomagnetite-ilmenite series (60 ∼ 90 %), with minor occurrences of clinopyroxeneclinopyroxene (0 ∼ 20 %), olivine (0 ∼ 10 %), and plagioclase (0 ∼ 10 %). The densely disseminated ores comprise minerals from the titanomagnetite-ilmenite series (45 ∼ 60 %), with minor occurrences of clinopyroxene-clinopyroxene (0 ∼ 25 %), olivine (0 ∼ 15 %), and plagioclase (0 ∼ 15 %). The predominant structures in the massive and densely disseminated ores are irregularly granular mosaic texture, with occasional presence of sulfides such as pyrrhotite, as well as later oxides like hematite. The moderately disseminated ores primarily consist of minerals from the titanomagnetite-ilmenite series (25 ∼ 45 %), with occurrences of clinopyroxene-clinopyroxene (25 ∼ 45 %), plagioclase (10 ∼ 15 %) and olivine (0 ∼ 10 %). The sparsely disseminated ores comprise minerals from the titanomagnetite-ilmenite series (15 ∼ 25 %), with occurrences of clinopyroxene-clinopyroxene (35 ∼ 50 %), plagioclase (15 ∼ 25 %) and olivine (0 ∼ 10 %).
The Panzhihua gabbroic intrusion has been divided into several zones from top to base including Upper zone (Uz), Middle zone (b) (Mzb), Middle zone (a) (Mza), Lower zone (Lz), Bottom zone (Bz) and Marginal zone (MGz). It's important to note that a ten-meter-thick layered intrusion comprising coarse-grained pegmatite gabbro and heavily altered ultramafic rocks have been recognized at the bottom of the Zhujiabaobao open-pit. The metallogenic phases of the Panzhihua Fe-Ti oxide deposit have been divided into magmatic, hydrothermal, and epithermal phases. The hydrothermal phase was further subdivided into two stages: the pyrrhotite (II)-linnaeite stage and chlorite-pyrrhotite (III)-pyrite stage followed by a supergene stage.

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Commodity List

This is a list of exploitable or exploited mineral commodities recorded from this region.


Mineral List

Mineral list contains entries from the region specified including sub-localities

40 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Rock list contains entries from the region specified including sub-localities

Select Rock List Type

Alphabetical ListTree Diagram

Detailed Mineral List:

ⓘAegirine-augite
Formula:(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘAenigmatite
Formula:Na4[Fe2+10Ti2]O4[Si12O36]
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘAlbite
Formula:Na(AlSi3O8)
ⓘ'Alkali Feldspar'
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘ'Amphibole Supergroup'
Formula:AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ'Apatite'
Formula:Ca5(PO4)3(Cl/F/OH)
ⓘArfvedsonite
Formula:[Na][Na2][Fe2+4Fe3+]Si8O22(OH)2
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘArsenopyrite
Formula:FeAsS
ⓘAugite
Formula:(CaxMgyFez)(Mgy1Fez1)Si2O6
ⓘAugite var. Ferroaugite
Formula:(CaxMgyFez)(Mgy1Fez1)Si2O6
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘBaddeleyite
Formula:ZrO2
ⓘCalcite
Formula:CaCO3
ⓘ'Calcium Amphibole Subgroup'
Formula:AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ⓘ'Calcium Amphibole Subgroup var. Hornblende'
Formula:AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ⓘChalcopyrite
Formula:CuFeS2
ⓘ'Chlorite Group'
ⓘClinoenstatite
Formula:MgSiO3
ⓘ'Clinopyroxene Subgroup'
ⓘCobaltpentlandite
Formula:Co9S8
ⓘDiopside
Formula:CaMgSi2O6
ⓘDolomite
Formula:CaMg(CO3)2
ⓘErlichmanite
Formula:OsS2
ⓘ'Fayalite-Forsterite Series'
ⓘ'Feldspar Group'
ⓘ'Ferro-eckermannite'
Formula:NaNa2(Fe2+4Al)Si8O22(OH)2
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘFerro-richterite
Formula:{Na}{CaNa}{Fe2+5}(Si8O22)(OH)2
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘFluorapatite
Formula:Ca5(PO4)3F
ⓘForsterite
Formula:Mg2SiO4
ⓘHematite
Formula:Fe2O3
ⓘHercynite
Formula:Fe2+Al2O4
ⓘ'Hornblende Root Name Group'
Formula:◻Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2
ⓘIlmenite
Formula:Fe2+TiO3
ⓘ'K Feldspar'
ⓘLinnaeite
Formula:Co2+Co3+2S4
ⓘMagnetite
Formula:Fe2+Fe3+2O4
ⓘMagnetite var. Titanium-bearing Magnetite
Formula:Fe2+(Fe3+,Ti)2O4
ⓘMagnetite var. Vanadium-bearing Magnetite
Formula:Fe2+(Fe3+,V3+ )2O4
ⓘMerenskyite
Formula:PdTe2
ⓘ'Mica Group'
ⓘMoncheite
Formula:Pt(Te,Bi)2
ⓘNative Iridium
Formula:(Ir,Os,Ru)
ⓘNative Iridium var. Osmiridium
Formula:(Ir,Os,Ru)
ⓘNative Platinum
Formula:Pt
ⓘ'Olivine Group'
Formula:M2SiO4
ⓘ'Orthopyroxene Subgroup'
ⓘPargasite
Formula:NaCa2(Mg4Al)(Si6Al2)O22(OH)2
ⓘPentlandite
Formula:(NixFey)Σ9S8
ⓘPhlogopite
Formula:KMg3(AlSi3O10)(OH)2
ⓘ'Plagioclase'
Formula:(Na,Ca)[(Si,Al)AlSi2]O8
ⓘPyrite
Formula:FeS2
ⓘ'Pyroxene Group'
Formula:ADSi2O6
ⓘPyrrhotite
Formula:Fe1-xS
ⓘQuartz
Formula:SiO2
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘRiebeckite
Formula:◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2
References:
Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
Zhou, M. F., Robinson, P. T., Lesher, C. M., Keays, R. R., Zhang, C. J., & Malpas, J. (2005). Geochemistry, petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe–Ti–V oxide deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Shellnutt, J. G., & Zhou, M. F. (2007). Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology, 243(3-4), 286-316.
Zhong, H., Zhu, W. G., Hu, R. Z., Xie, L. W., He, D. F., Liu, F., & Chu, Z. Y. (2009). Zircon U–Pb age and Sr–Nd–Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos, 110(1-4), 109-128.
Shellnutt, J. G., & Jahn, B. M. (2010). Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters, 289(3-4), 509-519.
Shellnutt, J. G., & Iizuka, Y. (2011). Mineralogy from three peralkaline granitic plutons of the Late Permian Emeishan large igneous province (SW China): evidence for contrasting magmatic conditions of A-type granitoids. European Journal of Mineralogy, 23(1), 45-61.
Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395.
ⓘ'Serpentine Subgroup'
Formula:D3[Si2O5](OH)4
ⓘSiegenite
Formula:CoNi2S4
ⓘSperrylite
Formula:PtAs2
ⓘSpinel
Formula:MgAl2O4
ⓘSpinel var. Pleonaste
Formula:(Mg,Fe)Al2O4
ⓘTitanite
Formula:CaTi(SiO4)O
ⓘTremolite
Formula:◻Ca2Mg5(Si8O22)(OH)2
ⓘUlvöspinel
Formula:TiFe2+2O4
ⓘZircon
Formula:Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Iridium1.AF.10(Ir,Os,Ru)
ⓘNative Platinum1.AF.10Pt
ⓘNative Iridium
var. Osmiridium		1.AF.10(Ir,Os,Ru)
Group 2 - Sulphides and Sulfosalts
ⓘCobaltpentlandite2.BB.15Co9S8
ⓘPentlandite2.BB.15(NixFey)Σ9S8
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘPyrrhotite2.CC.10Fe1-xS
ⓘLinnaeite2.DA.05Co2+Co3+2S4
ⓘSiegenite2.DA.05CoNi2S4
ⓘMerenskyite2.EA.20PdTe2
ⓘMoncheite2.EA.20Pt(Te,Bi)2
ⓘErlichmanite2.EB.05aOsS2
ⓘPyrite2.EB.05aFeS2
ⓘSperrylite2.EB.05aPtAs2
ⓘArsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
ⓘHercynite4.BB.05Fe2+Al2O4
ⓘMagnetite4.BB.05Fe2+Fe3+2O4
ⓘSpinel4.BB.05MgAl2O4
ⓘMagnetite
var. Titanium-bearing Magnetite		4.BB.05Fe2+(Fe3+,Ti)2O4
ⓘUlvöspinel4.BB.05TiFe2+2O4
ⓘSpinel
var. Pleonaste		4.BB.05(Mg,Fe)Al2O4
ⓘMagnetite
var. Vanadium-bearing Magnetite		4.BB.05Fe2+(Fe3+,V3+ )2O4
ⓘHematite4.CB.05Fe2O3
ⓘIlmenite4.CB.05Fe2+TiO3
ⓘQuartz4.DA.05SiO2
ⓘBaddeleyite4.DE.35ZrO2
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
ⓘDolomite5.AB.10CaMg(CO3)2
Group 8 - Phosphates, Arsenates and Vanadates
ⓘFluorapatite8.BN.05Ca5(PO4)3F
Group 9 - Silicates
ⓘForsterite9.AC.05Mg2SiO4
ⓘZircon9.AD.30Zr(SiO4)
ⓘTitanite9.AG.15CaTi(SiO4)O
ⓘClinoenstatite9.DA.10MgSiO3
ⓘAugite9.DA.15(CaxMgyFez)(Mgy1Fez1)Si2O6
ⓘDiopside9.DA.15CaMgSi2O6
ⓘAugite
var. Ferroaugite		9.DA.15(CaxMgyFez)(Mgy1Fez1)Si2O6
ⓘAegirine-augite9.DA.20(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
ⓘTremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2
ⓘPargasite9.DE.15NaCa2(Mg4Al)(Si6Al2)O22(OH)2
ⓘFerro-richterite9.DE.20{Na}{CaNa}{Fe2+5}(Si8O22)(OH)2
ⓘArfvedsonite9.DE.25[Na][Na2][Fe2+4Fe3+]Si8O22(OH)2
ⓘ'Ferro-eckermannite'9.DE.25NaNa2(Fe2+4Al)Si8O22(OH)2
ⓘRiebeckite9.DE.25◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2
ⓘAenigmatite9.DH.40Na4[Fe2+10Ti2]O4[Si12O36]
ⓘPhlogopite9.EC.20KMg3(AlSi3O10)(OH)2
ⓘAlbite9.FA.35Na(AlSi3O8)
Unclassified
ⓘ'Alkali Feldspar'-
ⓘ'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ'Chlorite Group'-
ⓘ'Feldspar Group'-
ⓘ'Calcium Amphibole Subgroup
var. Hornblende'		-AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ⓘ'Mica Group'-
ⓘ'Clinopyroxene Subgroup'-
ⓘ'Fayalite-Forsterite Series'-
ⓘ'Hornblende Root Name Group'-◻Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2
ⓘ'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
ⓘ'K Feldspar'-
ⓘ'Pyroxene Group'-ADSi2O6
ⓘ'Orthopyroxene Subgroup'-
ⓘ'Serpentine Subgroup'-D3[Si2O5](OH)4
ⓘ'Apatite'-Ca5(PO4)3(Cl/F/OH)
ⓘ'Olivine Group'-M2SiO4
ⓘ'Calcium Amphibole Subgroup'-AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2

List of minerals for each chemical element

HHydrogen
HⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
HⓘArfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
HⓘFerro-eckermanniteNaNa2(Fe42+Al)Si8O22(OH)2
HⓘFerro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
HⓘCalcium Amphibole Subgroup var.HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
HⓘPargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2
HⓘPhlogopiteKMg3(AlSi3O10)(OH)2
HⓘRiebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
HⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
HⓘHornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
HⓘSerpentine SubgroupD3[Si2O5](OH)4
HⓘApatiteCa5(PO4)3(Cl/F/OH)
HⓘCalcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
CCarbon
CⓘCalciteCaCO3
CⓘDolomiteCaMg(CO3)2
OOxygen
OⓘAegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
OⓘAenigmatiteNa4[Fe102+Ti2]O4[Si12O36]
OⓘAlbiteNa(AlSi3O8)
OⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
OⓘArfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
OⓘAugite(CaxMgyFez)(Mgy1Fez1)Si2O6
OⓘBaddeleyiteZrO2
OⓘCalciteCaCO3
OⓘClinoenstatiteMgSiO3
OⓘDiopsideCaMgSi2O6
OⓘDolomiteCaMg(CO3)2
OⓘFerro-eckermanniteNaNa2(Fe42+Al)Si8O22(OH)2
OⓘFerro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
OⓘFluorapatiteCa5(PO4)3F
OⓘForsteriteMg2SiO4
OⓘHematiteFe2O3
OⓘHercyniteFe2+Al2O4
OⓘCalcium Amphibole Subgroup var.HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
OⓘIlmeniteFe2+TiO3
OⓘMagnetiteFe2+Fe23+O4
OⓘPargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2
OⓘPhlogopiteKMg3(AlSi3O10)(OH)2
OⓘQuartzSiO2
OⓘRiebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
OⓘSpinelMgAl2O4
OⓘTitaniteCaTi(SiO4)O
OⓘMagnetite var.Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
OⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
OⓘUlvöspinelTiFe22+O4
OⓘZirconZr(SiO4)
OⓘSpinel var.Pleonaste(Mg,Fe)Al2O4
OⓘFayalite-Forsterite Series
OⓘHornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
OⓘPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
OⓘPyroxene GroupADSi2O6
OⓘSerpentine SubgroupD3[Si2O5](OH)4
OⓘApatiteCa5(PO4)3(Cl/F/OH)
OⓘOlivine GroupM2SiO4
OⓘCalcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
OⓘMagnetite var.Vanadium-bearing MagnetiteFe2+(Fe3+,V3+ )2O4
OⓘAugite var.Ferroaugite(CaxMgyFez)(Mgy1Fez1)Si2O6
FFluorine
FⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
FⓘFluorapatiteCa5(PO4)3F
FⓘCalcium Amphibole Subgroup var.HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
FⓘHornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
FⓘApatiteCa5(PO4)3(Cl/F/OH)
FⓘCalcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
NaSodium
NaⓘAegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
NaⓘAenigmatiteNa4[Fe102+Ti2]O4[Si12O36]
NaⓘAlbiteNa(AlSi3O8)
NaⓘArfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
NaⓘFerro-eckermanniteNaNa2(Fe42+Al)Si8O22(OH)2
NaⓘFerro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
NaⓘPargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2
NaⓘRiebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
NaⓘPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
MgⓘAegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
MgⓘAugite(CaxMgyFez)(Mgy1Fez1)Si2O6
MgⓘClinoenstatiteMgSiO3
MgⓘDiopsideCaMgSi2O6
MgⓘDolomiteCaMg(CO3)2
MgⓘForsteriteMg2SiO4
MgⓘPargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2
MgⓘPhlogopiteKMg3(AlSi3O10)(OH)2
MgⓘSpinelMgAl2O4
MgⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
MgⓘSpinel var.Pleonaste(Mg,Fe)Al2O4
MgⓘFayalite-Forsterite Series
MgⓘAugite var.Ferroaugite(CaxMgyFez)(Mgy1Fez1)Si2O6
AlAluminium
AlⓘAegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
AlⓘAlbiteNa(AlSi3O8)
AlⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
AlⓘFerro-eckermanniteNaNa2(Fe42+Al)Si8O22(OH)2
AlⓘHercyniteFe2+Al2O4
AlⓘCalcium Amphibole Subgroup var.HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
AlⓘPargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2
AlⓘPhlogopiteKMg3(AlSi3O10)(OH)2
AlⓘSpinelMgAl2O4
AlⓘSpinel var.Pleonaste(Mg,Fe)Al2O4
AlⓘHornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
AlⓘPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
AlⓘCalcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
SiSilicon
SiⓘAegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
SiⓘAenigmatiteNa4[Fe102+Ti2]O4[Si12O36]
SiⓘAlbiteNa(AlSi3O8)
SiⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
SiⓘArfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
SiⓘAugite(CaxMgyFez)(Mgy1Fez1)Si2O6
SiⓘClinoenstatiteMgSiO3
SiⓘDiopsideCaMgSi2O6
SiⓘFerro-eckermanniteNaNa2(Fe42+Al)Si8O22(OH)2
SiⓘFerro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
SiⓘForsteriteMg2SiO4
SiⓘCalcium Amphibole Subgroup var.HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
SiⓘPargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2
SiⓘPhlogopiteKMg3(AlSi3O10)(OH)2
SiⓘQuartzSiO2
SiⓘRiebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
SiⓘTitaniteCaTi(SiO4)O
SiⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
SiⓘZirconZr(SiO4)
SiⓘFayalite-Forsterite Series
SiⓘHornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
SiⓘPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiⓘPyroxene GroupADSi2O6
SiⓘSerpentine SubgroupD3[Si2O5](OH)4
SiⓘOlivine GroupM2SiO4
SiⓘCalcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
SiⓘAugite var.Ferroaugite(CaxMgyFez)(Mgy1Fez1)Si2O6
PPhosphorus
PⓘFluorapatiteCa5(PO4)3F
PⓘApatiteCa5(PO4)3(Cl/F/OH)
SSulfur
SⓘArsenopyriteFeAsS
SⓘChalcopyriteCuFeS2
SⓘCobaltpentlanditeCo9S8
SⓘErlichmaniteOsS2
SⓘLinnaeiteCo2+Co23+S4
SⓘPentlandite(NixFey)Σ9S8
SⓘPyriteFeS2
SⓘPyrrhotiteFe1-xS
SⓘSiegeniteCoNi2S4
ClChlorine
ClⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ClⓘCalcium Amphibole Subgroup var.HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ClⓘHornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
ClⓘApatiteCa5(PO4)3(Cl/F/OH)
ClⓘCalcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
KPotassium
KⓘPhlogopiteKMg3(AlSi3O10)(OH)2
CaCalcium
CaⓘAegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
CaⓘAugite(CaxMgyFez)(Mgy1Fez1)Si2O6
CaⓘCalciteCaCO3
CaⓘDiopsideCaMgSi2O6
CaⓘDolomiteCaMg(CO3)2
CaⓘFerro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
CaⓘFluorapatiteCa5(PO4)3F
CaⓘCalcium Amphibole Subgroup var.HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
CaⓘPargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2
CaⓘTitaniteCaTi(SiO4)O
CaⓘTremolite◻Ca2Mg5(Si8O22)(OH)2
CaⓘHornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
CaⓘPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
CaⓘApatiteCa5(PO4)3(Cl/F/OH)
CaⓘCalcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
CaⓘAugite var.Ferroaugite(CaxMgyFez)(Mgy1Fez1)Si2O6
TiTitanium
TiⓘAenigmatiteNa4[Fe102+Ti2]O4[Si12O36]
TiⓘAmphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
TiⓘIlmeniteFe2+TiO3
TiⓘTitaniteCaTi(SiO4)O
TiⓘMagnetite var.Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
TiⓘUlvöspinelTiFe22+O4
VVanadium
VⓘMagnetite var.Vanadium-bearing MagnetiteFe2+(Fe3+,V3+ )2O4
FeIron
FeⓘAegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
FeⓘAenigmatiteNa4[Fe102+Ti2]O4[Si12O36]
FeⓘArsenopyriteFeAsS
FeⓘArfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
FeⓘAugite(CaxMgyFez)(Mgy1Fez1)Si2O6
FeⓘChalcopyriteCuFeS2
FeⓘFerro-eckermanniteNaNa2(Fe42+Al)Si8O22(OH)2
FeⓘFerro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
FeⓘHematiteFe2O3
FeⓘHercyniteFe2+Al2O4
FeⓘIlmeniteFe2+TiO3
FeⓘMagnetiteFe2+Fe23+O4
FeⓘPentlandite(NixFey)Σ9S8
FeⓘPyriteFeS2
FeⓘPyrrhotiteFe1-xS
FeⓘRiebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
FeⓘMagnetite var.Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
FeⓘUlvöspinelTiFe22+O4
FeⓘSpinel var.Pleonaste(Mg,Fe)Al2O4
FeⓘFayalite-Forsterite Series
FeⓘMagnetite var.Vanadium-bearing MagnetiteFe2+(Fe3+,V3+ )2O4
FeⓘAugite var.Ferroaugite(CaxMgyFez)(Mgy1Fez1)Si2O6
CoCobalt
CoⓘCobaltpentlanditeCo9S8
CoⓘLinnaeiteCo2+Co23+S4
CoⓘSiegeniteCoNi2S4
NiNickel
NiⓘPentlandite(NixFey)Σ9S8
NiⓘSiegeniteCoNi2S4
CuCopper
CuⓘChalcopyriteCuFeS2
AsArsenic
AsⓘArsenopyriteFeAsS
AsⓘSperrylitePtAs2
ZrZirconium
ZrⓘBaddeleyiteZrO2
ZrⓘZirconZr(SiO4)
RuRuthenium
RuⓘNative Iridium(Ir,Os,Ru)
RuⓘNative Iridium var.Osmiridium(Ir,Os,Ru)
PdPalladium
PdⓘMerenskyitePdTe2
TeTellurium
TeⓘMerenskyitePdTe2
TeⓘMoncheitePt(Te,Bi)2
OsOsmium
OsⓘErlichmaniteOsS2
OsⓘNative Iridium(Ir,Os,Ru)
OsⓘNative Iridium var.Osmiridium(Ir,Os,Ru)
IrIridium
IrⓘNative Iridium(Ir,Os,Ru)
IrⓘNative Iridium var.Osmiridium(Ir,Os,Ru)
PtPlatinum
PtⓘMoncheitePt(Te,Bi)2
PtⓘNative PlatinumPt
PtⓘSperrylitePtAs2
BiBismuth
BiⓘMoncheitePt(Te,Bi)2

Geochronology

Mineralization age:Permian : 253.1 ± 1.9 Ma

Important note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.

Geologic TimeRocks, Minerals and Events
Phanerozoic
 Paleozoic
  Permian
   Lopingian
ⓘ Syenite253.1 ± 1.9 Ma

Localities in this Region

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Eurasian PlateTectonic Plate

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References

Wenchen Li (1992) Geology and genesis of the Panzhihua vanadiferous magnetite deposit. Geology and Prospecting, 28(10), 18-21.
Shijun Ni, Chengjiang Zhang, Yanguo Teng, Yuxiao Ma, Meifu Zhou, Sun Min, Malpas, J., Yuchang Li, Zhenguo Wang (2001) Environmental Impacts of Mining the Giant Panzhihua V-Ti Magnetite Deposit, SW China. Goldschmidt Conference Abstracts 2001, no. 3530.
Meifu Zhou, Robinson, P.T., Lesher, C.M., Keays, R.R., Chengjiang Zhang, Malpas, J. (2005) Geochemistry, Petrogenesis and Metallogenesis of the Panzhihua Gabbroic Layered Intrusion and Associated Fe–Ti–V Oxide Deposits, Sichuan Province, SW China. Journal of Petrology, 46(11), 2253-2280.
Hong Zhong, Weiguang Zhu (2006) Geochronology of layered mafic intrusions from the Pan–Xi area in the Emeishan large igneous province, SW China. Mineralium Deposita, 41(6), 599-606.
Junhong Zhao, Meifu Zhou (2006) Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua district (Sichuan Province, SW China): Implications for subduction-related metasomatism in the upper mantle. Precambrian Research, 152(1-2), 27-47.
Kwannang Pang, Chusi Li, Meifu Zhou, and Ripley, E.M. (2008): Abundant Fe–Ti oxide inclusions in olivine from the Panzhihua and Hongge layered intrusions, SW China: evidence for early saturation of Fe–Ti oxides in ferrobasaltic magma. Contributions to Mineralogy and Petrology 156, 307-321.
Wang, S., Sun, X., Li, Y., Xu, L., Fu, Y., Cong, F., ... & Lu, S. (2022). Baddeleyite U-Pb age and Hf isotopes, and metallogenic constraints of the Panzhihua carbonatite in SW China. Ore Geology Reviews, 105228.
Arndt, N., Ganino, C., & Li, C. (2023). Comment on: Baddeleyite U-Pb age and Hf isotopes, and constraints on genesis of the Panzhihua carbonatite in SW China by Wang et al.(2023). Ore Geology Reviews, 105305.
[1]Liu, Ruiqin, Ruan, Banxiao, Hu, Xinlu, Mei, Wei, Lv, Xinbiao, Zhang, Zhongcheng, Cheng, Zetao, Yang, Ao (2024) Occurrence and enrichment mechanism of Co in Fe-Ti oxide deposits: A case study of the world-class Panzhihua deposit in SW China.Ore Geology Reviews, 172. 106177doi:10.1016/j.oregeorev.2024.106177
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