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Baima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, Chinai
Regional Level Types
Baima V-Ti-Fe depositDeposit
Miyi CountyCounty
PanzhihuaPrefecture-level City
SichuanProvince
ChinaCountry

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Latitude & Longitude (WGS84):
27° 0' North , 102° 1' East
Latitude & Longitude (decimal):
Locality type:
Name(s) in local language(s):
白马钒钛铁矿, 米易县, 攀枝花市, 四川省, 中国


Vanadiferous titaniferous magnetite (V-Ti magnetite) deposit, hosted in layered gabbro of the mafic-ultramafic Baima intrusion which was emplaced into Lower Proterozoic metamorphic rocks (K-Ar age: 342-363 Ma).

The Baima intrusion is one of the four V-Ti magnetite-bearing mafic-ultramafic intrusions within the Panzhihua-Xichang (Pan-Xi) rift. Its outcrop area is about 100 km2.

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Standard Detailed Strunz Dana Chemical Elements

Mineral List


23 valid minerals.

Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Detailed Mineral List:

Aegirine
Formula: NaFe3+Si2O6
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Aegirine-augite
Formula: (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Albite-Anorthite Series'
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Allanite Group'
Formula: {A12+REE3+}{M3+2M32+}(Si2O7)(SiO4)O(OH)
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Amphibole Supergroup'
Formula: AX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Anorthite
Formula: Ca(Al2Si2O8)
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Bastnäsite'
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26; Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Chalcopyrite
Formula: CuFeS2
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Fayalite
Formula: Fe2+2SiO4
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Fayalite-Forsterite Series'
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Feldspar Group'
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Feldspar Group var: Perthite'
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
'Fergusonite'
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Ferro-richterite
Formula: {Na}{CaNa}{Fe2+5}(Si8O22)(OH)2
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Fluorapatite
Formula: Ca5(PO4)3F
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Fluorite
Formula: CaF2
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Forsterite
Formula: Mg2SiO4
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Hematite
Formula: Fe2O3
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Hercynite
Formula: Fe2+Al2O4
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
'Hornblende'
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Ilmenite
Formula: Fe2+TiO3
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26; Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Magnetite
Formula: Fe2+Fe3+2O4
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26; Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Magnetite var: Titaniferous Magnetite
Formula: Fe2+(Fe3+,Ti)2O4
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Magnetite var: Vanado-Magnetite
Formula: Fe2+Fe3+2O4
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Pentlandite
Formula: (FexNiy)Σ9S8
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Phlogopite
Formula: KMg3(AlSi3O10)(OH)2
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Pyrite
Formula: FeS2
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26; Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Pyrrhotite
Formula: Fe7S8
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Quartz
Formula: SiO2
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Riebeckite
Formula: ◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Thorite
Formula: Th(SiO4)
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Titanite
Formula: CaTi(SiO4)O
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Wollastonite
Formula: CaSiO3
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
Zircon
Formula: Zr(SiO4)
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.; Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Zircon var: Cyrtolite
Formula: Zr[(SiO4),(OH)4]
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.
Zircon var: Orvillite
Formula: near 9ZrO2 · 6SiO2 · 5H2O
Reference: Shellnutt, J. G., Zhou, M. F., & Zellmer, G. F. (2009). The role of Fe–Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap: an example from the Permian Baima igneous complex, SW China. Chemical Geology, 259(3-4), 204-217. Shellnutt, J. G., Wang, C. Y., Zhou, M. F., & Yang, Y. (2009). Zircon Lu–Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province (SW China): constraints on the mantle source. Journal of Asian Earth Sciences, 35(1), 45-55. 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. Zhong, H., Zhu, W. G., Chu, Z. Y., He, D. F., & Song, X. Y. (2007). SHRIMP U–Pb zircon geochronology, geochemistry, and Nd–Sr isotopic study of contrasting granites in the Emeishan large igneous province, SW China. Chemical Geology, 236(1-2), 112-133. Shellnutt, J. G., Jahn, B. M., & Dostal, J. (2010). Elemental and Sr–Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province, SW China. Lithos, 119(1-2), 34-46.

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pentlandite2.BB.15(FexNiy)Σ9S8
Pyrite2.EB.05aFeS2
Pyrrhotite2.CC.10Fe7S8
Group 3 - Halides
Fluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
Hematite4.CB.05Fe2O3
Hercynite4.BB.05Fe2+Al2O4
Ilmenite4.CB.05Fe2+TiO3
Magnetite4.BB.05Fe2+Fe3+2O4
var: Titaniferous Magnetite4.BB.05Fe2+(Fe3+,Ti)2O4
var: Vanado-Magnetite4.BB.05Fe2+Fe3+2O4
Quartz4.DA.05SiO2
Group 8 - Phosphates, Arsenates and Vanadates
Fluorapatite8.BN.05Ca5(PO4)3F
Group 9 - Silicates
Aegirine9.DA.25NaFe3+Si2O6
Aegirine-augite9.DA.20(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
Anorthite9.FA.35Ca(Al2Si2O8)
Fayalite9.AC.05Fe2+2SiO4
Ferro-richterite9.DE.20{Na}{CaNa}{Fe2+5}(Si8O22)(OH)2
Forsterite9.AC.05Mg2SiO4
Phlogopite9.EC.20KMg3(AlSi3O10)(OH)2
Riebeckite9.DE.25◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2
Thorite9.AD.30Th(SiO4)
Titanite9.AG.15CaTi(SiO4)O
Wollastonite9.DG.05CaSiO3
Zircon9.AD.30Zr(SiO4)
var: Cyrtolite9.AD.30Zr[(SiO4),(OH)4]
var: Orvillite9.AD.30near 9ZrO2 · 6SiO2 · 5H2O
Unclassified Minerals, Rocks, etc.
'Albite-Anorthite Series'-
'Allanite Group'-{A12+REE3+}{M3+2M32+}(Si2O7)(SiO4)O(OH)
'Amphibole Supergroup'-AX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
'Apatite'-Ca5(PO4)3(Cl/F/OH)
'Bastnäsite'-
'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
'Fayalite-Forsterite Series'-
'Feldspar Group'-
'var: Perthite'-
'Fergusonite'-
'Hornblende'-

List of minerals arranged by Dana 8th Edition classification

Group 2 - SULFIDES
AmBnXp, with (m+n):p = 9:8
Pentlandite2.7.1.1(FexNiy)Σ9S8
AmXp, with m:p = 1:1
Pyrrhotite2.8.10.1Fe7S8
AmBnXp, with (m+n):p = 1:1
Chalcopyrite2.9.1.1CuFeS2
AmBnXp, with (m+n):p = 1:2
Pyrite2.12.1.1FeS2
Group 4 - SIMPLE OXIDES
A2X3
Hematite4.3.1.2Fe2O3
Ilmenite4.3.5.1Fe2+TiO3
Group 7 - MULTIPLE OXIDES
AB2X4
Hercynite7.2.1.3Fe2+Al2O4
Magnetite7.2.2.3Fe2+Fe3+2O4
Group 9 - NORMAL HALIDES
AX2
Fluorite9.2.1.1CaF2
Group 41 - ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
A5(XO4)3Zq
Fluorapatite41.8.1.1Ca5(PO4)3F
Group 51 - NESOSILICATES Insular SiO4 Groups Only
Insular SiO4 Groups Only with all cations in octahedral [6] coordination
Fayalite51.3.1.1Fe2+2SiO4
Forsterite51.3.1.2Mg2SiO4
Insular SiO4 Groups Only with cations in >[6] coordination
Thorite51.5.2.3Th(SiO4)
Zircon51.5.2.1Zr(SiO4)
Group 52 - NESOSILICATES Insular SiO4 Groups and O,OH,F,H2O
Insular SiO4 Groups and O, OH, F, and H2O with cations in [6] and/or >[6] coordination
Titanite52.4.3.1CaTi(SiO4)O
Group 65 - INOSILICATES Single-Width,Unbranched Chains,(W=1)
Single-Width Unbranched Chains, W=1 with chains P=2
Aegirine65.1.3c.2NaFe3+Si2O6
Aegirine-augite65.1.3b.2(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
Single-Width Unbranched Chains, W=1 with chains P=3
Wollastonite65.2.1.1cCaSiO3
Group 71 - PHYLLOSILICATES Sheets of Six-Membered Rings
Sheets of 6-membered rings with 2:1 layers
Phlogopite71.2.2b.1KMg3(AlSi3O10)(OH)2
Group 75 - TECTOSILICATES Si Tetrahedral Frameworks
Si Tetrahedral Frameworks - SiO2 with [4] coordinated Si
Quartz75.1.3.1SiO2
Unclassified Minerals, Mixtures, etc.
'Albite-Anorthite Series'-
'Allanite Group'-{A12+REE3+}{M3+2M32+}(Si2O7)(SiO4)O(OH)
'Amphibole Supergroup'-AX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Anorthite-Ca(Al2Si2O8)
'Apatite'-Ca5(PO4)3(Cl/F/OH)
'Bastnäsite'-
'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
'Fayalite-Forsterite Series'-
'Feldspar Group'-
'var: Perthite'-
'Fergusonite'-
Ferro-richterite-{Na}{CaNa}{Fe2+5}(Si8O22)(OH)2
'Hornblende'-
Magnetite
var: Titaniferous Magnetite
-Fe2+(Fe3+,Ti)2O4
var: Vanado-Magnetite-Fe2+Fe3+2O4
Riebeckite-◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2
Zircon
var: Cyrtolite
-Zr[(SiO4),(OH)4]
var: Orvillite-near 9ZrO2 · 6SiO2 · 5H2O

List of minerals for each chemical element

HHydrogen
H Amphibole SupergroupAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
H BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
H PhlogopiteKMg3(AlSi3O10)(OH)2
H Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
H ApatiteCa5(PO4)3(Cl/F/OH)
H Riebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
H Allanite Group{A12+REE3+}{M23+M32+}(Si2O7)(SiO4)O(OH)
H Zircon (var: Orvillite)near 9ZrO2 · 6SiO2 · 5H2O
H Zircon (var: Cyrtolite)Zr[(SiO4),(OH)4]
OOxygen
O Magnetite (var: Titaniferous Magnetite)Fe2+(Fe3+,Ti)2O4
O Amphibole SupergroupAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
O Magnetite (var: Vanado-Magnetite)Fe2+Fe23+O4
O BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
O ForsteriteMg2SiO4
O PhlogopiteKMg3(AlSi3O10)(OH)2
O FluorapatiteCa5(PO4)3F
O HercyniteFe2+Al2O4
O IlmeniteFe2+TiO3
O WollastoniteCaSiO3
O AnorthiteCa(Al2Si2O8)
O MagnetiteFe2+Fe23+O4
O FayaliteFe22+SiO4
O Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
O QuartzSiO2
O AegirineNaFe3+Si2O6
O ApatiteCa5(PO4)3(Cl/F/OH)
O TitaniteCaTi(SiO4)O
O ZirconZr(SiO4)
O HematiteFe2O3
O Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
O Riebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
O Allanite Group{A12+REE3+}{M23+M32+}(Si2O7)(SiO4)O(OH)
O ThoriteTh(SiO4)
O Zircon (var: Orvillite)near 9ZrO2 · 6SiO2 · 5H2O
O Zircon (var: Cyrtolite)Zr[(SiO4),(OH)4]
FFluorine
F Amphibole SupergroupAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
F BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
F FluorapatiteCa5(PO4)3F
F ApatiteCa5(PO4)3(Cl/F/OH)
F FluoriteCaF2
NaSodium
Na Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
Na AegirineNaFe3+Si2O6
Na Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Na Riebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
MgMagnesium
Mg BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
Mg ForsteriteMg2SiO4
Mg PhlogopiteKMg3(AlSi3O10)(OH)2
Mg Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
AlAluminium
Al Amphibole SupergroupAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Al BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
Al PhlogopiteKMg3(AlSi3O10)(OH)2
Al HercyniteFe2+Al2O4
Al AnorthiteCa(Al2Si2O8)
Al Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
SiSilicon
Si Amphibole SupergroupAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Si BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
Si ForsteriteMg2SiO4
Si PhlogopiteKMg3(AlSi3O10)(OH)2
Si WollastoniteCaSiO3
Si AnorthiteCa(Al2Si2O8)
Si FayaliteFe22+SiO4
Si Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
Si QuartzSiO2
Si AegirineNaFe3+Si2O6
Si TitaniteCaTi(SiO4)O
Si ZirconZr(SiO4)
Si Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Si Riebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
Si Allanite Group{A12+REE3+}{M23+M32+}(Si2O7)(SiO4)O(OH)
Si ThoriteTh(SiO4)
Si Zircon (var: Orvillite)near 9ZrO2 · 6SiO2 · 5H2O
Si Zircon (var: Cyrtolite)Zr[(SiO4),(OH)4]
PPhosphorus
P FluorapatiteCa5(PO4)3F
P ApatiteCa5(PO4)3(Cl/F/OH)
SSulfur
S PyrrhotiteFe7S8
S Pentlandite(FexNiy)Σ9S8
S PyriteFeS2
S ChalcopyriteCuFeS2
ClChlorine
Cl Amphibole SupergroupAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Cl ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
K BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
K PhlogopiteKMg3(AlSi3O10)(OH)2
CaCalcium
Ca FluorapatiteCa5(PO4)3F
Ca WollastoniteCaSiO3
Ca AnorthiteCa(Al2Si2O8)
Ca Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
Ca ApatiteCa5(PO4)3(Cl/F/OH)
Ca TitaniteCaTi(SiO4)O
Ca FluoriteCaF2
Ca Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
TiTitanium
Ti Magnetite (var: Titaniferous Magnetite)Fe2+(Fe3+,Ti)2O4
Ti Amphibole SupergroupAX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Ti IlmeniteFe2+TiO3
Ti TitaniteCaTi(SiO4)O
FeIron
Fe Magnetite (var: Titaniferous Magnetite)Fe2+(Fe3+,Ti)2O4
Fe Magnetite (var: Vanado-Magnetite)Fe2+Fe23+O4
Fe BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg)([Si/Al]Si2O10)(OH/F)2
Fe HercyniteFe2+Al2O4
Fe IlmeniteFe2+TiO3
Fe PyrrhotiteFe7S8
Fe Pentlandite(FexNiy)Σ9S8
Fe PyriteFeS2
Fe ChalcopyriteCuFeS2
Fe MagnetiteFe2+Fe23+O4
Fe FayaliteFe22+SiO4
Fe Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
Fe AegirineNaFe3+Si2O6
Fe HematiteFe2O3
Fe Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Fe Riebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
NiNickel
Ni Pentlandite(FexNiy)Σ9S8
CuCopper
Cu ChalcopyriteCuFeS2
ZrZirconium
Zr ZirconZr(SiO4)
Zr Zircon (var: Orvillite)near 9ZrO2 · 6SiO2 · 5H2O
Zr Zircon (var: Cyrtolite)Zr[(SiO4),(OH)4]
ThThorium
Th ThoriteTh(SiO4)

Geochronology

Mineralization age: Permian : 262 ± 2 Ma to 256.2 Ma

Important note: This table is based only on rock and mineral ages recorded below 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
ⓘ Zircon (youngest age)256.2 Ma
ⓘ Syenite (youngest age)258 ± 4 Ma
ⓘ Syenite (oldest age)259 ± 5 Ma
   Guadalupian
ⓘ Gabbro261 ± 2 Ma
ⓘ Zircon (oldest age)262 ± 2 Ma

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Fuwen Chen (1990): Petrologic study on Baima ore-bearing layered mafic-ultramafic intrusion. Acta Petrologica Sinica 6(4), 12-26 (in Chinese with English abstract).
Hong Zhong and 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.

External Links


Other Regions, Features and Areas containg this locality

AsiaContinent
China
Eurasian PlateTectonic Plate

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