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Miyi County, Panzhihua, Sichuan, Chinai
Regional Level Types
Miyi CountyCounty
PanzhihuaPrefecture-level City
SichuanProvince
ChinaCountry

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Neighbouring regions:
Huili County, Liangshan Yi, Sichuan, China
Yanbian County, Panzhihua, Sichuan, China
Yanyuan County, Liangshan Yi, Sichuan, China
Dechang County, Liangshan Yi, Sichuan, China
Type:
County
Mindat Locality ID:
189112
Long-form identifier:
1:2:189112:9
GUID (UUID V4):
3945623d-157e-4b7f-9b62-961858afa19f
Other Languages:
View 13 more...
French:
Xian de Miyi, Panzhihua, Sichuan, Chine
German:
Miyi, Panzhihua, Sichuan, China
Italian:
Contea di Miyi, Panzhihua, Sichuan, Cina
Russian:
Мии, Паньчжихуа, Сычуань, Китай
Simplified Chinese:
米易县, 攀枝花市, 四川省, 中国
Cebuano:
Miyi Xian, Sichuan Sheng, Tsina
Dutch:
Miyi, Panzhihua, Sichuan, China
Farsi/Persian:
مایای, پنژیهوا, سیچوآن, جمهوری خلق چین
Gan:
米易县, 攀枝花市, 四川, 中國
Hakka:
Mí-yi-yen, Pân-kî-fâ-sṳ, Si-chhôn, Chûng-fà
Japanese:
米易県, 攀枝花市, 四川省, 中国
Korean:
미이현, 판즈화시, 쓰촨성, 중국
Minnan / Hokkien-Taiwanese:
Bí-e̍k-koān, Phan-chi-hoa-chhī, Sù-chhoan-séng, Tiong-hôa
Norwegian:
Miyi, Panzhihua, Sichuan, Kina
Polish:
Miyi, Panzhihua, Syczuan, Chiny
Swedish:
Miyi, Panzhihua, Sichuan, Kina
Vietnamese:
Mễ Dịch, Phàn Chi Hoa, Tứ Xuyên, Trung Quốc
Wu Chinese:
米易县, 攀枝花市, 四川省, 中国


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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

51 valid minerals. 1 (TL) - type locality of 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

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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
Formula: Na(AlSi3O8)
Reference: Lin, C., LIu, Y., Wang, Z., & Hong, W. (1995). Rare element and rare-earth element deposits of China. Mineral deposits of China, 3, 226-279.
ⓘ 'Alkali Feldspar'
Reference: Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
ⓘ 'Allanite Group'
Formula: (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
Reference: Fenlian Wang, Taiping Zhao, and Wei Chen (2012): Mineral Deposits 31(2), 293-308
ⓘ Altaite
Formula: PbTe
Reference: Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ 'Amphibole Supergroup'
Formula: AB2C5((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.
ⓘ Arfvedsonite
Formula: [Na][Na2][Fe2+4Fe3+]Si8O22(OH)2
Reference: Lin, C., LIu, Y., Wang, Z., & Hong, W. (1995). Rare element and rare-earth element deposits of China. Mineral deposits of China, 3, 226-279.
ⓘ 'Bastnäsite'
Formula: (Ce/Nd/Y/REE)(CO3)F
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/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Reference: Li Zhao, Zhaochong Zhang, Fusheng Wang, Yanli Hao, Yu Ai, and Tiezheng Yang (2006): Acta Petrologica Sinica 22(6), 1565-1578
ⓘ Bornite
Formula: Cu5FeS4
Reference: Li, X., Zhu, J., Lu, R., Gu, Y., Wu, X., & Chen, Y. (1997). Study on the occurrence of platinum in Xinjie Cu Ni sulfide deposits by a combination of SPM and NAA. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 130(1), 617-622.
ⓘ Borovskite
Formula: Pd3SbTe4
Reference: Yao, Y., and Viljoen, M.J. (2003): Goldschmidt Conference Abstracts 2003, A560
ⓘ Chalcopyrite
Formula: CuFeS2
Reference: Li, X., Zhu, J., Lu, R., Gu, Y., Wu, X., & Chen, Y. (1997). Study on the occurrence of platinum in Xinjie Cu Ni sulfide deposits by a combination of SPM and NAA. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 130(1), 617-622.; Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ 'Chlorite Group'
Reference: Li Zhao, Zhaochong Zhang, Fusheng Wang, Yanli Hao, Yu Ai, and Tiezheng Yang (2006): Acta Petrologica Sinica 22(6), 1565-1578
ⓘ Chromite
Formula: Fe2+Cr3+2O4
Reference: http://www.wits.ac.za/geosciences/Research/EGRI/Circulars/pdf_files/358.pdf; Wang, C. Y., & Zhou, M. F. (2005, January). Mineral chemistry of Fe-Ti oxides from the Xinjie PGE-bearing layered mafic-ultramafic intrusion in Sichuan, SW China. In Mineral deposit research: Meeting the global challenge (pp. 481-485). Springer Berlin Heidelberg.
ⓘ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Reference: Li Zhao, Zhaochong Zhang, Fusheng Wang, Yanli Hao, Yu Ai, and Tiezheng Yang (2006): Acta Petrologica Sinica 22(6), 1565-1578
ⓘ Erlichmanite
Formula: OsS2
ⓘ 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: http://www.wits.ac.za/geosciences/Research/EGRI/Circulars/pdf_files/358.pdf
ⓘ '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
ⓘ Haitaite-(La) (TL)
Formula: LaU4+Fe3+2(Ti13Fe2+4Fe3+)O38
Type Locality:
Reference: Wang, F., Fan, G., Li, T., Ge, X., Wu, Y., Wang, H., Yao, J. (2022) Haitaite-(La), LaU4+Fe3+2(Ti13Fe2+4Fe3+)Σ18O38, a New Member of the Crichtonite Group. Acta Geologica Sinica, 96(6), 2007-2014.; Wang, F., Fan, G., Li, T., Ge, X., Wu,Y., Wang, H., and Yao, J. (2021) Haitaite-(La), IMA 2019-033a, in: CNMNC Newsletter 60. European Journal of Mineralogy, 33(2), 203–208. https://doi.org/10.5194/ejm-33-203-2021.
ⓘ 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
ⓘ Hessite
Formula: Ag2Te
Reference: Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ '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: http://www.wits.ac.za/geosciences/Research/EGRI/Circulars/pdf_files/358.pdf; Wang, C. Y., & Zhou, M. F. (2005, January). Mineral chemistry of Fe-Ti oxides from the Xinjie PGE-bearing layered mafic-ultramafic intrusion in Sichuan, SW China. In Mineral deposit research: Meeting the global challenge (pp. 481-485). Springer Berlin Heidelberg.
ⓘ Ishikawaite
Formula: U4+Fe2+Nb2O8
Reference: Zhang Peishan, Yang Zhuming, Tao Kejie, and Yang Xueming (1996): "Mineralogy and Geology of Rare Earths in China", Science Press (Beijing), 226 pp.
ⓘ 'K Feldspar'
Reference: Xu, Zhengqi, Minghui Yin, Youliang Chen, Lu Xiang, Hao Song, Chengjiang Zhang, Jian Yao, and Hu Guo. (2021) "Genesis of Megacrystalline Uraninite: A Case Study of the Haita Area of the Western Margin of the Yangtze Block, China" Minerals 11, no. 11: 1173. https://doi.org/10.3390/min11111173
ⓘ Laurite
Formula: RuS2
ⓘ Magnetite
Formula: Fe2+Fe3+2O4
Reference: Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ Magnetite var. Titanium-bearing Magnetite
Formula: Fe2+(Fe3+,Ti)2O4
Reference: http://www.wits.ac.za/geosciences/Research/EGRI/Circulars/pdf_files/358.pdf; Wang, C. Y., & Zhou, M. F. (2005, January). Mineral chemistry of Fe-Ti oxides from the Xinjie PGE-bearing layered mafic-ultramafic intrusion in Sichuan, SW China. In Mineral deposit research: Meeting the global challenge (pp. 481-485). Springer Berlin Heidelberg.
ⓘ Magnetite var. Vanadium-bearing Magnetite
Formula: Fe2+(Fe3+,V3+ )2O4
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
ⓘ Merenskyite
Formula: PdTe2
Reference: Yao, Y., and Viljoen, M.J. (2003): Goldschmidt Conference Abstracts 2003, A560; Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ Michenerite
Formula: PdBiTe
Reference: Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ Millerite
Formula: NiS
ⓘ Molybdenite
Formula: MoS2
Reference: Xu, Zhengqi, Minghui Yin, Youliang Chen, Lu Xiang, Hao Song, Chengjiang Zhang, Jian Yao, and Hu Guo. (2021) "Genesis of Megacrystalline Uraninite: A Case Study of the Haita Area of the Western Margin of the Yangtze Block, China" Minerals 11, no. 11: 1173. https://doi.org/10.3390/min11111173
ⓘ Moncheite
Formula: Pt(Te,Bi)2
Reference: Yao, Y., and Viljoen, M.J. (2003): Goldschmidt Conference Abstracts 2003, A560; Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Reference: Li Zhao, Zhaochong Zhang, Fusheng Wang, Yanli Hao, Yu Ai, and Tiezheng Yang (2006): Acta Petrologica Sinica 22(6), 1565-1578
ⓘ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
Reference: Li Zhao, Zhaochong Zhang, Fusheng Wang, Yanli Hao, Yu Ai, and Tiezheng Yang (2006): Acta Petrologica Sinica 22(6), 1565-1578
ⓘ Nepheline
Formula: Na3K(Al4Si4O16)
Reference: Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
ⓘ Nickeline
Formula: NiAs
ⓘ Pentlandite
Formula: (NixFey)Σ9S8
Reference: Yao, Y., and Viljoen, M.J. (2003): Goldschmidt Conference Abstracts 2003, A560; Li, X., Zhu, J., Lu, R., Gu, Y., Wu, X., & Chen, Y. (1997). Study on the occurrence of platinum in Xinjie Cu Ni sulfide deposits by a combination of SPM and NAA. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 130(1), 617-622.; Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ Phlogopite
Formula: KMg3(AlSi3O10)(OH)2
Reference: Fuwen Chen (1990): Acta Petrologica Sinica 6(4), 12-26
ⓘ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Reference: http://www.wits.ac.za/geosciences/Research/EGRI/Circulars/pdf_files/358.pdf
ⓘ Platinum
Formula: Pt
ⓘ Pyrite
Formula: FeS2
ⓘ 'Pyrochlore Group'
Formula: A2Nb2(O,OH)6Z
Reference: Fenlian Wang, Taiping Zhao, and Wei Chen (2012): Mineral Deposits 31(2), 293-308
ⓘ 'Pyroxene Group'
Formula: ADSi2O6
Reference: Xu, Zhengqi, Minghui Yin, Youliang Chen, Lu Xiang, Hao Song, Chengjiang Zhang, Jian Yao, and Hu Guo. (2021) "Genesis of Megacrystalline Uraninite: A Case Study of the Haita Area of the Western Margin of the Yangtze Block, China" Minerals 11, no. 11: 1173. https://doi.org/10.3390/min11111173
ⓘ Pyrrhotite
Formula: Fe1-xS
Reference: Li, X., Zhu, J., Lu, R., Gu, Y., Wu, X., & Chen, Y. (1997). Study on the occurrence of platinum in Xinjie Cu Ni sulfide deposits by a combination of SPM and NAA. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 130(1), 617-622.; Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ Quartz
Formula: SiO2
Reference: http://www.wits.ac.za/geosciences/Research/EGRI/Circulars/pdf_files/358.pdf
ⓘ 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.
ⓘ Samarskite-(Y)
Formula: YFe3+Nb2O8
Reference: Zhang Peishan, Yang Zhuming, Tao Kejie, and Yang Xueming (1996): "Mineralogy and Geology of Rare Earths in China", Science Press (Beijing), 226 pp.
ⓘ Siegenite
Formula: CoNi2S4
ⓘ Sodalite
Formula: Na4(Si3Al3)O12Cl
Reference: Zhang, Y., Luo, Y., & Yang, C. (Eds.). (1990). Panxi Rift and its geodynamics. Geological Publishing House.
ⓘ Sperrylite
Formula: PtAs2
Reference: Li, X., Zhu, J., Lu, R., Gu, Y., Wu, X., & Chen, Y. (1997). Study on the occurrence of platinum in Xinjie Cu Ni sulfide deposits by a combination of SPM and NAA. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 130(1), 617-622.; Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ Sudburyite
Formula: PdSb
ⓘ Tellurobismuthite
Formula: Bi2Te3
Reference: Zhu, W. G., Zhong, H., Hu, R. Z., Liu, B. G., He, D. F., Song, X. Y., & Deng, H. L. (2010). Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Emeishan Large Igneous Province, SW China. Mineralogy and Petrology, 98(1-4), 167-180.
ⓘ 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.
ⓘ Uraninite
Formula: UO2
Habit: cubes to 1cm
Reference: Xu, Zhengqi, Minghui Yin, Youliang Chen, Lu Xiang, Hao Song, Chengjiang Zhang, Jian Yao, and Hu Guo. (2021) "Genesis of Megacrystalline Uraninite: A Case Study of the Haita Area of the Western Margin of the Yangtze Block, China" Minerals 11, no. 11: 1173. https://doi.org/10.3390/min11111173
ⓘ Wollastonite
Formula: Ca3(Si3O9)
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.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘPlatinum1.AF.10Pt
Group 2 - Sulphides and Sulfosalts
ⓘAltaite2.CD.10PbTe
ⓘBornite2.BA.15Cu5FeS4
ⓘBorovskite2.LA.60Pd3SbTe4
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘErlichmanite2.EB.05aOsS2
ⓘHessite2.BA.60Ag2Te
ⓘLaurite2.EB.05aRuS2
ⓘMerenskyite2.EA.20PdTe2
ⓘMichenerite2.EB.25PdBiTe
ⓘMillerite2.CC.20NiS
ⓘMolybdenite2.EA.30MoS2
ⓘMoncheite2.EA.20Pt(Te,Bi)2
ⓘNickeline2.CC.05NiAs
ⓘPentlandite2.BB.15(NixFey)Σ9S8
ⓘPyrite2.EB.05aFeS2
ⓘPyrrhotite2.CC.10Fe1-xS
ⓘSiegenite2.DA.05CoNi2S4
ⓘSperrylite2.EB.05aPtAs2
ⓘSudburyite2.CC.05PdSb
ⓘTellurobismuthite2.DC.05Bi2Te3
Group 3 - Halides
ⓘFluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
ⓘChromite4.BB.05Fe2+Cr3+2O4
ⓘHaitaite-(La) (TL)4.CC.LaU4+Fe3+2(Ti13Fe2+4Fe3+)O38
ⓘHematite4.CB.05Fe2O3
ⓘHercynite4.BB.05Fe2+Al2O4
ⓘIlmenite4.CB.05Fe2+TiO3
ⓘIshikawaite4.DB.25U4+Fe2+Nb2O8
ⓘMagnetite4.BB.05Fe2+Fe3+2O4
ⓘvar. Titanium-bearing Magnetite4.BB.05Fe2+(Fe3+,Ti)2O4
ⓘvar. Vanadium-bearing Magnetite4.BB.05Fe2+(Fe3+,V3+ )2O4
ⓘ'Pyrochlore Group'4.00.A2Nb2(O,OH)6Z
ⓘQuartz4.DA.05SiO2
ⓘSamarskite-(Y)4.DB.25YFe3+Nb2O8
ⓘUraninite4.DL.05UO2
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
ⓘAlbite9.FA.35Na(AlSi3O8)
ⓘAnorthite9.FA.35Ca(Al2Si2O8)
ⓘArfvedsonite9.DE.25[Na][Na2][Fe2+4Fe3+]Si8O22(OH)2
ⓘEpidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘFayalite9.AC.05Fe2+2SiO4
ⓘFerro-richterite9.DE.20{Na}{CaNa}{Fe2+5}(Si8O22)(OH)2
ⓘForsterite9.AC.05Mg2SiO4
ⓘMuscovite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘvar. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘNepheline9.FA.05Na3K(Al4Si4O16)
ⓘPhlogopite9.EC.20KMg3(AlSi3O10)(OH)2
ⓘRiebeckite9.DE.25◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2
ⓘSodalite9.FB.10Na4(Si3Al3)O12Cl
ⓘThorite9.AD.30Th(SiO4)
ⓘTitanite9.AG.15CaTi(SiO4)O
ⓘWollastonite9.DG.05Ca3(Si3O9)
ⓘZircon9.AD.30Zr(SiO4)
ⓘvar. Cyrtolite9.AD.30Zr[(SiO4),(OH)4]
ⓘvar. Orvillite9.AD.30near 9ZrO2 · 6SiO2 · 5H2O
Unclassified Minerals, Rocks, etc.
ⓘ'Alkali Feldspar'-
ⓘ'Allanite Group'-(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
ⓘ'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ'Apatite'-Ca5(PO4)3(Cl/F/OH)
ⓘ'Bastnäsite'-(Ce/Nd/Y/REE)(CO3)F
ⓘ'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
ⓘ'Chlorite Group'-
ⓘ'Fayalite-Forsterite Series'-
ⓘ'Feldspar Group'-
ⓘ'var. Perthite'-
ⓘ'Fergusonite'-
ⓘ'Hornblende'-
ⓘ'K Feldspar'-
ⓘ'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
ⓘ'Pyroxene Group'-ADSi2O6

List of minerals for each chemical element

HHydrogen
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 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Hⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Hⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hⓘ Pyrochlore GroupA2Nb2(O,OH)6Z
Hⓘ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
Hⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Hⓘ MuscoviteKAl2(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ⓘ Zircon var. Orvillitenear 9ZrO2 · 6SiO2 · 5H2O
Hⓘ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
Hⓘ Arfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
CCarbon
Cⓘ Bastnäsite(Ce/Nd/Y/REE)(CO3)F
OOxygen
Oⓘ Haitaite-(La)LaU4+Fe23+(Ti13Fe42+Fe3+)O38
Oⓘ QuartzSiO2
Oⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
Oⓘ IlmeniteFe2+TiO3
Oⓘ ChromiteFe2+Cr23+O4
Oⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Oⓘ Samarskite-(Y)YFe3+Nb2O8
Oⓘ IshikawaiteU4+Fe2+Nb2O8
Oⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Oⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oⓘ Pyrochlore GroupA2Nb2(O,OH)6Z
Oⓘ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
Oⓘ Magnetite var. Vanadium-bearing MagnetiteFe2+(Fe3+,V3+ )2O4
Oⓘ ForsteriteMg2SiO4
Oⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Oⓘ FluorapatiteCa5(PO4)3F
Oⓘ HercyniteFe2+Al2O4
Oⓘ WollastoniteCa3(Si3O9)
Oⓘ AnorthiteCa(Al2Si2O8)
Oⓘ MagnetiteFe2+Fe23+O4
Oⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Oⓘ FayaliteFe22+SiO4
Oⓘ Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
Oⓘ AegirineNaFe3+Si2O6
Oⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Oⓘ TitaniteCaTi(SiO4)O
Oⓘ ZirconZr(SiO4)
Oⓘ HematiteFe2O3
Oⓘ Bastnäsite(Ce/Nd/Y/REE)(CO3)F
Oⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Oⓘ Riebeckite◻[Na2][Fe32+Fe23+]Si8O22(OH)2
Oⓘ ThoriteTh(SiO4)
Oⓘ Zircon var. Orvillitenear 9ZrO2 · 6SiO2 · 5H2O
Oⓘ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
Oⓘ Arfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
Oⓘ AlbiteNa(AlSi3O8)
Oⓘ SodaliteNa4(Si3Al3)O12Cl
Oⓘ NephelineNa3K(Al4Si4O16)
Oⓘ Pyroxene GroupADSi2O6
Oⓘ UraniniteUO2
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 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Fⓘ FluorapatiteCa5(PO4)3F
Fⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Fⓘ FluoriteCaF2
Fⓘ Bastnäsite(Ce/Nd/Y/REE)(CO3)F
NaSodium
Naⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
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
Naⓘ Arfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
Naⓘ AlbiteNa(AlSi3O8)
Naⓘ SodaliteNa4(Si3Al3)O12Cl
Naⓘ NephelineNa3K(Al4Si4O16)
MgMagnesium
Mgⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Mgⓘ ForsteriteMg2SiO4
Mgⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Mgⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
AlAluminium
Alⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
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 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Alⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Alⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Alⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Alⓘ HercyniteFe2+Al2O4
Alⓘ AnorthiteCa(Al2Si2O8)
Alⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Alⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Alⓘ AlbiteNa(AlSi3O8)
Alⓘ SodaliteNa4(Si3Al3)O12Cl
Alⓘ NephelineNa3K(Al4Si4O16)
SiSilicon
Siⓘ QuartzSiO2
Siⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
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 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Siⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Siⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Siⓘ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
Siⓘ ForsteriteMg2SiO4
Siⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Siⓘ WollastoniteCa3(Si3O9)
Siⓘ AnorthiteCa(Al2Si2O8)
Siⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Siⓘ FayaliteFe22+SiO4
Siⓘ Ferro-richterite{Na}{CaNa}{Fe52+}(Si8O22)(OH)2
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ⓘ ThoriteTh(SiO4)
Siⓘ Zircon var. Orvillitenear 9ZrO2 · 6SiO2 · 5H2O
Siⓘ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
Siⓘ Arfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
Siⓘ AlbiteNa(AlSi3O8)
Siⓘ SodaliteNa4(Si3Al3)O12Cl
Siⓘ NephelineNa3K(Al4Si4O16)
Siⓘ Pyroxene GroupADSi2O6
PPhosphorus
Pⓘ FluorapatiteCa5(PO4)3F
Pⓘ ApatiteCa5(PO4)3(Cl/F/OH)
SSulfur
Sⓘ ChalcopyriteCuFeS2
Sⓘ PyrrhotiteFe1-xS
Sⓘ PyriteFeS2
Sⓘ MilleriteNiS
Sⓘ ErlichmaniteOsS2
Sⓘ LauriteRuS2
Sⓘ SiegeniteCoNi2S4
Sⓘ Pentlandite(NixFey)Σ9S8
Sⓘ BorniteCu5FeS4
Sⓘ MolybdeniteMoS2
ClChlorine
Clⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Clⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Clⓘ SodaliteNa4(Si3Al3)O12Cl
KPotassium
Kⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Kⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Kⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Kⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Kⓘ NephelineNa3K(Al4Si4O16)
CaCalcium
Caⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Caⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Caⓘ FluorapatiteCa5(PO4)3F
Caⓘ WollastoniteCa3(Si3O9)
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ⓘ Haitaite-(La)LaU4+Fe23+(Ti13Fe42+Fe3+)O38
Tiⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
Tiⓘ IlmeniteFe2+TiO3
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 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Tiⓘ TitaniteCaTi(SiO4)O
VVanadium
Vⓘ Magnetite var. Vanadium-bearing MagnetiteFe2+(Fe3+,V3+ )2O4
CrChromium
Crⓘ ChromiteFe2+Cr23+O4
FeIron
Feⓘ Haitaite-(La)LaU4+Fe23+(Ti13Fe42+Fe3+)O38
Feⓘ ChalcopyriteCuFeS2
Feⓘ PyrrhotiteFe1-xS
Feⓘ PyriteFeS2
Feⓘ Pentlandite(NixFey)Σ9S8
Feⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
Feⓘ IlmeniteFe2+TiO3
Feⓘ ChromiteFe2+Cr23+O4
Feⓘ Samarskite-(Y)YFe3+Nb2O8
Feⓘ IshikawaiteU4+Fe2+Nb2O8
Feⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Feⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Feⓘ Magnetite var. Vanadium-bearing MagnetiteFe2+(Fe3+,V3+ )2O4
Feⓘ HercyniteFe2+Al2O4
Feⓘ BorniteCu5FeS4
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
Feⓘ Arfvedsonite[Na][Na2][Fe42+Fe3+]Si8O22(OH)2
CoCobalt
Coⓘ SiegeniteCoNi2S4
NiNickel
Niⓘ MilleriteNiS
Niⓘ NickelineNiAs
Niⓘ SiegeniteCoNi2S4
Niⓘ Pentlandite(NixFey)Σ9S8
CuCopper
Cuⓘ ChalcopyriteCuFeS2
Cuⓘ BorniteCu5FeS4
AsArsenic
Asⓘ NickelineNiAs
Asⓘ SperrylitePtAs2
YYttrium
Yⓘ Samarskite-(Y)YFe3+Nb2O8
Yⓘ Bastnäsite(Ce/Nd/Y/REE)(CO3)F
ZrZirconium
Zrⓘ ZirconZr(SiO4)
Zrⓘ Zircon var. Orvillitenear 9ZrO2 · 6SiO2 · 5H2O
Zrⓘ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
NbNiobium
Nbⓘ Samarskite-(Y)YFe3+Nb2O8
Nbⓘ IshikawaiteU4+Fe2+Nb2O8
Nbⓘ Pyrochlore GroupA2Nb2(O,OH)6Z
MoMolybdenum
Moⓘ MolybdeniteMoS2
RuRuthenium
Ruⓘ LauriteRuS2
PdPalladium
Pdⓘ SudburyitePdSb
Pdⓘ BorovskitePd3SbTe4
Pdⓘ MerenskyitePdTe2
Pdⓘ MicheneritePdBiTe
AgSilver
Agⓘ HessiteAg2Te
SbAntimony
Sbⓘ SudburyitePdSb
Sbⓘ BorovskitePd3SbTe4
TeTellurium
Teⓘ BorovskitePd3SbTe4
Teⓘ MerenskyitePdTe2
Teⓘ MoncheitePt(Te,Bi)2
Teⓘ MicheneritePdBiTe
Teⓘ TellurobismuthiteBi2Te3
Teⓘ HessiteAg2Te
Teⓘ AltaitePbTe
LaLanthanum
Laⓘ Haitaite-(La)LaU4+Fe23+(Ti13Fe42+Fe3+)O38
CeCerium
Ceⓘ Bastnäsite(Ce/Nd/Y/REE)(CO3)F
NdNeodymium
Ndⓘ Bastnäsite(Ce/Nd/Y/REE)(CO3)F
OsOsmium
Osⓘ ErlichmaniteOsS2
PtPlatinum
Ptⓘ SperrylitePtAs2
Ptⓘ PlatinumPt
Ptⓘ MoncheitePt(Te,Bi)2
PbLead
Pbⓘ AltaitePbTe
BiBismuth
Biⓘ MoncheitePt(Te,Bi)2
Biⓘ MicheneritePdBiTe
Biⓘ TellurobismuthiteBi2Te3
ThThorium
Thⓘ ThoriteTh(SiO4)
UUranium
Uⓘ Haitaite-(La)LaU4+Fe23+(Ti13Fe42+Fe3+)O38
Uⓘ IshikawaiteU4+Fe2+Nb2O8
Uⓘ UraniniteUO2

Geochronology

Mineralization age: Phanerozoic : 262 ± 2 Ma to 224 ± 8 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
 Mesozoic
  Triassic
   Late/Upper Triassic
ⓘ Zircon (youngest age)224 ± 8 MaMaomaogou Complex, Miyi County, Panzhihua, Sichuan, China
    
  
 Paleozoic
  Permian
   Lopingian
ⓘ Syenite (youngest age)258 ± 4 MaBaima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, China
ⓘ Syenite (oldest age)259 ± 5 MaBaima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, China
   Guadalupian
ⓘ Gabbro261 ± 2 MaBaima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, China
ⓘ Zircon (oldest age)262 ± 2 MaBaima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, China

Fossils

There are 1 fossil localities from the PaleoBioDB database within this region.

BETA TEST - These data are provided on an experimental basis and are taken from external databases. Mindat.org has no control currently over the accuracy of these data.

Occurrences9
Youngest Fossil Listed466 Ma (Middle Ordovician)
Oldest Fossil Listed479 Ma (Early/Lower Ordovician)
Stratigraphic Units
UnitNo. OccurrencesAge
Hongsiya9478.6 - 466 Ma (Ordovician)
Fossils from RegionClick here to show the list.
Accepted NameHierarchy Age
Asaphellus
genus		Animalia : Arthropoda : Trilobita : Asaphida : Asaphidae : Asaphellus478.6 - 466 Ma
Ordovician
Paramegalaspis
genus		Animalia : Arthropoda : Trilobita : Asaphida : Asaphidae : Paramegalaspis478.6 - 466 Ma
Ordovician
Psilocephalina
genus		Animalia : Arthropoda : Trilobita : Asaphida : Asaphidae : Psilocephalina478.6 - 466 Ma
Ordovician
Taihungshania
genus		Animalia : Arthropoda : Trilobita : Asaphida : Taihungshaniidae : Taihungshania478.6 - 466 Ma
Ordovician
Lingulella
genus		Animalia : Brachiopoda : Lingulata : Lingulida : Obolidae : Lingulella478.6 - 466 Ma
Ordovician
Hesperorthis
genus		Animalia : Brachiopoda : Rhynchonellata : Orthida : Hesperorthidae : Hesperorthis478.6 - 466 Ma
Ordovician
Orthis
genus		Animalia : Brachiopoda : Rhynchonellata : Orthida : Orthidae : Orthis478.6 - 466 Ma
Ordovician
Sinorthis
genus		Animalia : Brachiopoda : Rhynchonellata : Orthida : Orthidae : Sinorthis478.6 - 466 Ma
Ordovician
Didymograptus
genus		Animalia : Hemichordata : Dichograptidae : Didymograptus478.6 - 466 Ma
Ordovician
Fossil LocalitiesClick to show 1 fossil locality

Other Databases

Wikipedia:https://en.wikipedia.org/wiki/Miyi_County
Wikidata ID:Q677700
GeoNames ID:1800429

Localities in this Region

China
China

Other Regions, Features and Areas that Intersect

Asia
Eurasian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.
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