Orvillite from Southwest China, China


China
Sichuan Liangshan Yi Dechang County ⓘ Cida intrusion	Hong Zhong, Weiguang Zhu, Zhuyin Chu, Defeng He, and Xieyan Song (2007): Chemical Geology 236(1/2), 112-133.
Panzhihua Miyi County ⓘ Baima V-Ti-Fe deposit	Zhong, H., Campbell, I. H., Zhu, W. G., Allen, C. M., Hu, R. Z., Xie, L. W., & He, D. F. (2011). Timing and source constraints on the relationship between mafic and felsic intrusions in the Emeishan large igneous province. Geochimica et Cosmochimica Acta, 75(5), 1374-1395. Shellnutt, J. G., 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., 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.

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