Luobusa-Ophiolith

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• Minerals (131)
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• Rocks (12)
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Literatur:

• Bai, W.J., Zhou, M.F., Robinson, P.T., et al. (1993): Possible diamond-bearing mantle peridotites and chromites in the Luobusa and Dongqiao ophiolites, Tibet. Can. J. Earth Sciences 30, 1650-59.
• Zhou, M., Robinson, P.T., Malpas, J., and Li Zijin (1996): Podiform Chromitites in the Luobusa Ophiolite (S Tibet): Implications for Melt-Rock Interaction and Chromite Segregation in the Upper Mantle. J. Petrol. 37(1), 3-21.
• Bai, W. et al. (2000): The PGE and base-metal alloys in the podiform chromitites of the Luobusa ophiolite, S Tibet. Can. Min. 38(3), 585-98. http://pubs.nrc-cnrc.gc.ca/mineral/mineral38/58538-3.pdf
• Bai, W.J., Zhou, M.F., and Fang, Q.S. (2000): Origin of podiform chromitites, diamonds and associated mineral assemblage in the Luobusha ophiolite, Tibet. Seismological Press (Beijing), 98 S.
• Bai, W.J., Fang, Q.S., Zhang, Z.M., et al. (2001): Crystal structure of forstertite from podiform chromitite in Luobusha ophiolite of Tibet and its implications. Acta Petrol. et Mineral. 20(1), 1-9.
• Bai, W.J., Yang, J.S., Fang, Q.S., et al. (2001): Study on a storehouse of ultrahigh pressure mantle minerals - podiform chromite deposits. Earth Science Frontiers 8(3), 111-21.
• Aitchison, J.C. et al. (2002): New insights into the evolution of the Yarlung Tsangpo suture zone, Xizang (Tibet), China. Episodes 25(2), 90-94. http://www.episodes.org/backissues/252/090-94%20Hongkong.pdf
• Bai, W., J. Yang, Q.Fang & B. Yan (2003): An unusual mantle mineral group in ophiolite, Tibet. Pres. Alice Wain Memorial W. Norway Eclogite Field Symp., Selje, Norway, June 21-28 2003. http://www.ngu.no/FileArchive/165/2003_055.pdf
• Yang, J., W. Bai, Q. Fang, B. Yan, H. Rong, and Robinson, P. (2003): Newly discovered coesite-kyanite aggregates in the Luobusa ophiolite, S Tibet, China, originated from exhumed mantle? Pres. Alice Wain Memorial W Norway Eclogite Field Symp., Selje, Norway, June 21-28 2003. http://www.ngu.no/FileArchive/165/2003_055.pdf
• Zhou, M.F., Robinson, P.T., Malpas, J., Edwards, S.J. and Qi, L., (2005). REE and PGE geochemical constraints on the formation of dunites in the Luobusa ophiolite, Southern Tibet. J. Petrol., v.46, S.615–39.
• Bai, W., N. Shi, Q. Fang, G. Li, M. Xiong, J. Yang, and H. Rong (2006): Luobusaite: A New Mineral. Acta Geol. Sinica 80(5), 656-59. (Typ-Publ.)
• Weiß, S. (2007). Neue Mineralien: Luobosait. Lapis, Jg.32, Nr.5, S.45+54.
• Yang, J.S., Dobrzhinetskaya, L., Bai, W.J. et al. (2007). Diamond- and coesite-bearing chromitites from the Luobusa ophiolite, Tibet. Geology. doi:10.1130/G23766A.1
• Weiß, S. (2008). Korrektur Luobosait. Lapis, Jg.33, Nr.1, S.8+58.
• Fang, Q. et al. (2009). Qusongit. Amer. Min. 94, 387-90. (Typ-Publ.)
• Shi, N. et al. (2009). Yarlongit. Acta Geol. Sinica 83 (1), 52-56. (Typ-Publ.)
• Li, G. et al. (2009). Zangboit. Can. Min.47, 1265-74. (Typ-Publ.)
• Yamamoto, S., Komiya, T., Hirose, K., Maruyama, S. (2009). Coesite and clinopyroxene exsolution lamellae in chromites: In-situ ultrahigh-pressure evidence from podiform chromitites in the Luobusa ophiolite, southern Tibet. Lithos. doi:10.1016/j.lithos.2008.05.003
• Xiong, F. et al. (2014). Different type of chromitite and genetic model from Luobusa ophiolite. Tibet. Acta Petrol. Sinica, v.30, S.2137–63.
• Xu, X.Z., Yang, J.S., Robinson, P.T. et al. (2015). Origin of ultrahigh pressure and highly reduced minerals in podiform chromitites and associated mantle peridotites of the Luobusa ophiolite, Tibet. Gondwana Res. doi:10.1016/j.gr.2014.05.010
• Wang, Y. et al. (2023): Tennantite-(Ni), Cu6(Cu4Ni2)As4S13, from Luobusa ophiolite, Tibet, China: a new Ni member of the tetrahedrite group. Min. Mag., Vol.87, Nr.4, S.591-98. doi:10.1180/mgm.2023.41 (Typ-Publ.)
• Wang, Y. et al. (2023): Tetrahedrite-(Ni), Cu6(Cu4Ni2)Sb4S13, the first nickel member of tetrahedrite group mineral from Luobusa chromite deposits, Tibet, China. Am. Min., Vol.108, Nr.10, S.1984-1992. (Typ-Publ.)