参考文献:1. Bai, W. J., Robinson, P. T., Fang, Q. S., et al., 2000. The PGE and Base-Metal Alloys in the Podiform Chromitites of the Luobusa Ophiolite, Southern Tibet. / The Canadian Mineralogist, 38(3): 585-98 CrossRef 2. Robinson, P. T., Bai, W. J., Malpas, J., et al., 2004, Ultra-High Pressure Minerals in the Luobusa Ophiolite, Tibet, and Their Tectonic Implications. In: Malpas, J., Fletcher, C. J.N., Ali, J. R., et al., eds., Aspects of the Tectonic Evolution of China. / Geological Society Special Publication, 226: 247-72 3. Yang, J. S., Bai, W. J., Fang, Q. S., et al., 2003. Silicon-Rutile—An Ultra-high Pressure (UHP) Mineral from an Ophiolite. / Progress in Natural Science, 13(7): 528-31 4. Yang, J. S., Dobrzhinetskaya, L., Bai, W. J., et al., 2007. Diamond- and Coesite-Bearing Chromitites from the Luobusa Ophiolite, Tibet. / Geology, 35(10): 875-78 CrossRef 5. Yang, J. S., Xu, Z. Q., Li, Z. L., et al., 2009. Discovery of an Eclogite Belt in the Lhasa Block, Tibet: A New Border for Paleo-Tethys / Journal of Asian Earth Sciences, 34: 76-9 CrossRef
作者单位:Jingsui Yang (1) Haibing Li (1) Paul T. Robinson (2)
1. Key Laboratory for Continental Dynamics of the Ministry of Land and Resouces, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037, China 2. Department of Earth Sciences, Dalhousie University, Halifax, NS, B3H 3J5, Canada