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Volume 20 Issue 2
Apr 2009
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Jingsui Yang, Haibing Li, Paul T Robinson. Foreword. Journal of Earth Science, 2009, 20(2): 205-208. doi: 10.1007/s12583-009-0020-5
Citation: Jingsui Yang, Haibing Li, Paul T Robinson. Foreword. Journal of Earth Science, 2009, 20(2): 205-208. doi: 10.1007/s12583-009-0020-5

Foreword

doi: 10.1007/s12583-009-0020-5
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  • 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): 585–598 doi: 10.2113/gscanmin.38.3.585
    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: 247–272
    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): 528–531 doi: 10.1080/10020070312331343970
    Yang, J. S., Dobrzhinetskaya, L., Bai, W. J., et al., 2007. Diamond- and Coesite-Bearing Chromitites from the Luobusa Ophiolite, Tibet. Geology, 35(10): 875–878 doi: 10.1130/G23766A.1
    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: 76–89 doi: 10.1016/j.jseaes.2008.04.001
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