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Jingsui Yang , Haibing Li , Paul T. Robinson

Journal of Earth Science ›› 2009, Vol. 20 ›› Issue (2) : 205 -208.

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Journal of Earth Science ›› 2009, Vol. 20 ›› Issue (2) : 205 -208. DOI: 10.1007/s12583-009-0020-5
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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

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References

[1]

Bai W. J., Robinson P. T., Fang Q. S., . The PGE and Base-Metal Alloys in the Podiform Chromitites of the Luobusa Ophiolite, Southern Tibet. The Canadian Mineralogist, 2000, 38(3): 585-598.

[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: 247–272

[3]

Yang J. S., Bai W. J., Fang Q. S., . Silicon-Rutile—An Ultra-high Pressure (UHP) Mineral from an Ophiolite. Progress in Natural Science, 2003, 13(7): 528-531.

[4]

Yang J. S., Dobrzhinetskaya L., Bai W. J., . Diamond- and Coesite-Bearing Chromitites from the Luobusa Ophiolite, Tibet. Geology, 2007, 35(10): 875-878.

[5]

Yang J. S., Xu Z. Q., Li Z. L., . Discovery of an Eclogite Belt in the Lhasa Block, Tibet: A New Border for Paleo-Tethys?. Journal of Asian Earth Sciences, 2009, 34: 76-89.

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