摘要
Peridotites are an important part of ophiolites： they not only record plate tectonic settings and events, but also offer help to interpret the composition of the mantle and the effect of the deep mantle. The Yarlung-Zangbo suture zone extends more than 2000 km along southern Tibet,
Peridotites are an important part of ophiolites： they not only record plate tectonic settings and events, but also offer help to interpret the composition of the mantle and the effect of the deep mantle. The Yarlung-Zangbo suture zone extends more than 2000 km along southern Tibet,
基金
supported by grants from the Ministry of Science and Technology of China (2014DFR21270)
China Geological Survey (12120115026801, 12120115027201, 201511022)
the Fund from the State Key Laboratory of Continental Tectonics and Dynamics (Z1301-a20)
