Ophiolitic Chromitites Originated from Ancient SCLM  

作　　者：SHI R. D GRIFFIN W. L O'REILLY S. Y HUANG Q. S LIU D. L GONG X. H CHENG S. S WU K YI G.D 

机构地区：[1]Institute of Tibetan Plateau Research, CAS, Beijing 100101, China [2]GEMOC/CCFS, Earth and Planetary Sciences, Macquarie University, NSW 2109, Australia [3]Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, China

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A02期84-84,共1页地质学报（英文版）

基　　金：supported by the National Basic Research Program of China (2011CB403101);the National Natural Science Foundation of China (41372063 and 41172059)

摘　　要：Ophiolitic chromitites are traditionally considered as the products of melt-mantle interaction in the supra-subduction zone after partial melting of mantle peridotites during upwelling of asthenosphere at oceanic spreading centers.Ophiolitic chromitites are traditionally considered as the products of melt-mantle interaction in the supra-subduction zone after partial melting of mantle peridotites during upwelling of asthenosphere at oceanic spreading centers.

分 类 号：P542[天文地球—构造地质学] P618.3[天文地球—地质学]