Modification of the High-Pressure-Type Chromites into the Low-Pressure-Type: Petrological Investigation of the Podiform Chromitites in the Luobusa Ophiolite, Tibet  

作　　者：YAMAMOTO Shinji KOMIYA Tsuyoshi MARUYAMA Shigenori 

机构地区：[1]Graduate School of Arts and Sciences, The University of Tokyo [2]ELSI (Earth-Life Science Institute), Tokyo Institute of Technology

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A02期104-104,共1页地质学报（英文版）

摘　　要：The podiform chromitites in the Luobusa ophiolite, Southem Tibet, have received much attention because of the presence of ultrahigh-pressure minerals, such as micro- diamonds （Bai et al., 1993; Yang et al., 2007; Xu et al.,The podiform chromitites in the Luobusa ophiolite, Southem Tibet, have received much attention because of the presence of ultrahigh-pressure minerals, such as micro- diamonds （Bai et al., 1993; Yang et al., 2007; Xu et al.,

分 类 号：P618.3[天文地球—矿床学]