Two Contrasting Ophiolites in One Suture Zone: a Case Study from East Kunlun Orogenic Belt, North Tibetan Plateau

被引：1
|
作者：
ZHANG Hang [1 ]
MA Changqian [1 ,2 ]
XIONG Fuhao [1 ]
JIANG Hongan [1 ]
LIU Bin [1 ]
GUO Pan [1 ]
机构：
[1] Faculty of Earth Sciences,China University of Geosciences
[2] State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences
来源：
Acta Geologica Sinica(English Edition) | 2015年 / S2期
关键词：
D O I：
暂无
中图分类号：
P542 [构造运动];
学科分类号：
070904 ;
摘要：
Ophiolites are fragments of upper mantle and oceanic crust(Dewey and Bird,1971;Coleman,1977;Nicolas,1989)that were consisting of mantle peridotites and a suite of magmatic rocks.Importantly,ophiolite suite is the key sign for the boundary between two terranes,and could be produced in varied settings,such as continent-continent
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页码：111 / 112
页数：2
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