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

引用

页码：111 / 112

页数：2

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