Late Ordovician to Early Silurian Tectonic Events in the Himalayan Terrain

被引:0
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作者
GAO Li'e [1 ]
ZENG Lingsen [1 ]
HU Guyue [2 ]
WANG Yuhua [1 ,3 ]
GAO Jiahao [1 ,4 ]
SHANG Zhen [1 ,4 ]
WANG Yaying [1 ]
机构
[1] Institute of Geology, Chinese Academy of Geological Sciences
[2] Institute of Mineral Resources, Chinese Academy of Geological Sciences
[3] School of Earth and Space Sciences, Peking University
[4] China University of Geosciences
基金
美国国家科学基金会;
关键词
Late Ordovician to Early Silurian Tectonic Events in the Himalayan Terrain; ICP;
D O I
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中图分类号
P542 [构造运动];
学科分类号
摘要
Objective The Himalaya terrain together with the ribbon terrains(e.g.,Lhasa,Qiangtang,and Sibumasu blocks)of the Gondwana supercontinent has experienced episodic tectonic events since the Neoproterozoic.However,almost not any documentation with regard to the tectonic processes links the peri-Gondwana subduction between
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页码:1049 / 1050
页数:2
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