Subduction-zone peridotites and their records of
crust-mantle interaction
作者：Jianping ZHENG[1];Qing XIONG[1];Yi ZHAO[1];Wenbo LI[1]; 作者机构：[1]School of Earth Sciences,State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China;[1]School of Earth Sciences,State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China;[1]School of Earth Sciences,State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan
430074,China;[1]School of Earth Sciences,State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China; 来源：中国科学 年：2019 卷：062 期：007
页码：P.1033-1052 页数：20 中图分类：P 正文语种：CHI
关键词：Subduction zone;Ophiolite;Orogenic peridotite;Mantle wedge;Metasomatism;Crust-mantle interaction
摘要：Subduction is the core process of plate tectonics. The mantle wedge in subduction-zone systems represents a key tectonic unit, playing a significant role in material cycling and energy exchange
Subduction-zone peridotites and their records of crust-mantle interaction
