Subduction-zone peridotites and their records of crust-mantle interaction

来源：用户分享时间：2025/7/7 16:42:23 本文由

说明：文章内容仅供预览，部分内容可能不全，需要完整文档或者需要复制内容，请下载word后使用。下载word有问题请添加微信号:xxxxxxx或QQ：xxxxxx 处理（尽可能给您提供完整文档），感谢您的支持与谅解。

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

搜索更多关于： Subduction-zone peridotites an 的文档

Subduction-zone peridotites and their records of crust-mantle interaction.doc 将本文的Word文档下载到电脑，方便复制、编辑、收藏和打印

下载这篇word文档

本文链接：https://www.diyifanwen.net/c1q7cf5euz09o8y29wt5t6vudb8bhn000za3_1.html（转载请注明文章来源）