岩浆如何链接地球深部过程与浅部系统？

郑建平; 马强; 苏玉平; 陈明; 平先权; 戴宏坤

doi:10.3799/dqkx.2022.805

岩浆如何链接地球深部过程与浅部系统？

doi: 10.3799/dqkx.2022.805

郑建平^{1, 2,},
马强^{1, 2},
苏玉平¹,
陈明¹,
平先权¹,
戴宏坤²

1.
中国地质大学地球科学学院, 湖北武汉 430074
2.
中国地质大学地质过程与矿产资源国家重点实验室, 湖北武汉 430078

详细信息

作者简介:
郑建平(1964-), 男，教授，主要研究深源岩石与岩石圈演化.E-mail: jpzheng@cug.edu.cn

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出版历程
- 刊出日期: 2022-10-25

How does the Magma Link the Earth Deep Process with the Shallow System？

摘要

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参考文献(14)

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[13]	郑建平, 戴宏坤, 2018. 西太平洋板片俯冲与后撤引起华北东部地幔置换并导致陆内盆-山耦合. 中国科学: 地球科学, 48(4): 436-456. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201804004.htm
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