雷琼地区地壳及浅部地慢结构的背景噪声层析成像(英文)

雷琼地区地壳及浅部地慢结构的背景噪声层析成像(英文)

论文摘要

<正>The region of Leizhou Peninsula and Hainan Island in Southern China, or Lei-Qiong for short, has seen extensive volcanic activities since late Cenozoic. Several lines of evidence from geophysics and geochemistry indicate the Hainan mantle plume, which likely originates from the lower mantle, is responsible for the large-flux, intraplate volcanisms in this region. However, the interactions between the rising mantle materials and the overlaying plate, in particular how surface volcanos connect with their deep

论文目录

文章来源

类型: 国内会议

作者: Mohan Pan,TIing Yang,Yuhang Dai,Le Ba Manh

来源: 2019年中国地球科学联合学术年会 2019-10-27

年度: 2019

分类: 基础科学

专业: 地质学

单位: Southern University of Science and Technology,Tongji University

分类号: P542

DOI: 10.26914/c.cnkihy.2019.064293

页码: 75

总页数: 1

文件大小: 899k

下载量: 1

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雷琼地区地壳及浅部地慢结构的背景噪声层析成像(英文)
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