The Lithospheric Structure in the South China Block from Receiver Function: Implications for the Source of Mineral System

被引：0

作者：

CHEN Changxin ^{[1
,2
,3
]}

LV Qingtian ^{[1
,2
]}

CHEN Ling ^{[4
,5
,6
]}

SHI Danian ^{[1
,2
]}

YAN Jiayong ^{[1
,2
]}

AI Yinshuang ^{[6
,7
]}

机构：

[1] Chinese Academy of Geological Sciences

[2] Sino Probe Center, Chinese Academy of Geological Sciences and China Geological Survey

[3] Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences

[4] State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences

[5] CAS Center for Excellence in Deep Earth Science

[6] University of Chinese Academy of Sciences

[7] Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences

来源：

Acta Geologica Sinica(English Edition) | 2021年 / S1期

基金：

中国国家自然科学基金;

关键词：

D O I：

暂无

中图分类号：

P31 [大地（岩石界）物理学（固体地球物理学）]; P57 [矿物学];

学科分类号：

070801 ; 070901 ;

摘要：

The South China block(SC), composed of Cathaysia(CA), Jiangnan Orogenic belt(JNB), and Yangtze block(YB), is one of the most important poly-metallic metallogenic provinces in the world(Zhang et al., 2013), containing of four famous major Mesozoic metallogenic belts, involving the Middle-Lower Yangtze Fe-Cu-Au metallogenic belt(MYMB),

引用

页码：28 / 30

页数：3

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