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),
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页码：28 / 30
页数：3
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