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  4. 岩石圈演化国家重点实验室
Crustal structure along the Wanzai-Yongchun profile in the Cathaysia Block, Southeast China, constrained by a joint active- and passive-source seismic experiment

文献类型：期刊论文

作者Huang, Minfu2,3; Xu, Tao1,3; Lu, Qingtian7; Lin, Jiyan2,3,6; Bai, Zhiming1,3; Deng, Yangfan5; Zhang, Yongqian7; Badal, Jose4
刊名GEOPHYSICAL JOURNAL INTERNATIONAL
出版日期2022-06-21
卷号231期号:1页码:384-393
关键词Joint inversion Image processing Crustal imaging Crustal structure Asia
ISSN号0956-540X
DOI10.1093/gji/ggac198
英文摘要Since the Mesozoic, the South China Block (SCB) has experienced multiple episodes of tectonic magmatism accompanied by metallogenesis. To explore the seismic velocity structure of the crust and its connection with mineralization, we constructed a wide-angle reflection and refraction (WARR) profile by deploying 435 short-period seismometers across the Cathaysia Block in Southeast China. Receiver functions and the H-kappa stacking method were applied using a reference 2-D velocity model obtained from the analysis of WARR data. Integration of active- and passive-source seismic data enabled us to obtain an image of the crust and the average Vp/Vs ratio value of the SCB and produce several results: (1) The crustal thickness varies west-to-east from 28 km below the Qinhang metallogenic belt to 32 km below the Wuyishan metallogenic belt, and the average value of the Vp/Vs ratio for the crust is 1.71. Both the thickness of the crust and the average Vp/Vs ratio are lower than the average global values for the continental crust. (2) The relatively low Vp/Vs ratio and thin crust along the profile could be generated by thinning of the lower crust in the SCB as a result of the backarc extension related to westward subduction of the Paleo-Pacific plate below East Asia. (3) The Moho depth estimated from H-kappa stacking with the help of the background P-wave velocity model modified by the WARR model fits better than using a global seismic velocity model with its common conversion point image, which supports a potential seismic data analysis technique provided with a joint deployment of both active- and passive-source seismic observation system with a shorter period.
WOS关键词MANTLE STRUCTURE BENEATH ; RECEIVER FUNCTIONS ; VELOCITY STRUCTURE ; MOHO DEPTH ; THICKNESS ; PETROGENESIS ; GEODYNAMICS ; ORIGIN ; ROCKS ; RATIO
资助项目National Key Research and Development Program of China[2016YFC0600201] ; National Natural Science Foundation of China[42130807] ; National Natural Science Foundation of China[41774097] ; National Natural Science Foundation of China[41974048]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000814811100006
出版者OXFORD UNIV PRESS
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/105895]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Xu, Tao; Lu, Qingtian
作者单位1.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
4.Univ Zaragoza, Phys Earth, Pedro Cerbuna 12, Zaragoza 50009, Spain
5.Chinese Acad Sci, Staie Key Lab Isotope Geochem, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China
6.China Earthquake Adm, Geophys Explorat Ctr, Zhengzhou 450002, Peoples R China
7.Chinese Acad Geol Sci, Beijing 100037, Peoples R China
推荐引用方式
GB/T 7714		 Huang, Minfu,Xu, Tao,Lu, Qingtian,et al. Crustal structure along the Wanzai-Yongchun profile in the Cathaysia Block, Southeast China, constrained by a joint active- and passive-source seismic experiment[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2022,231(1):384-393.
APA Huang, Minfu.,Xu, Tao.,Lu, Qingtian.,Lin, Jiyan.,Bai, Zhiming.,...&Badal, Jose.(2022).Crustal structure along the Wanzai-Yongchun profile in the Cathaysia Block, Southeast China, constrained by a joint active- and passive-source seismic experiment.GEOPHYSICAL JOURNAL INTERNATIONAL,231(1),384-393.
MLA Huang, Minfu,et al."Crustal structure along the Wanzai-Yongchun profile in the Cathaysia Block, Southeast China, constrained by a joint active- and passive-source seismic experiment".GEOPHYSICAL JOURNAL INTERNATIONAL 231.1(2022):384-393.

入库方式： OAI收割

来源：地质与地球物理研究所

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