中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The crustal velocity structure of the continental deep subduction belt: Study on the eastern Dabie orogen by seismic wide-angle reflection/refraction

文献类型:期刊论文

作者Liu, FT; Xu, PF; Liu, JS; Yin, ZX; Chun, KY; Zhang, XK; Zhang, CK; Zhao, JR
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2003-05-01
卷号46期号:3页码:366-372
关键词continental deep subduction belt Eastern Dabie orogen deep seismic sounding crustal velocity structure
ISSN号0001-5733
文献子类Article
英文摘要Six two-dimensional crustal structure profiles in the eastern Dabie, Anhui Province, have been obtained by the wide-angle reflection/refraction. The results reveal that the crust of the eastern Dabie orogen presents a high-velocity dome, the velocity in the middle- and lower-crust's metamorphic rocks exposed on the surface in the core of the dome approaches 5.0 km/s, the low velocity layers (body) with about 6.1 km/s has developed in upper-middle crust in it's both sides wing, the Moho discontinuity relatively largely varies. and ranges from similar to 41 km in the core to 32 similar to 34 km in both sides, and a 4 km Moho-offset is observed beneath along Xiaotian-Muzitan Fault. We recognize that the eastern Dabie orogen shows a velocity-pattern of typical continent-continent deep subduction/collision style. The Moho offset may be related with the deep subduction of the Yangtze Block, and represents the suture zone between the Yangtze/Sino-Korean Block collision. Therefore, the high-velocity dome may occur by collision/extrusion between the both continental Blocks and the low velocity layers (body) mentioned above may play an important role in the post-collisional crust extension and exhumation of the ultra-high press metamorphic rocks.
WOS关键词ULTRAHIGH-PRESSURE ; METAMORPHIC BELTS ; CENTRAL CHINA ; BENEATH ; COLLISION ; ROCKS
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000183344600014
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/79001]  
专题中国科学院地质与地球物理研究所
通讯作者Liu, FT
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Univ Toronto, Dept Phys, Toronto, ON M5S 2J5, Canada
3.CSB, Res Ctr Explorat Geophys, Zhengzhou 450002, Peoples R China
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Liu, FT,Xu, PF,Liu, JS,et al. The crustal velocity structure of the continental deep subduction belt: Study on the eastern Dabie orogen by seismic wide-angle reflection/refraction[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2003,46(3):366-372.
APA Liu, FT.,Xu, PF.,Liu, JS.,Yin, ZX.,Chun, KY.,...&Zhao, JR.(2003).The crustal velocity structure of the continental deep subduction belt: Study on the eastern Dabie orogen by seismic wide-angle reflection/refraction.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,46(3),366-372.
MLA Liu, FT,et al."The crustal velocity structure of the continental deep subduction belt: Study on the eastern Dabie orogen by seismic wide-angle reflection/refraction".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 46.3(2003):366-372.

入库方式: OAI收割

来源:地质与地球物理研究所

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