中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
East-west crustal structure and "down-bowing" Moho under the northern Tibet revealed by wide-angle seismic proflle

文献类型:期刊论文

作者Zhang, ZJ; Li, YK; Wang, GJ; Teng, JW; Klemperer, S; Li, JW; Fan, JY; Chen, Y
刊名SCIENCE IN CHINA SERIES D-EARTH SCIENCES
出版日期2002-06-01
卷号45期号:6页码:550-558
ISSN号1006-9313
关键词northern Tibet wide-angle seismic profile P- and S-wave velocity Poisson's ratio "down-bowing" Moho eastward flow of materials
文献子类Article
英文摘要We recognized 6 sets of reflecting P- and S-wave events from Moho and other interfaces within the crust, respectively, with the wide-angle seismic data acquired from 510 km-long Selincuo-Ya'anduo profile in the northern Tibet, fitted the observed events with forward modeling, and interpreted crustal structure of P- and S-wave velocities and Poisson's ratio under the profile. The results demonstrate that the crustal structure between Yarlungzangbo and Bangong-Nujiang sutures changes abruptly, and the crust is the thickest at the middle part of the profile with thickness of 80 km or more. The "down-bowing" Moho is the striking feature for the crustal variation along the west-east direction. The Moho uplifts with steps, and the uplifting rate westward is greater than that eastward. The heterogeneity of P- and S-wave velocities exists both vertically and horizontally, and one lower velocity layer (LVL) exists with the depth range of 27-34 km and the thickness range of 5-7 km. For the upper crust, Poisson's ratio is the lowest at the middle part of the profile; for the lower crust, the Poisson's ratio at the east segment is lower than that at west segment, which means that the crustal rigidity for the upper crust is different from the lower crust, and the lower crust under the east segment of the profile is more ductile. We infer that the substance in the lower crust endured eastward flow along with the collision between Eurasian and Indian plates, and the "down-bowing" Moho is attributable to the multi-phase E-W tectonic processes.
WOS关键词SOUTHERN TIBET ; PLATEAU ; BENEATH ; TRAVERSE
WOS研究方向Geology
语种英语
出版者SCIENCE CHINA PRESS
WOS记录号WOS:000175593200008
源URL[http://ir.iggcas.ac.cn/handle/132A11/77587]  
专题中国科学院地质与地球物理研究所
通讯作者Zhang, ZJ
作者单位1.Acad Sinica, Inst Geol & Geophys, Beijing 100101, Peoples R China
2.Minist Land & Resources, Acad Geol Sci, Yanjiao 101601, Peoples R China
3.Stanford Univ, Dept Geophys, Stanford, CA 94305 USA
推荐引用方式
GB/T 7714
Zhang, ZJ,Li, YK,Wang, GJ,et al. East-west crustal structure and "down-bowing" Moho under the northern Tibet revealed by wide-angle seismic proflle[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2002,45(6):550-558.
APA Zhang, ZJ.,Li, YK.,Wang, GJ.,Teng, JW.,Klemperer, S.,...&Chen, Y.(2002).East-west crustal structure and "down-bowing" Moho under the northern Tibet revealed by wide-angle seismic proflle.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,45(6),550-558.
MLA Zhang, ZJ,et al."East-west crustal structure and "down-bowing" Moho under the northern Tibet revealed by wide-angle seismic proflle".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 45.6(2002):550-558.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。