中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Slip partitioning in the northeast Pamir-Tian Shan convergence zone

文献类型:期刊论文

作者Fu, Bihong1; Ninomiya, Yoshiki2; Guo, Jianming
刊名TECTONOPHYSICS
出版日期2010-03-10
卷号483期号:3-4页码:344-364
关键词Late Cenozoic Slip Partitioning Intracontinental Mountain Building Pamir-tian Shan Convergence Zone India-eurasia Collision
ISSN号0040-1951
DOI10.1016/j.tecto.2009.11.003
文献子类Article
英文摘要Based on a detailed analysis of satellite imagery combined with field geologic and geomorphic observations, we have mapped late Cenozoic folds and faults in the northeastern Pamir-Tian Shan convergence zone. It is a unique example to understand intracontinental ongoing mountain building within India-Eurasia collision system. in the front of northeastern Pamir, our investigations reveal that the NW-WNW-trending folds display a right-stepping en echelon pattern and NW-WNW-striking faults are mainly characterized by south-dipping thrusts with an extensive dextral strike-slip component. Drainage systems across the active faults show a systematic right-lateral offset. In contrast, structural style of the ENE trending fold-and-thrust belts are predominated by south-north directed shortening southwest of the Tian Shan. Our results also infer that oblique thrusting accommodates as long-term dextral slip rate of ca. 4.0 mm/yr during the late Cenozoic time north of the Pamir topographic front. Tectono-stratigraphic evidence suggests that the tectonic deformation was initiated at ca. 3-5 Ma in the study area. We suggest that intracontinental mountain building in the Pamir-Tian Shan convergence zone should be attributed to the crustal shortening caused by folding and thrusting as well as block rotation related to strike-slip faulting within the India-Eurasia collision system. (C) 2009 Elsevier B.V. All rights reserved.
WOS关键词POSITIONING SYSTEM MEASUREMENTS ; DAY CRUSTAL DEFORMATION ; EURASIA COLLISION ZONE ; INDIA-ASIA COLLISION ; TIEN-SHAN ; TARIM BASIN ; KARAKORAM FAULT ; NORTHWEST CHINA ; STRUCTURAL FEATURES ; REGIONAL TECTONICS
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000275927000012
出版者ELSEVIER SCIENCE BV
资助机构NSFC(40721003) ; NSFC(40721003) ; Chinese Academy of Sciences(KZCX2-YW-12) ; Chinese Academy of Sciences(KZCX2-YW-12) ; NSFC(40721003) ; NSFC(40721003) ; Chinese Academy of Sciences(KZCX2-YW-12) ; Chinese Academy of Sciences(KZCX2-YW-12) ; NSFC(40721003) ; NSFC(40721003) ; Chinese Academy of Sciences(KZCX2-YW-12) ; Chinese Academy of Sciences(KZCX2-YW-12) ; NSFC(40721003) ; NSFC(40721003) ; Chinese Academy of Sciences(KZCX2-YW-12) ; Chinese Academy of Sciences(KZCX2-YW-12)
源URL[http://ir.iggcas.ac.cn/handle/132A11/72999]  
专题中国科学院地质与地球物理研究所
通讯作者Fu, Bihong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Div Tibetan Plateau Res, Key Lab Earths Deep Interior, Beijing 100029, Peoples R China
2.Natl Inst Adv Ind Sci & Technol, Geol Survey Japan, Tsukuba, Ibaraki 3058567, Japan
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Fu, Bihong,Ninomiya, Yoshiki,Guo, Jianming. Slip partitioning in the northeast Pamir-Tian Shan convergence zone[J]. TECTONOPHYSICS,2010,483(3-4):344-364.
APA Fu, Bihong,Ninomiya, Yoshiki,&Guo, Jianming.(2010).Slip partitioning in the northeast Pamir-Tian Shan convergence zone.TECTONOPHYSICS,483(3-4),344-364.
MLA Fu, Bihong,et al."Slip partitioning in the northeast Pamir-Tian Shan convergence zone".TECTONOPHYSICS 483.3-4(2010):344-364.

入库方式: OAI收割

来源:地质与地球物理研究所

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