中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A thin-skinned collisional model for the Taiwan orogeny

文献类型:期刊论文

作者Ding, ZY; Yang, YQ; Yao, ZX; Zhang, GH
刊名TECTONOPHYSICS
出版日期2001-03-15
卷号332期号:3页码:321-331
关键词Taiwan orogeny collision of plates global positioning data finite-element method
ISSN号0040-1951
文献子类Article
英文摘要The thin-skinned tectonics model was often used for the collision orogeny of Taiwan. However, the suture zone of collision and faulting were not included in that model. It is not convenient for understanding the pattern of the plate collision around Taiwan and the contributions of collision and faulting to the mountain building. Moreover, thr results obtained from the thin-skinned tectonics model cannot be compared with the GPS (Global Positioning System) data across the suture zone of collision. Based on a number of recent studies, we present a different model, called the thin-skinned collisional model, for the Taiwan orogeny as an attempt at solving the problems mentioned above. The model differs from the existing thin-skinned tectonics model for Taiwan mainly in that it has: included the suture tent: of the plate collision and faulting in the thin-skinned block, and thus enables us to probe into the collision pattern and to compare it with the GPS data. Several arguments are put forward to support this model. The model is theoretically tested by the use of the elasto-plastic finite-element method. From the computed results we find that the model fits the observation data well. for they can reproduce the velocity distribution measured by GPS and the major topography features of Taiwan. In particular, the computed results suggest. at least theoretically, that the Longitudinal Valley of eastern Taiwan would be a ramp valley and its western boundary fault would be the collision boundary between the Eurasian plate and the Philippine Sea plate. Taking the theoretical results into account, a new type of plate convergence boundary in the Longitudinal Valley area could emerge from the thin-skinned collisional model. (C) 2001 Elsevier Science B.V. All rights reserved.
WOS关键词EVOLUTIONARY MODEL ; DEFORMATION ; ARC ; GEODYNAMICS ; CONSTRAINTS ; BUDGET ; GPS
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000168595700002
出版者ELSEVIER SCIENCE BV
源URL[http://ir.iggcas.ac.cn/handle/132A11/77029]  
专题中国科学院地质与地球物理研究所
通讯作者Ding, ZY
作者单位1.Peking Univ, Dept Geol, Beijing 100871, Peoples R China
2.China Seismol Bur, Inst Geol, Beijing 100029, Peoples R China
3.Acad Sinica, Inst Geophys, Beijing 100101, Peoples R China
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GB/T 7714
Ding, ZY,Yang, YQ,Yao, ZX,et al. A thin-skinned collisional model for the Taiwan orogeny[J]. TECTONOPHYSICS,2001,332(3):321-331.
APA Ding, ZY,Yang, YQ,Yao, ZX,&Zhang, GH.(2001).A thin-skinned collisional model for the Taiwan orogeny.TECTONOPHYSICS,332(3),321-331.
MLA Ding, ZY,et al."A thin-skinned collisional model for the Taiwan orogeny".TECTONOPHYSICS 332.3(2001):321-331.

入库方式: OAI收割

来源:地质与地球物理研究所

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