中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Late Cenozoic differential uplift-exhumation of batholith and propagation of uplift recorded by fission track thermochronology in Chayu area, the southeast margin of the Tibetan plateau

文献类型:期刊论文

作者Lei YongLiang1,2; Zhong DaLai2; Jia ChengZao3; Ji JianQing4; Zhang Jin5
刊名ACTA PETROLOGICA SINICA
出版日期2008-02-01
卷号24期号:2页码:384-394
关键词fission track uplift-exhumation propagation late miocene chayu area Tibetan Plateau
ISSN号1000-0569
文献子类Article
英文摘要Study on Late Cenozoic propagation of uplift in the southeast margin of the Tibetan Plateau is critical to link with development of intra-continental deformation in the periphery of the Tibetan Plateau. The apatite fission track analysis in Chayu area of the southeast Tibetan Plateau reveals that the Late Cenozoic differential uplift.-exhumation of Demula, Arza Congla and Chayu batholiths, which arrayed from north to south and controlled by faults, is a proxy of propagation of uplift. The time series of uplift-exhumation are ca. 15. 1 similar to 13. 7Ma, 6. 3 similar to 4. 3Ma, 3. 5 similar to 3. 3Ma, 1. 9 similar to 1. 7Ma and 1. 1 similar to 1.0 Ma and the overall activities show southward propagation and migration. It is in Late Miocene (ca. 6 similar to 5Ma) that uplift-exhumation rate turns speedup with a regional response in southeast Tibet and northwest Yunnan and may establish the development pattern of modern terrain for the southeast margin of the Tibetan Plateau. From the southeast. to northeast of the Tibetan Plateau, the outward propagation and growth of late Cenozoic deformation is characterized by multistage, coeval and disequilibrium developments.
WOS关键词LOWER CRUSTAL FLOW ; EASTERN MARGIN ; THERMAL HISTORY ; APATITE ; DEFORMATION ; GROWTH ; BASIN ; DENUDATION ; TECTONICS ; EVOLUTION
WOS研究方向Geology
语种英语
WOS记录号WOS:000259117600018
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/68852]  
专题中国科学院地质与地球物理研究所
通讯作者Lei YongLiang
作者单位1.PetroChina, Key Lab Basin Struct & Petr Accumulat, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.PetroChina Co Ltd, Beijing 100010, Peoples R China
4.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
5.China Earthquake Adm, Inst Geol, Beijing 100029, Peoples R China
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Lei YongLiang,Zhong DaLai,Jia ChengZao,et al. Late Cenozoic differential uplift-exhumation of batholith and propagation of uplift recorded by fission track thermochronology in Chayu area, the southeast margin of the Tibetan plateau[J]. ACTA PETROLOGICA SINICA,2008,24(2):384-394.
APA Lei YongLiang,Zhong DaLai,Jia ChengZao,Ji JianQing,&Zhang Jin.(2008).Late Cenozoic differential uplift-exhumation of batholith and propagation of uplift recorded by fission track thermochronology in Chayu area, the southeast margin of the Tibetan plateau.ACTA PETROLOGICA SINICA,24(2),384-394.
MLA Lei YongLiang,et al."Late Cenozoic differential uplift-exhumation of batholith and propagation of uplift recorded by fission track thermochronology in Chayu area, the southeast margin of the Tibetan plateau".ACTA PETROLOGICA SINICA 24.2(2008):384-394.

入库方式: OAI收割

来源:地质与地球物理研究所

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