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The western Central Asian Orogenic Belt: A window to accretionary orogenesis and continental growth

文献类型：期刊论文

作者Xiao, Wenjiao1,2; Santosh, M.3,4
刊名GONDWANA RESEARCH
出版日期2014-05-01
卷号25期号:4页码:1429-1444
关键词Multiple arc systems Circum-microcontinent amalgamation Tectonics Continent growth Central Asian Orogenic Belt
ISSN号1342-937X
DOI10.1016/j.gr.2014.01.008
文献子类Review
英文摘要The architecture of accretionary orogens is a key to understand continental growth. Here we present an overview of the orogenic components and their amalgamation in the western Central Asian Orogenic Belt (CAOB). The CAOB records the convergence and interactions among various types of orogenic components including the Japan-type, Mariana-type, and Alaska-Aleutian-type arc systems, as well as the active marginal sequences of the Siberia Craton, which incorporated wide accretionary complexes and accreted arcs and terranes. During construction of the CAOB, the Kazakhstan arc chain was characterized by multiple subduction, whereas the northern fringe of the Tarim Craton remained mostly as a passive margin. The multiple convergence and accretions among these various orogenic components generated huge orogenic collages in the late Paleozoic and even in the early Triassic, involving parallel amalgamation, circum-microcontinent amalgamation and oroclinal bending. The preservation of trapped basins played a significant role in orogenesis with some parts of the oceanic plate being subducted and others behaving as rigid units. The orogenesis in the CAOB was long-lived, lasting for more than 800 m.y., involving multiple-subduction and long, continuous accretion, and featuring the complexity of accretionary orogenesis and continent growth. (C) 2014 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
WOS关键词ZIRCON U-PB ; CARBONIFEROUS VOLCANIC-ROCKS ; PALEOZOIC TECTONIC EVOLUTION ; PHANEROZOIC CRUSTAL GROWTH ; NW CHINA IMPLICATIONS ; NORTH TIEN-SHAN ; INNER-MONGOLIA ; ULTRAHIGH-PRESSURE ; NORTHWESTERN CHINA ; SOUTHERN ALTAIDS
WOS研究方向Geology
语种英语
WOS记录号WOS:000347279400011
出版者ELSEVIER SCIENCE BV
资助机构Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150) ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150) ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150) ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; Major State Basic Research Development Program of China(2014CB44801 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; Chinese Government under the 1000 Talent Plan ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150)
源URL[http://ir.iggcas.ac.cn/handle/132A11/85041]  
专题中国科学院地质与地球物理研究所
通讯作者Xiao, Wenjiao
作者单位1.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.China Univ Geosci Beijing, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
4.Kochi Univ, Fac Sci, Div Interdisciplinary Sci, Kochi 7808520, Japan
推荐引用方式
GB/T 7714		 Xiao, Wenjiao,Santosh, M.. The western Central Asian Orogenic Belt: A window to accretionary orogenesis and continental growth[J]. GONDWANA RESEARCH,2014,25(4):1429-1444.
APA Xiao, Wenjiao,&Santosh, M..(2014).The western Central Asian Orogenic Belt: A window to accretionary orogenesis and continental growth.GONDWANA RESEARCH,25(4),1429-1444.
MLA Xiao, Wenjiao,et al."The western Central Asian Orogenic Belt: A window to accretionary orogenesis and continental growth".GONDWANA RESEARCH 25.4(2014):1429-1444.

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来源：地质与地球物理研究所

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