Structures and detrital zircon ages of the Devonian-Permian Tarbagatay accretionary complex in west Junggar, China: imbricated ocean plate stratigraphy and implications for amalgamation of the CAOB
文献类型：期刊论文
| 作者 | Chen, Yichao1,2; Xiao, Wenjiao1,3,4; Windley, Brian F.5; Zhang, Ji'en3; Zhou, Kefa1; Sang, Miao1,2 |
| 刊名 | INTERNATIONAL GEOLOGY REVIEW
 |
| 出版日期 | 2017 |
| 卷号 | 59期号:9页码:1097-1115 |
| 关键词 | Western Junggar melange coherent unit detrital zircon age CAOB |
| ISSN号 | 0020-6814 |
| DOI | 10.1080/00206814.2016.1185652 |
| 文献子类 | Article |
| 英文摘要 | The Tarbagatay Complex, located in northwest Junggar, is situated tectonically between the Zharma-Saur arc to the north and the Tacheng terrane and the Boshchekol-Chingiz arc to the south. This Complex belt is variably composed of ophiolitic melange, sedimentary melange, and coherent units of turbidites and shallow water sediments. These rocks crop out in fault-bound slices with fault-parallel asymmetric folds. Both the lithologies and deformation features of the Tarbagatay Complex suggest an accretionary origin generally with a top-to-the-south tectonic vergence, suggesting N-dipping subduction beneath the Zharma-Saur arc. The presence of a former ocean is indicated by the Ordovician ophiolite melanges and related marine fossils. The time duration of the Tarbagatay Complex can be bracketed by detrital zircon ages of turbidites and shallow water sediments with a lower limit of major peak ages of 350-370Ma, and an upper limit of middle Permian indicated by detrital zircon ages of 262.3Ma. Based on these data, we suggest that the subduction of the Tarbagatay Ocean likely started in the Late Devonian and lasted until the middle Permian. Taking into account the formation of the northern part of the Kazakhstan orocline, which has a similar temporal-spatial framework, we propose a tectonic model for the western CAOB that involves accretion and amalgamation from the Ordovician to the middle Permian. |
| WOS关键词 | ASIAN OROGENIC BELT ; CONTINENTAL-CRUST ; JAPANESE ISLANDS ; NW CHINA ; SUBDUCTION ; XINJIANG ; GROWTH ; PALEOGEOGRAPHY ; TECTONICS ; EVOLUTION |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000402857500004 |
| 出版者 | TAYLOR & FRANCIS INC |
| 资助机构 | National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Major State Basic Research Development Programme of China(2014CB44801) ; Major State Basic Research Development Programme of China(2014CB44801) ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41202150 ; 41202150 ; 41472208 ; 41472208 ; 41102132) ; 41102132) ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Major State Basic Research Development Programme of China(2014CB44801) ; Major State Basic Research Development Programme of China(2014CB44801) ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41202150 ; 41202150 ; 41472208 ; 41472208 ; 41102132) ; 41102132) ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Major State Basic Research Development Programme of China(2014CB44801) ; Major State Basic Research Development Programme of China(2014CB44801) ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41202150 ; 41202150 ; 41472208 ; 41472208 ; 41102132) ; 41102132) ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Major State Basic Research Development Programme of China(2014CB44801) ; Major State Basic Research Development Programme of China(2014CB44801) ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; One Hundred Talent Programme B of the Chinese Academy of Sciences ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41202150 ; 41202150 ; 41472208 ; 41472208 ; 41102132) ; 41102132) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/52888]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 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.Univ Chinese Acad Sci, Beijing, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 4.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China 5.Univ Leicester, Dept Geol, Leicester, Leics, England |
| 推荐引用方式 GB/T 7714 | Chen, Yichao,Xiao, Wenjiao,Windley, Brian F.,et al. Structures and detrital zircon ages of the Devonian-Permian Tarbagatay accretionary complex in west Junggar, China: imbricated ocean plate stratigraphy and implications for amalgamation of the CAOB[J]. INTERNATIONAL GEOLOGY REVIEW,2017,59(9):1097-1115. |
| APA | Chen, Yichao,Xiao, Wenjiao,Windley, Brian F.,Zhang, Ji'en,Zhou, Kefa,&Sang, Miao.(2017).Structures and detrital zircon ages of the Devonian-Permian Tarbagatay accretionary complex in west Junggar, China: imbricated ocean plate stratigraphy and implications for amalgamation of the CAOB.INTERNATIONAL GEOLOGY REVIEW,59(9),1097-1115. |
| MLA | Chen, Yichao,et al."Structures and detrital zircon ages of the Devonian-Permian Tarbagatay accretionary complex in west Junggar, China: imbricated ocean plate stratigraphy and implications for amalgamation of the CAOB".INTERNATIONAL GEOLOGY REVIEW 59.9(2017):1097-1115. |
入库方式： OAI收割
来源：地质与地球物理研究所
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