Tectonic-magmatic framework identified by remote sensing analyses and geochronology in West Junggar, Central Asian Orogenic Belt
文献类型:期刊论文
作者 | Zhang, Guo-Liang5,7; Hong, Tao1,6; Xu, Xing-Wang2,3,7; Wu, Chu4,7; Li, Hao7; Chen, Yuan-Wei5 |
刊名 | GEOLOGICAL JOURNAL |
出版日期 | 2020-11-03 |
页码 | 18 |
ISSN号 | 0072-1050 |
关键词 | Darbut Fault Remote sensing analyses Tectonic evolution West Junggar |
DOI | 10.1002/gj.4028 |
英文摘要 | The temporal and spatial evolutions of the Darbut Fault deformation patterns were analysed for multiple deformation stages in this study by using a regional geological survey, quantitative remote sensing image analyses, and structural analyses. Remote sensing images indicating that the Karamay granitoid batholith is greenish-grey, the Hongshan granitoid batholith is yellowish-green along the Darbut Fault, and the Miaoergou, Akebasitao, and Hatu granitoid batholiths are round in shape and luminous yellow colour. The remote sensing images of the Darbut Fault, Hongshan granitoid batholith, and data from previous research suggest that the upright folds (F-1) in the Carboniferous strata near the Darbut Fault and northeast-southwest (NE-SW) striking sub-vertical dextral shear zones in the melanges represent the regional dextral strike-slip shear zones. The NE-SW striking transcurrent sinistral strike-slip faults and 'S-shaped' drag folds (F-2) overprinted the dextral shear zones. The Hongshan batholith is a complex pluton, which was composed of alkaline feldspar granite, syenite granite, and monzogranite. The LA-ICP-MS U-Pb 311-307 Ma of zircons from the ductilely deformed Hongshan alkaline feldspar granite and monzogranites are formed during the dextral shear zone of the Darbut Fault. The 302 Ma Hongshan alkaline feldspar granite is contemporarily formed during the sinistral strike-slip stage of the Darbut Fault. The Hongshan complex pluton has a prolonged formation age and witnesses the whole process of ocean-land conversion from the capture of island arc-related rocks, granite formed in the post-collision stage, and dyke swarms formed in the intracontinental extension stage. |
WOS关键词 | NW CHINA IMPLICATIONS ; LA-ICP-MS ; CONTINENTAL ARC ; GEOCHEMICAL CHARACTERISTICS ; OPHIOLITIC MELANGES ; NORTHWESTERN CHINA ; NORTHERN XINJIANG ; TRACE-ELEMENTS ; CRUSTAL GROWTH ; SAWUER REGION |
资助项目 | National Natural Science Foundation of China[41672088 41802093] ; National Natural Science Foundation of China[41672088] ; National Key R&D Program of China[2017YFC0601201 2018YFC0604002] ; China Postdoctoral Science Foundation[2018M630201] ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences[KLMR2017-10] |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | WILEY |
WOS记录号 | WOS:000584006900001 |
资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Foundation of Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/98214] |
专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
通讯作者 | Hong, Tao |
作者单位 | 1.Southern Marine Sci & Engn Guangdong Lab, Zhuhai, Peoples R China 2.Chinese Acad Sci, Inst Earth Sci, Beijing, Peoples R China 3.Univ Chinese Acad Sci, Beijing, Peoples R China 4.Dev & Res Ctr China Geol Survey, Beijing, Peoples R China 5.Space Star Technol Co Ltd, Beijing, Peoples R China 6.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangdong Prov Key Lab Geodynam & Geohazards, Guangzhou, Peoples R China 7.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang, Guo-Liang,Hong, Tao,Xu, Xing-Wang,et al. Tectonic-magmatic framework identified by remote sensing analyses and geochronology in West Junggar, Central Asian Orogenic Belt[J]. GEOLOGICAL JOURNAL,2020:18. |
APA | Zhang, Guo-Liang,Hong, Tao,Xu, Xing-Wang,Wu, Chu,Li, Hao,&Chen, Yuan-Wei.(2020).Tectonic-magmatic framework identified by remote sensing analyses and geochronology in West Junggar, Central Asian Orogenic Belt.GEOLOGICAL JOURNAL,18. |
MLA | Zhang, Guo-Liang,et al."Tectonic-magmatic framework identified by remote sensing analyses and geochronology in West Junggar, Central Asian Orogenic Belt".GEOLOGICAL JOURNAL (2020):18. |
入库方式: OAI收割
来源:地质与地球物理研究所
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