中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
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
DOI10.1002/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

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。