中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Two key switches in regional stress field during multi-stage deformation in the Carboniferous-Triassic southernmost Altaids (Beishan, NW China): Response to orocline-related roll-back processes

文献类型:期刊论文

作者Tian, Zhonghua1; Xiao, Wenjiao3,4,5; Windley, Brian F.2; Huang, Peng5; Zhang, Ji'en3,4; Ao, Songjian3,4; Zhang, Zhiyong3,4; Song, Dongfang3,4; Liu, Fulai1
刊名GEOLOGICAL SOCIETY OF AMERICA BULLETIN
出版日期2021-11-01
卷号133期号:11-12页码:2591-2611
ISSN号0016-7606
DOI10.1130/B35898.1
英文摘要The orogenic architecture of the Altaids of Central Asia was created by multiple large-scale slab roll-back and oroclinal bending. However, no regional structural deformation related to roll-back processes has been described. In this paper, we report a structural study of the Beishan orogenic collage in the southernmost Altaids, which is located in the southern wing of the Tuva-Mongol Orocline. Our new field mapping and structural analysis integrated with an electron backscatter diffraction study, paleontology, U-Pb dating, Ar-39-Ar-40 dating, together with published isotopic ages enables us to construct a detailed deformation-time sequence: During D-1 times many thrusts were propagated northwards. In D-2 there was ductile sinistral shearing at 336-326 Ma. In D-3 times there was top-to-W/WNW ductile thrusting at 303-289 Ma. Two phases of folding were defined as D-4 and D-5. Three stages of extensional events (E-1-E-3) separately occurred during D-1-D-5. Two switches of the regional stress field were identified in the Carboniferous to Early Permian (D-1-E-1-D-2-D-3-E-2) and Late Permian to Early Triassic (D-4-E-3-D-5). These two switches in the stress field were associated with formation of bimodal volcanic rocks, and an extensional interarc basin with deposition of Permian-Triassic sediments, which can be related to two stages of roll-back of the subduction zone on the Paleo-Asian oceanic margin. We demonstrate for the first time that two key stress field switches were responses to the formation of the Tuva-Mongol Orocline.
WOS关键词ZIRCON U-PB ; NIUJUANZI OPHIOLITIC MELANGE ; EASTERN TIANSHAN BELT ; CENTRAL-ASIA ; NORTHWEST CHINA ; OROGENIC BELT ; ACCRETIONARY OROGENESIS ; GEOCHEMISTRY ; TECTONICS ; GEOCHRONOLOGY
资助项目National Key Research and Development Program of China[2017YFC0601206] ; National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41822204] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18020203] ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences[QYZDJ-SSW-SYS012]
WOS研究方向Geology
语种英语
WOS记录号WOS:000714983400001
出版者GEOLOGICAL SOC AMER, INC
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences of the Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/103818]  
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 Geol Sci, Inst Geol, Beijing 100037, Peoples R China
2.Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Xinjiang Inst Ecol & Geog, Xinjiang Key Lab Mineral Resources & Digital Geol, Urumqi 830011, Peoples R China
推荐引用方式
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Tian, Zhonghua,Xiao, Wenjiao,Windley, Brian F.,et al. Two key switches in regional stress field during multi-stage deformation in the Carboniferous-Triassic southernmost Altaids (Beishan, NW China): Response to orocline-related roll-back processes[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2021,133(11-12):2591-2611.
APA Tian, Zhonghua.,Xiao, Wenjiao.,Windley, Brian F..,Huang, Peng.,Zhang, Ji'en.,...&Liu, Fulai.(2021).Two key switches in regional stress field during multi-stage deformation in the Carboniferous-Triassic southernmost Altaids (Beishan, NW China): Response to orocline-related roll-back processes.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,133(11-12),2591-2611.
MLA Tian, Zhonghua,et al."Two key switches in regional stress field during multi-stage deformation in the Carboniferous-Triassic southernmost Altaids (Beishan, NW China): Response to orocline-related roll-back processes".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 133.11-12(2021):2591-2611.

入库方式: OAI收割

来源:地质与地球物理研究所

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