中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Evolution of the Zagros sector of Neo-Tethys: Tectonic and magmatic events that shaped its rifting, seafloor spreading and subduction history

文献类型:期刊论文

作者Jafari, Amin1,2; Ao, Songjian2; Jamei, Susan3; Ghasemi, Habibollah1
刊名EARTH-SCIENCE REVIEWS
出版日期2023-06-01
卷号241页码:19
ISSN号0012-8252
关键词Iran Zagros Neo-Tethys Sanandaj-Sirjan Zone Subduction
DOI10.1016/j.earscirev.2023.104419
英文摘要The evolution of the Neo-Tethys realm had a significant impact on the Phanerozoic paleogeography of the Iran Plateau. However, there remains significant debate regarding the timing of the opening and closure of the Neo-Tethys ocean, as well as the initial stages of subduction and the style of subduction. In this paper, we review the geological data relevant to the Zagros sector of the Neo-Tethys and the associated arc zones (SaSZ and UDMA) in order to update our understanding of the geodynamic history of this region, from early rifting to final closure. Our analysis of Late Devonian-Early Permian rift-related rocks and subsequent subsidence and shallow marine sedimentation through the Triassic period provides compelling evidence for the occurrence of rifting and the formation of a passive margin in the Late Paleozoic. The Late Triassic closure of the Paleo-Tethys ocean in northern Iran marks the inception of Neo-Tethys ocean subduction. Our revised perspective on the subduction style suggests that subduction of the Neo-Tethys oceanic slab began simultaneously across the entire zone in the Late Triassic-Early Jurassic, leading to the production of intraoceanic arc magmatic rocks. However, the variable rates of magma production and the change in the geochemical signature of magmatic rocks from oceanic to continental type observed in the northern domain during the Middle-Late Jurassic indicate a shift from intra-oceanic arc to continental arc subduction. In the southern segment, intraoceanic subduction was still ongoing during this time period. While the early Cretaceous in the southern segment is characterized by the initial obduction of ophiolites, the Late Cretaceous in the entire zone is marked by the underthrusting of the Arabian passive margin, coinciding with the obduction of Cretaceous ophiolites on the overriding plate and the subse-quent subduction of stretched and denser continental Arabian lithosphere with overlying ophiolites. Our tectonic reconstruction highlights the asynchronous nature of the final closure of the Neo-Tethys, which occurred first along the northern margin during the Late Eocene-Early Oligocene and then along the southern margin during the Miocene.
WOS关键词SANANDAJ-SIRJAN ZONE ; ZIRCON U-PB ; ARABIA-EURASIA COLLISION ; OIB-TYPE COMPONENTS ; FOLDED BELT FARS ; NW IRAN EVIDENCE ; CONTINENTAL COLLISION ; NEYRIZ OPHIOLITE ; GEODYNAMIC EVOLUTION ; METAMORPHIC COMPLEX
资助项目National Natural Science Foundation of China[42261144673] ; National Natural Science Foundation of China[41822204] ; National Natural Science Foundation of China[41888101] ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China[2022A03010-1]
WOS研究方向Geology
语种英语
出版者ELSEVIER
WOS记录号WOS:000990587800001
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 ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, 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 ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, 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 ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, 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 ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China ; Science and Technology Major Project of Xinjiang Uygur Autonomous Region, China
源URL[http://ir.iggcas.ac.cn/handle/132A11/110900]  
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Ao, Songjian
作者单位1.Shahrood Univ Technol, Fac Earth Sci, Dept Petrol & Econ Geol, Shahrood, Iran
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
3.Shahid Beheshti Univ, Fac Earth Sci, Tehran, Iran
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Jafari, Amin,Ao, Songjian,Jamei, Susan,et al. Evolution of the Zagros sector of Neo-Tethys: Tectonic and magmatic events that shaped its rifting, seafloor spreading and subduction history[J]. EARTH-SCIENCE REVIEWS,2023,241:19.
APA Jafari, Amin,Ao, Songjian,Jamei, Susan,&Ghasemi, Habibollah.(2023).Evolution of the Zagros sector of Neo-Tethys: Tectonic and magmatic events that shaped its rifting, seafloor spreading and subduction history.EARTH-SCIENCE REVIEWS,241,19.
MLA Jafari, Amin,et al."Evolution of the Zagros sector of Neo-Tethys: Tectonic and magmatic events that shaped its rifting, seafloor spreading and subduction history".EARTH-SCIENCE REVIEWS 241(2023):19.

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来源:地质与地球物理研究所

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