中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Cretaceous Episodic Extension in the South China Block, East Asia: Evidence From the Yuechengling Massif of Central South China

文献类型:期刊论文

作者Chu, Yang2,3,4,5; Lin, Wei2,3; Faure, Michel6; Xue, Zhenhua7; Ji, Wenbin1; Feng, Zhentian2,3
刊名TECTONICS
出版日期2019-10-01
卷号38期号:10页码:3675-3702
关键词detachment fault Cretaceous back-arc extension episodic extension subduction cyclicity South China East Asia
ISSN号0278-7407
DOI10.1029/2019TC005516
英文摘要In the Cretaceous, the subduction of the Izanagi/Paleo-Pacific plates beneath the South China Block (SCB) created a wide back-arc domain characterized by numerous extensional basins coeval with voluminous magmatism. The SCB witnessed the whole evolution by records of widespread extensional structures to accommodate the lithospheric stretching. In the interior of the SCB, the Yuechengling (YCL) Massif preserves a large, low-angle detachment fault, the Ziyuan Detachment (ZYD) at the western margin, and a high-angle ductile normal fault, the Tianhu Fault (THF), in the middle of the massif. Both faults display ductile shearing with top-to-the west kinematics but play different roles in two stages of extension. In the early stage at 140-120 Ma, the THF deformed the eastern YCL pluton at a temperature of similar to 350 degrees C, but the ZYD shows limited movement at this time. On the contrary, the later stage (100-85 Ma) is characterized by pervasive middle- to high-temperature deformation (similar to 400-500 degrees C) and rapid exhumation along the ZYD, but the THF only underwent a near-surface brittle overprint. Across the SCB, the two-phase extension is widely recorded in other extensional structures and coincides with magmatic flare-ups at its eastern margin, suggesting episodic changes in the subduction dip. Combined with two compressional events that took place between the intervals of extension, the SCB experienced two cycles of compression-extension at 155-120 and 120-85 Ma. This periodicity is tentatively interpreted as a combined effect from the Izanagi/Paleo-Pacific subduction angle change and a thickening-foundering process in the arc region.
WOS关键词METAMORPHIC CORE COMPLEX ; DAYUNSHAN-MUFUSHAN BATHOLITH ; MESOZOIC TECTONIC EVOLUTION ; QINGYANG-JIUHUA MASSIF ; U-PB AGE ; NORTH CHINA ; OROGENIC BELT ; STRUCTURAL-ANALYSIS ; XUEFENGSHAN BELT ; FAULT ZONE
资助项目Ministry of Science and Technology[2016YFC0600401] ; Ministry of Science and Technology[2016YFC0600102] ; National Natural Science Foundation of China[91855212] ; National Natural Science Foundation of China[41872208] ; National Natural Science Foundation of China[41302161] ; International Partnership Program of the Chinese Academy of Sciences[GJHZ1776] ; China Scholarship Council[201804910283]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000497909700009
出版者AMER GEOPHYSICAL UNION
资助机构Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council
源URL[http://ir.iggcas.ac.cn/handle/132A11/95854]  
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Chu, Yang
作者单位1.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian, Shaanxi, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
4.Univ Durham, Dept Earth Sci, Durham, England
5.Chinese Acad Sci, Innovat Acad Sci, Beijing, Peoples R China
6.Univ Orleans, Inst Sci Terre Orleans, UMR 7327, Orleans, France
7.China Univ Geosci, Sch Earth Sci, Wuhan, Hubei, Peoples R China
推荐引用方式
GB/T 7714
Chu, Yang,Lin, Wei,Faure, Michel,et al. Cretaceous Episodic Extension in the South China Block, East Asia: Evidence From the Yuechengling Massif of Central South China[J]. TECTONICS,2019,38(10):3675-3702.
APA Chu, Yang,Lin, Wei,Faure, Michel,Xue, Zhenhua,Ji, Wenbin,&Feng, Zhentian.(2019).Cretaceous Episodic Extension in the South China Block, East Asia: Evidence From the Yuechengling Massif of Central South China.TECTONICS,38(10),3675-3702.
MLA Chu, Yang,et al."Cretaceous Episodic Extension in the South China Block, East Asia: Evidence From the Yuechengling Massif of Central South China".TECTONICS 38.10(2019):3675-3702.

入库方式: OAI收割

来源:地质与地球物理研究所

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