湖南NW向常德-安仁断裂的地质特征、活动历史及构造性质

柏道远; 李银敏; 钟响; 李彬; 黄乐清; 伍贵华; 李超; 姜文

doi:10.3799/dqkx.2018.571

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2496-2517

Bai Daoyuan, Li Yinmin, Zhong Xiang, Li Bin, Huang Leqing, Wu Guihua, Li Chao, Jiang Wen, 2018. Geological Features, Activity History and Tectonic Attribute of NW-Trending Changde-Anren Fault in Hunan. Earth Science, 43(7): 2496-2517. doi: 10.3799/dqkx.2018.571

Citation:

Bai Daoyuan, Li Yinmin, Zhong Xiang, Li Bin, Huang Leqing, Wu Guihua, Li Chao, Jiang Wen, 2018. Geological Features, Activity History and Tectonic Attribute of NW-Trending Changde-Anren Fault in Hunan. Earth Science, 43(7): 2496-2517. doi: 10.3799/dqkx.2018.571

Citation:

Bai Daoyuan, Li Yinmin, Zhong Xiang, Li Bin, Huang Leqing, Wu Guihua, Li Chao, Jiang Wen, 2018. Geological Features, Activity History and Tectonic Attribute of NW-Trending Changde-Anren Fault in Hunan. Earth Science, 43(7): 2496-2517. doi: 10.3799/dqkx.2018.571

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Geological Features, Activity History and Tectonic Attribute of NW-Trending Changde-Anren Fault in Hunan

doi: 10.3799/dqkx.2018.571

Hunan Institute of Geological Survey, Changsha 410016, China

Received Date: 2017-11-20
Publish Date: 2018-07-15

Abstract

Abstract

Changde-Anren fault is a NW-trending deep fault in eastern Hunan, and its geological features, activity history and tectonic attributes have not been studied systematically. Based on regional geological survey and research data, the authors summarized the general features of the fault, analyzed the nature, genesis and forming ages of the secondary structures origined from the fault, and then reconstructed the activity history, probed in the tectonic attributes and deformation mechanisms of the fault. Main conclusions are as follows:Changde-Anren fault is a NW-trending (330°) basement hidden fault with outcropped fault only in part of north segment and appears as a NW-striking magma-uplift belt. It is a deep major fault breaking through the middle and lower crust and cutting into lithospheric mantle, and dipping northeast with dip angle of 54°. The fault experienced long-term activity as follows. It was a transform fault with strike-slip motion during Neoproterozoic Lengjiaxi Period, strike-slipped dextrally under regional S-N compression in Wuling Movement causing the clockwise rotation of the structural lineaments to the north of Taojiang, extended and controlled the sedimentary facies in Early Banxi Period and Early Nanhua, strike-slipped dextrally under regional S-N compression and fromed secondary NWW-trending thrust faults in Caledonian Movement, strike-slipped sinistrally with thrust and formed secondary NW-trending sinistral strike-slip fault and Anren "y"-type structure under regional NW to NWW compression in late Middle Triassic Indosinian Movement, strike-slipped dextrally under regional S-N compression and formed secondary NWW-trending thrust faults and uplifts during Late Trias-Early Jurassic, strike-slipped sinistrally under regional NWW compression and formed secondary NEE-trending dextral strike-slip fault in Middle Jurassic Early Yanshanian Movement, extended and formed small-scale NW-trending regulative faults controlling the boundary of the southwest end of NNE-trending faulted basins during Cretaceous-Paleogene. Changde-Anren fault was probably a transform fault crosscutting back-arc basin and island arc on the southeastern margin of Yangtze block and Huanan ocean. The uplift along Changde-Anren fault was formed in Indosinain Movement controlled by deep thrust, and rose further for large-scale granitic magmatism in Late Triassic. The hidden properties of the fault were provided by several facts such as follows:The fault developed in Lengjiaxi Group and Nanhua as synsedimentary fault but not in Sinian-Upper Paleozoic; there existed weak detachment layer of Jinjiadong Formation at the bottom of Sinian; NE to NNE-trending major faults cut Changde-Anren fault into several segments with relative independent motion; there occurred a large number of granitic bodies and Cretaceous-Paleogene basins.
- Changde-Anren fault,
- hidden fault,
- magma-uplift belt,
- several tectonic movements,
- transform fault,
- deformation mechanisms,
- tectonics

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References(143)

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