雪峰山西侧梵净山—桑植地区构造变形特征

周小军; 李三忠; 王岳军; 刘静

doi:10.3799/dqkx.2011.104

Volume 36 Issue 6

Jun. 2011

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Article Navigation > Earth Science > 2011 > 36(6): 985-992

ZHOU Xiao-jun, LI San-zhong, WANG Yue-jun, LIU Jing, 2011. Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift. Earth Science, 36(6): 985-992. doi: 10.3799/dqkx.2011.104

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ZHOU Xiao-jun, LI San-zhong, WANG Yue-jun, LIU Jing, 2011. Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift. Earth Science, 36(6): 985-992. doi: 10.3799/dqkx.2011.104

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Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift

doi: 10.3799/dqkx.2011.104

1.
School of Petroleum Engineering, Southwest Petroleum University, Chengdu 610500, China
2.
College of Marine Geosciences, Ocean University of China, Qingdao 266003, China
3.
Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China
4.
Department of Geology, Northwest University, Xi'an 710069, China
5.
State Key Laboratory of Oil and Gas Reservior Geology and Exploitation, Chengdu 610500, China

Received Date: 2011-03-10
Available Online: 2021-11-10
Publish Date: 2011-06-15

Abstract

Abstract

Our study area from the Fanjing Mountain to the Sangzhi County is a part of the propagation tectonic zone of the Xuefengshan Precambrian basement. Expounding the deformation in the area facilitates not only the understanding of the deformation in and around the Xuefengshan, but also the exploration in the marine strata in the southern China. Complex history of deformation in the area can be divided into two-stage Indosinian deformation and two-stage Yanshanian deformation. Two-stage Indosinian deformation is of NEE-EW- and NE-striking folding or faulting. Two-stage Yanshanian deformation is of NE- and NNE-NS-striking faulting or folding. Based on the structural analysis and the tectonic setting, this paper suggests that Indosinian deformation mechanism is mainly related to closing of Tethys Ocean and scissor-style collision of South China to North China plates; however, Yanshanian deformation mechanism is mainly related to northwestward subduction of Izanaqi plate and Kula-Pacific plate.
- Yangtze plate,
- Xuefeng uplift,
- tectonics,
- fold superimposition,
- unconformity,
- petroleum geology

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References(42)

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Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift

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