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XU Antao, LI Fengjie, LIU Kui, XIANG Pengfei, ZHAO Chenyuan, HU Peng. 2018. The characteristics and sedimentary model of Storm deposits in the Lower Devonian strata of Beichuan[J]. Geology in China, 45(5): 1049-1061. doi: 10.12029/gc20180512
Citation: XU Antao, LI Fengjie, LIU Kui, XIANG Pengfei, ZHAO Chenyuan, HU Peng. 2018. The characteristics and sedimentary model of Storm deposits in the Lower Devonian strata of Beichuan[J]. Geology in China, 45(5): 1049-1061. doi: 10.12029/gc20180512
shu

The characteristics and sedimentary model of Storm deposits in the Lower Devonian strata of Beichuan

  • 1.

    Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

  • 2.

    University of Chinese Academy of Sciences, Beijing 100049, China

  • 3.

    College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China

  • 4.

    Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

  • 5.

    College of Geosciences, China University of Petroleum, Beijing 102249, China

    • Fund Project: Supported by National Natural Science Foundation of China (No. 41172100) and Student's Platform for Innovation and Entrepreneurship Training Program in Sichuan Province (No. 201510616099)
More Information
  • Author Bio: XU Antao, male, born in 1993, master candidate, majors in marine geology; E-mail:xuantao193@163.com
  • Corresponding author: LI Fengjie, male, born in 1972, doctor, professor, majors in sedimentary geology and sequence stratigraphy; E-mail:lifengjie72@163.com 
Received Date:  08 July 2016
Revised Date:  25 February 2018
Publish Date:  25 October 2018
    Abstract

  • Based on the actual measurement data of the storm depositional sections in the Lower Devonian strata of Beichuan and the study of section structures and sedimentary evolution of Ganxi Formation and Xiejiawan Formation, the authors established storm depositional sequences and depositional models of the study area. Storm deposits are widely developed in the Lower Devonian strata of Beichuan, and such geological phenomena as the erosion surface, gutter casts, shell lag deposits, parallel bedding, hummocky cross-stratification, biological genesis structures and other storm sedimentary structures are well developed. In the study area, 3 types of storm deposits and 7 types of storm depositional sequences are developed. The storm deposits in the Lower Devonian strata of Beichuan have good significance for the study of palaeolatitude, palaeoclimate and palaeogeography, because they provide proper evidence for the northward movement of Yangtze plate and tropical or subtropical climate environment of Beichuan area in the Early Devonian period.

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