琼东南盆地华光凹陷大型海底重力滑动系统特征及其成因机制

李林; 张成; 闫春; 杨涛涛; 解习农; 王少凯; 储生明

doi:10.3799/dqkx.2021.014

Volume 46 Issue 10

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(10): 3707-3716

Li Lin, Zhang Cheng, Yan Chun, Yang Taotao, Xie Xi'nong, Wang Shaokai, Chu Shengming, 2021. Characteristics and Genetic Mechanism of a Large-Scale Submarine Gravity-Driven System in Huaguang Depression, Qiongdongnan Basin. Earth Science, 46(10): 3707-3716. doi: 10.3799/dqkx.2021.014

Citation:

Li Lin, Zhang Cheng, Yan Chun, Yang Taotao, Xie Xi'nong, Wang Shaokai, Chu Shengming, 2021. Characteristics and Genetic Mechanism of a Large-Scale Submarine Gravity-Driven System in Huaguang Depression, Qiongdongnan Basin. Earth Science, 46(10): 3707-3716. doi: 10.3799/dqkx.2021.014

Citation:

Li Lin, Zhang Cheng, Yan Chun, Yang Taotao, Xie Xi'nong, Wang Shaokai, Chu Shengming, 2021. Characteristics and Genetic Mechanism of a Large-Scale Submarine Gravity-Driven System in Huaguang Depression, Qiongdongnan Basin. Earth Science, 46(10): 3707-3716. doi: 10.3799/dqkx.2021.014

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Characteristics and Genetic Mechanism of a Large-Scale Submarine Gravity-Driven System in Huaguang Depression, Qiongdongnan Basin

doi: 10.3799/dqkx.2021.014

1.
PetroChina Hangzhou Institute of Geology, Hangzhou 310023, China
2.
Hubei Key Laboratory of Marine Geology Resources, China University of Geosciences, Wuhan 430074, China
3.
Southern Marine Science and Engineering Guangdong Laboratory, Guangzhou 511458, China

Received Date: 2020-11-24
Available Online: 2021-11-03
Publish Date: 2021-11-03

Abstract

Abstract

The study on submarine gravity-driven system (SGDS) is of great significance to understand the stability of submarine slope and the deep-water sedimentary processes. A large-scale SGDS sliding from south to north developed in the upper Miocene and above strata in the Huaguang depression of the Qiongdongnan basin, northern margin of the South China Sea. Based on regional 2D seismic data, in this paper it describes the characteristics of seismic facies and development of this large-scale SGDS and discusses its genetic mechanism. The development of the SGDS, composed of five elements including extensional domain, transitional domain, contractional domain, sliding surface and weak layer, could be divided into three stages as follows: the Late Miocene pre-gravity-sliding stage, the Pliocene syn-gravity-sliding stage, and the Quaternary post-gravity-sliding stage. During the fore-gravity-sliding stage, the channel complex was deposited on the bathyal argillaceous slope, and served on the material basis for gravity sliding. During the syn-gravity-sliding stage, which is the main stage of the SGDS development, the sediments were draped on the topography caused by intense deformation, and at the same time, there was also a certain degree of deformation. During the post-gravity-sliding stage, meaning the shrinking of the SGDS, the sediments gradually filled up the topography caused by gravity sliding and continued to deposit. It is indicated that the slope topography and high-speed sediment supply is the basis for the development of the SGDS, and the activation of basement faults and diapirism may be the trigger for its development.
- submarine gravity-driven system,
- mass transport deposit,
- seismic reflection characteristics,
- trigger mechanism,
- Qiongdongnan basin,
- hydrocarbon

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