莺歌海盆地构造演化与强烈沉降机制的分析和模拟

孙珍; 钟志洪; 周蒂

Volume 32 Issue 3

May 2007

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SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

Citation:

SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

Citation:

SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

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The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin

1.
CAS Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou 510301, China
2.
Department of Science and Technology, Shenzhen Branch of CNOOC, Guangzhou 510240, China

Received Date: 2006-08-28
Publish Date: 2007-05-25

Abstract

Abstract

During Eocene period, rapid subsidence occurred in the Yinggehai basin where more than 17 km of sedimentary cover has been accumulated.According to the analogue modeling experiments, the rigid massif on the Indochina block could be one of the most important factors contributing to the strong subsidence and high sedimentation rate of the basin.Combined the geological analysis with analogue modeling experiments, the evolution of the Yinggehai basin could be divided into four main stages: (1) Before 42 Ma, controlled by the southeastward extension of the Beibu Gulf basin on the northern continental margin, the Yinggehai basin experienced dextral pull-apart.Bounded by NS-trending Yingxi fault, the transtensional areas mainly are the northwest part and along the eastern boundary of the basin. (2) From 42 to 21 Ma, the development of the main rift body in Yinggehai basin was mainly controlled by the southward slip and clockwise rotation of the Indochina block along the Red River fault zone, and the sedimentation was strengthened due to the sinistral transtension.In the east, the subsidence is deepened due to the dextral transtension. (3) From 21 to 10.4 Ma, the sinistral movement of the Indochina block slowed down to still.From 21 to 15.5 Ma, the northwest part of the basin began to inverse locally because of post-rift thermal subsidence of the whole basin. (4) From 10.4 Ma to present, the basin was affected by the dextral movement of the South China block along the Red River fault zone and thermal accident in a new phase at 5 Ma.
- Yinggehai basin,
- tectonic evolution,
- strong subsidence,
- analogue modeling

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References(49)

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The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin

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