渤海湾盆地黄河口凹陷东洼断裂体系发育特征及其变形过程的构造物理模拟

杨海风; 吕丁友; 孙永河; 赵野; 张志强; 赵梦

doi:10.3799/dqkx.2020.189

Volume 46 Issue 7

Jul. 2021

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Article Navigation > Earth Science > 2021 > 46(7): 2391-2402

Yang Haifeng, Lü Dingyou, Sun Yonghe, Zhao Ye, Zhang Zhiqiang, Zhao Meng, 2021. The Fault System and Its Tectonophysics Simulation in the Eastern Huanghekou Sag in Bohai Bay Basin. Earth Science, 46(7): 2391-2402. doi: 10.3799/dqkx.2020.189

Citation:

Yang Haifeng, Lü Dingyou, Sun Yonghe, Zhao Ye, Zhang Zhiqiang, Zhao Meng, 2021. The Fault System and Its Tectonophysics Simulation in the Eastern Huanghekou Sag in Bohai Bay Basin. Earth Science, 46(7): 2391-2402. doi: 10.3799/dqkx.2020.189

Citation:

Yang Haifeng, Lü Dingyou, Sun Yonghe, Zhao Ye, Zhang Zhiqiang, Zhao Meng, 2021. The Fault System and Its Tectonophysics Simulation in the Eastern Huanghekou Sag in Bohai Bay Basin. Earth Science, 46(7): 2391-2402. doi: 10.3799/dqkx.2020.189

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The Fault System and Its Tectonophysics Simulation in the Eastern Huanghekou Sag in Bohai Bay Basin

doi: 10.3799/dqkx.2020.189

1.
Tianjin Branch, China National Offshore Oil Cooperation, Tianjin 300459, China
2.
School of Earth Sciences, Northeast Petroleum University, Daqing 163318, China

Received Date: 2020-07-02
Publish Date: 2021-07-15

Abstract

Abstract

The eastern Huanghekou Sag was a typical hydrocarbon-rich sag in Bohai Bay Basin. The fault system of the sag were studied based on new 3D seismic interpretation. A combination of structure interpretation and tectonophisics simulation were applied to reconstruct the tectonic evolution. The results showed that controlled by strike slip and extensional stress, the studied area developed NNE-NE strike slip fault system and EW-NEE extensional fault system, experiencing four stages: the Ek-Es⁴ (the Kongdian Formation: The 4th member of the Shahejie Formation) initial extension-twist rifting stage, the Es³ (the 3rd member of the Shahejie Formation) strike slip extension rifting stage, the Es^1-2-Ed (the 1st and 2nd member of the Shahejie Formation-the Dongying Formation) strike slip stage, and the Ng-Nm (the Guantao Formation-the Minghuazhen Formation) extension twisting stage. The major strike slip fault developed by activating the NE extensional faults formed during the initial stage. The major extensional fault developed on the basis of SN extensional stress during the strike slip extension rifting stage. During the strike slip stage, extension weakened, the faults of all directions activated due to SN extensional stress and showed strike slip-extension complex deformation. During the extension-twisting stage, some of the earlier major faults activated and in the meanwhile, many new secondary faults formed in Neogene.
- strike slip-extensional fault system,
- fault distribution,
- tectonophysics simulation,
- tectonic evolution stage,
- the eastern Huanghekou Sag,
- tectonics

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References(37)

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The Fault System and Its Tectonophysics Simulation in the Eastern Huanghekou Sag in Bohai Bay Basin

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