珠江口盆地构造演化旋回及其新生代沉积环境变迁

郑金云; 高阳东; 张向涛; 庞雄; 张青林; 劳妙姬; 冯轩

doi:10.3799/dqkx.2021.258

Volume 47 Issue 7

Jul. 2022

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Article Navigation > Earth Science > 2022 > 47(7): 2374-2390

Zheng Jinyun, Gao Yangdong, Zhang Xiangtao, Pang Xiong, Zhang Qinglin, Lao Miaoji, Feng Xuan, 2022. Tectonic Evolution Cycles and Cenozoic Sedimentary Environment Changes in Pearl River Mouth Basin. Earth Science, 47(7): 2374-2390. doi: 10.3799/dqkx.2021.258

Citation:

Zheng Jinyun, Gao Yangdong, Zhang Xiangtao, Pang Xiong, Zhang Qinglin, Lao Miaoji, Feng Xuan, 2022. Tectonic Evolution Cycles and Cenozoic Sedimentary Environment Changes in Pearl River Mouth Basin. Earth Science, 47(7): 2374-2390. doi: 10.3799/dqkx.2021.258

Citation:

Zheng Jinyun, Gao Yangdong, Zhang Xiangtao, Pang Xiong, Zhang Qinglin, Lao Miaoji, Feng Xuan, 2022. Tectonic Evolution Cycles and Cenozoic Sedimentary Environment Changes in Pearl River Mouth Basin. Earth Science, 47(7): 2374-2390. doi: 10.3799/dqkx.2021.258

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Tectonic Evolution Cycles and Cenozoic Sedimentary Environment Changes in Pearl River Mouth Basin

doi: 10.3799/dqkx.2021.258

Zheng Jinyun^{1, 2
,
,},
Gao Yangdong^{1, 2},
Zhang Xiangtao^{1, 2},
Pang Xiong^{1, 2},
Zhang Qinglin^{1, 2},
Lao Miaoji^{1, 2},
Feng Xuan^{1, 2}

1.
Shenzhen Branch of CNOOC Ltd., Shenzhen 518054, China
2.
CNOOC Deepwater Development Ltd., Shenzhen 518054, China

Received Date: 2021-09-30
Publish Date: 2022-07-25

Abstract

Abstract

There is still a lack of systematic understanding of the evolution process of the Pearl River Mouth Basin since the Mesozoic and its response to the evolution of sedimentary environment. Based on the comparative analysis of the magmatic activity, architectural style of depression and its modification, typical structural deformation style and migration of sedimentary centers, the tectonic evolution of the Pearl River Mouth Basin in Meso-Cenozoic can be divided into 4 stages and 7 periods: (1) the evolution stage of the continental-margin magmatic arc and forearc basin, dominated by paleo-Pacific plate subduction, from Middle Jurassic to early Late Cretaceous (~170-90 Ma); (2) the evolution stage of peripheral foreland basin/post-orogenic collapse to active rift basin in back-arc area, dominated by the subduction retreat of Pacific plate, from Late Cretaceous to Middle Eocene (~90-43 Ma); (3) the evolution stage of passive continental margin, dominated by South China block's extrusion and proto-South China Sea subduction, from Middle Eocene to Middle Miocene (~43-10 Ma); (4) the evolution stage of compression and tensional-shear faults, dominated by NWW upward thrust of the Philippine Sea Plate, since the Late Miocene (~10-0 Ma).~90 Ma, ~43 Ma and~10 Ma are three important periods of tectonic transformation. The subduction of the West Pacific transformed from Andean-type subduction to West Pacific-type subduction in~90 Ma, and the rifting transformed from active rift to passive continental margin extension in ~43 Ma, and the tectonic environment transformed from passive continental margin extension to compression and wrench in ~10 Ma. In this process, with the development and extinction of the proto-South China Sea and the South China Sea, the sedimentary environment in the Cenozoic rifting period gradually transgressed from east to west and from south to north. In the post-rifting period, under the control of phased differential subsidence from south to north, depositional environment transformed from shallow water to deep water, which resulted in significant zoning differences of the petroleum geological conditions in Zhu Ⅰ/Ⅲ, Zhu Ⅱ and Zhu Ⅳ depressions.
- Pearl River Mouth Basin,
- tectonic evolution,
- sedimentary environment evolution,
- staged differential subsidence,
- structural geology

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Tectonic Evolution Cycles and Cenozoic Sedimentary Environment Changes in Pearl River Mouth Basin

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