南海礼乐滩碳酸盐台地的发育及其新生代构造响应

方鹏高; 丁巍伟; 方银霞; 赵中贤

doi:10.3799/dqkx.2015.182

Volume 40 Issue 12

Dec. 2015

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Fang Penggao, Ding Weiwei, Fang Yinxia, Zhao Zhongxian, 2015. Development of Carbonate Platform and Its Response to Cenozoic Tectonic in Reed Bank Area, the South China Sea. Earth Science, 40(12): 2052-2066. doi: 10.3799/dqkx.2015.182

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Fang Penggao, Ding Weiwei, Fang Yinxia, Zhao Zhongxian, 2015. Development of Carbonate Platform and Its Response to Cenozoic Tectonic in Reed Bank Area, the South China Sea. Earth Science, 40(12): 2052-2066. doi: 10.3799/dqkx.2015.182

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Development of Carbonate Platform and Its Response to Cenozoic Tectonic in Reed Bank Area, the South China Sea

doi: 10.3799/dqkx.2015.182

Fang Penggao^{1, 2
,},
Ding Weiwei^{1, 2
,
,},
Fang Yinxia^{1, 2},
Zhao Zhongxian³

1.
Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
2.
Key Laboratory of Submarine Geosciences, State Oceanic Administration, Hangzhou 310012, China
3.
Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences, Guangzhou 510301, China

Received Date: 2015-04-22
Publish Date: 2015-12-15

Abstract

Abstract

In order to research the role of carbonate platform in the evolution of basin, the development of the carbonate platform and its correlation with the Cenozoic tectonic subsidence characteristics in the Reed Bank area in the southern South China Sea are explored in this study. The rate and amount of tectonic subsidence, and the tectonics are analyzed on the basis of two multi-channel seismic profiles across the Reed Bank area in NW-SE direction. Detailed seismic interpretations prove the occurrence of a wide distributed carbonate platform developed between the Late Oligocene to Early Miocene, which was submerged after the Middle Miocene. Reconstruction of the tectonic subsidence history shows that the tectonic subsidence was controlled by the tectonic activities in different periods, and could be divided into 5 episodes: the slow subsidence episode (Paleocene to Early Oligocene, rifting stage), the uplift and erosion episode (Late Oligocene to Early Miocene, drifting stage), the accelerating subsidence episode(the latest Early Miocene, post-drift stage 1), the intensive subsidence episode(Miocene, post-drift stage 2), and the steady subsidence episode (Late Miocene to present, post-rift stage 3). The development stage of the carbonate platform was consistent with the drifting stage of the South China Sea, during which the tectonic subsidence analysis suggests an uplift and erosion characteristics. This stable shallow water environment was favorable to the development of carbonates. During the drifting stage, large-scale mantle under the oceanic basin and the lateral temperature gradients under the continental margin might have triggered a secondary mantle convection under the rifted Reed Bank basin, resulting in the uplift and erosion activities in this stage, and the wide-development of carbonate platform.
- the South China Sea,
- Reed Bank area,
- carbonate platform,
- tectonics,
- secondary convection

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References(75)

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Development of Carbonate Platform and Its Response to Cenozoic Tectonic in Reed Bank Area, the South China Sea

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