南沙海域礼乐盆地沉积过程和演化

李鹏春; 赵中贤; 张翠梅; 谢辉; 陈广浩

doi:10.3799/dqkx.2011.087

Volume 36 Issue 5

Sep. 2011

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LI Peng-chun, ZHAO Zhong-xian, ZHANG Cui-mei, XIE Hui, CHEN Guang-hao, 2011. Depositional Process and Evolution of Liyue Basin in Southern South China Sea. Earth Science, 36(5): 837-844. doi: 10.3799/dqkx.2011.087

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LI Peng-chun, ZHAO Zhong-xian, ZHANG Cui-mei, XIE Hui, CHEN Guang-hao, 2011. Depositional Process and Evolution of Liyue Basin in Southern South China Sea. Earth Science, 36(5): 837-844. doi: 10.3799/dqkx.2011.087

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Depositional Process and Evolution of Liyue Basin in Southern South China Sea

doi: 10.3799/dqkx.2011.087

1.
CAS Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou 510301, China
2.
Graduate University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2011-05-28
Available Online: 2021-11-10
Publish Date: 2011-09-15

Abstract

Abstract

The evolution of rift-drift-subsidence can usually be illuminated by sedimental style, subsidence history and structural style, so it's possible to understand basin evolution through analysis of depositional process and coupling tectonic-sedimentary.In this paper, infill stratigraphy, subsidence history and structural characteristics are analyzed.The results show that Liyue basin is characterized by typical "tow-layer" structural pattern, which is separated by a regional breakup unconformity (T₆₀). The horsts and grabens are in low basin overlain by upper depressions of the Neogene.And the half-grabens characterized by asymmetric wedge-shape are bounded by both normal faults and large-scale listric faults, which controlled the sedimentary cycles.The subsidence method is mainly tectonic subsidence before 23.8 Ma but is thermal subsidence after Late Oligocene.There were three regional subsidence episodes, and each subsidence rate was from slow to fast.Liyue basin is primarily composed of three regressive cycles of rift infilling influenced by regional tectonic, which correspond to three stages of basin development.The first stage, characterized by extensional stress, is related to early rift development from approximately 45 Ma until Early Oligocene.Featured by both extension and strike-slip stress, the second is associated with rift-drift development from initiation of sea floor spreading in South China Sea at 30 Ma until the end of sea floor spreading at Middle Miocene.And the third is late post-rift subsidence from approximately 16 Ma until 5.5 Ma, which is controlled by transpressive stress field.
- marine geology,
- sedimentation,
- basin evolution,
- Liyue basin

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References(52)

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