南沙海槽构造‒地层格架及其动力学意义

高圆圆; 任建业; 佟殿君

doi:10.3799/dqkx.2021.246

Volume 47 Issue 7

Jul. 2022

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Article Navigation > Earth Science > 2022 > 47(7): 2536-2548

Gao Yuanyuan, Ren Jianye, Tong Dianjun, 2022. Tectono-Stratigraphic Framework in Nansha Trough and Its Dynamic Significance. Earth Science, 47(7): 2536-2548. doi: 10.3799/dqkx.2021.246

Citation:

Gao Yuanyuan, Ren Jianye, Tong Dianjun, 2022. Tectono-Stratigraphic Framework in Nansha Trough and Its Dynamic Significance. Earth Science, 47(7): 2536-2548. doi: 10.3799/dqkx.2021.246

Gao Yuanyuan, Ren Jianye, Tong Dianjun, 2022. Tectono-Stratigraphic Framework in Nansha Trough and Its Dynamic Significance. Earth Science, 47(7): 2536-2548. doi: 10.3799/dqkx.2021.246

Citation:

Gao Yuanyuan, Ren Jianye, Tong Dianjun, 2022. Tectono-Stratigraphic Framework in Nansha Trough and Its Dynamic Significance. Earth Science, 47(7): 2536-2548. doi: 10.3799/dqkx.2021.246

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Tectono-Stratigraphic Framework in Nansha Trough and Its Dynamic Significance

doi: 10.3799/dqkx.2021.246

Gao Yuanyuan^{1
,
,},
Ren Jianye^{1, 2
,
,
,},
Tong Dianjun¹

1.
Hubei Key Laboratory of Marine Geological Resources, China University of Geosciences, Wuhan 430074, China
2.
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China

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

Abstract

Abstract

In order to clarify the tectono-stratigraphic framework and genetic mechanism of the Nansha trough basin, in this paper, the quantitative calculation of fault activity and subsidence history is carried out based on the interpretation of regional 2D seismic data in the Nansha trough. Four first-order sequence interfaces (Tg, T60, T50 and T0) have been identified in the Nansha trough basin. On the basis of these four first-order sequence interfaces, the Nansha trough basin can be divided into three basin prototypes: the Paleocene-Oligocene (Tg‒T60) rift basin, the Early Miocene (T60‒T50) depression basin and the Middle Miocene (T50‒T0) foreland basin. From the Cenozoic, the Nansha trough basin has gradually migrated from NW to SE. Comparative analysis from the previous study shows that the Nansha trough foreland basin is formed by the superposition of multi-phased foreland basins. Bounded by the Sarawak orogenic unconformity, the deep regional unconformity and the shallow regional unconformity, the Nansha trough foreland basin can be divided into three stages of the foreland basin: the Early Oligocene to Miocene, the Middle Miocene to the Early Pliocene and the Late Pliocene to present. The Nansha trough belongs to the third phase of the whole foreland basin and is still developing now.
- South China Sea,
- Nansha trough,
- tectonic-stratigraphic framework,
- foreland basin,
- Sarawak orogeny,
- marine geology

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References(53)

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Tectono-Stratigraphic Framework in Nansha Trough and Its Dynamic Significance

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