南海后扩张期大陆边缘闭合过程及成因机制

解习农; 赵帅; 任建业; 杨允柳; 姚永坚

doi:10.3799/dqkx.2022.265

Volume 47 Issue 10

Oct. 2022

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Article Navigation > Earth Science > 2022 > 47(10): 3524-3542

Xie Xinong, Zhao Shuai, Ren Jianye, Yang Yunliu, Yao Yongjian, 2022. Marginal Sea Closure Process and Genetic Mechanism of South China Sea during Post-Spreading Period. Earth Science, 47(10): 3524-3542. doi: 10.3799/dqkx.2022.265

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Xie Xinong, Zhao Shuai, Ren Jianye, Yang Yunliu, Yao Yongjian, 2022. Marginal Sea Closure Process and Genetic Mechanism of South China Sea during Post-Spreading Period. Earth Science, 47(10): 3524-3542. doi: 10.3799/dqkx.2022.265

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Marginal Sea Closure Process and Genetic Mechanism of South China Sea during Post-Spreading Period

doi: 10.3799/dqkx.2022.265

1.
Hubei Key Laboratory of Marine Geological Resources, China University of Geosciences, Wuhan 430074, China
2.
Research Institute of Exploration and Development, SINOPEC Jianghan Oilfield, Wuhan 430079, China
3.
Guangzhou Marine Geological Survey, Guangzhou 510075, China

Received Date: 2022-04-19
Publish Date: 2022-10-25

Abstract

Abstract

The South China Sea (SCS) is the largest marginal sea in the West Pacific, but the study of dynamic processes after the termination of the SCS seafloor spreading is not so clear. In this paper it reveals the evolution of the southern and eastern margins of the SCS during the post-SCS spreading period through systematic studies on the identification of tectonically unconformities, contemporaneous sedimentary records of fold-and-thrust belt. The results show that the southern and eastern margins of the SCS have undergone the evolution of multiple microplates from subduction to collision since the Miocene. Several collision boundaries with different characteristics were developed, including continent-continent collision, arc-continent collision and ocean-arc subduction. The southern margin of the SCS belongs to the proto-SCS slab pull tectonic zone, the Sarawak-Zengmu block in northwest Borneo took the lead in the collision, followed by the Sabah-Nansha block collision in northeast Borneo and the Palawan-Cagayan arc collision in the southwest Palawan island. Since the Middle Miocene, these tectonic events have led to the gradual extinction of the proto-SCS from west to east in a scissor-like pattern, and in the formation of a southern collisional margin characterized by microplate collisions, deep-sea trough development and thick sediments filling in the orogenic foreland. The eastern margin of the SCS is part of the Philippine subduction-collision tectonic zone. Subduction of the SCS oceanic crust to the Philippine Sea plate began in the Miocene, but the arc-continent collisions confined to the northern and southern ends of the eastern margin with further oblique subduction of the Philippine Sea plate. The interaction among the Australia-India plate, the Philippine Sea plate and the Eurasian plate controls the marginal sea closure process in the SCS. The ongoing closure process in the SCS is mainly concentrated on the southern and eastern margins, the eastern margin shows a closure process characterized by the extinction of oceanic crust, while the southern margin is a closure process characterized by the collision of microplates. Therefore, the continental margin evolution during the post-SCS spreading period can provide an excellent example for the study of marginal sea closure process, and is also important for the protection of national maritime rights and interests and the study of the dynamics of continental margins in the SCS.

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Marginal Sea Closure Process and Genetic Mechanism of South China Sea during Post-Spreading Period

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