大洋板块运动方向反转控制活动陆缘岩石圈张裂过程数值模拟

李付成; 孙珍; 张江阳

doi:10.3799/dqkx.2018.581

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3762-3777

Li Fucheng, Sun Zhen, Zhang Jiangyang, 2018. Numerical Studies on Continental Lithospheric Breakup in Response to the Extension Induced by Subduction Direction Inversion. Earth Science, 43(10): 3762-3777. doi: 10.3799/dqkx.2018.581

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Li Fucheng, Sun Zhen, Zhang Jiangyang, 2018. Numerical Studies on Continental Lithospheric Breakup in Response to the Extension Induced by Subduction Direction Inversion. Earth Science, 43(10): 3762-3777. doi: 10.3799/dqkx.2018.581

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Numerical Studies on Continental Lithospheric Breakup in Response to the Extension Induced by Subduction Direction Inversion

doi: 10.3799/dqkx.2018.581

Li Fucheng^{1,2,3
,},
Sun Zhen^{1
,
,},
Zhang Jiangyang¹

1.
CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou 510301, China
2.
Key Laboratory of Submarine Geosciences of State Oceanic Administration, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 266071, China
3.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 310012, China

Received Date: 2018-02-02
Publish Date: 2018-10-20

Abstract

Abstract

In order to investigate how the extension induced by subduction direction inversion affects the continental breakup, we conduct numerical simulation to represent the subduction process in the early stage and the extension induced by subduction direction inversion in the later stage. Meanwhile, different geological bodies, such as oceanic plate with smooth surface, seamount chains, oceanic plateau and weak zone, are added in the model during the early subduction stage. Results show that the extension induced by subduction direction inversion would cause lithospheric thinning, necking and breakup, being accompanied by asthenospheric upwelling and partial melting due to decompression. In addition, the margin deforms to different degrees once the geological bodies enter the early subduction, exerting influence on the strain localization in the subsequent extension, leading to the lithospheric breakup at various locations and start timings. Our results are compatible with the characteristics of timing migration of breakup unconformity in the South China Sea margin, and also offer reference for the geodynamic studies in other passive margins.
- subduction direction inversion,
- continental lithospheric breakup,
- timing migration of breakup,
- South China Sea margin,
- tectonic geology

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References(111)

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Numerical Studies on Continental Lithospheric Breakup in Response to the Extension Induced by Subduction Direction Inversion

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