北吕宋岛弧火山活动和台湾造山带造山事件约束下的台湾弧前盆地演化

许淑梅; 王琳华; 李三忠; 刘永江; 訾可; 权日; 舒鹏程; 周越; 郭芮洁; 张宝珠; 王曼茜; 刘政东

doi:10.3799/dqkx.2024.004

Volume 50 Issue 2

Feb. 2025

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Article Navigation > Earth Science > 2025 > 50(2): 466-477

Xu Shumei, Wang Linhua, Li Sanzhong, Liu Yongjiang, Zi Ke, Quan Ri, Shu Pengcheng, Zhou Yue, Guo Ruijie, Zhang Baozhu, Wang Manxi, Liu Zhengdong, 2025. The Evolution of the Taiwan Forearc Basin Constrained by the Volcanic Activities of the North Luzon Island Arc and the Orogenic Events of the Taiwan Orogen Belt. Earth Science, 50(2): 466-477. doi: 10.3799/dqkx.2024.004

Citation:

Xu Shumei, Wang Linhua, Li Sanzhong, Liu Yongjiang, Zi Ke, Quan Ri, Shu Pengcheng, Zhou Yue, Guo Ruijie, Zhang Baozhu, Wang Manxi, Liu Zhengdong, 2025. The Evolution of the Taiwan Forearc Basin Constrained by the Volcanic Activities of the North Luzon Island Arc and the Orogenic Events of the Taiwan Orogen Belt. Earth Science, 50(2): 466-477. doi: 10.3799/dqkx.2024.004

Citation:

Xu Shumei, Wang Linhua, Li Sanzhong, Liu Yongjiang, Zi Ke, Quan Ri, Shu Pengcheng, Zhou Yue, Guo Ruijie, Zhang Baozhu, Wang Manxi, Liu Zhengdong, 2025. The Evolution of the Taiwan Forearc Basin Constrained by the Volcanic Activities of the North Luzon Island Arc and the Orogenic Events of the Taiwan Orogen Belt. Earth Science, 50(2): 466-477. doi: 10.3799/dqkx.2024.004

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The Evolution of the Taiwan Forearc Basin Constrained by the Volcanic Activities of the North Luzon Island Arc and the Orogenic Events of the Taiwan Orogen Belt

doi: 10.3799/dqkx.2024.004

Xu Shumei^{1, 2, 3
,
,},
Wang Linhua^{1, 2},
Li Sanzhong^{1, 2, 3},
Liu Yongjiang^{1, 2, 3},
Zi Ke^{1, 2},
Quan Ri^{1, 2},
Shu Pengcheng^{1, 2},
Zhou Yue^{1, 2},
Guo Ruijie^{1, 2},
Zhang Baozhu^{1, 2},
Wang Manxi^{1, 2},
Liu Zhengdong^{1, 2}

1.
Key Laboratory of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Qingdao 266100, China
2.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Qingdao 266100, China

Received Date: 2024-01-12
Available Online: 2025-02-26
Publish Date: 2025-02-25

Abstract

Abstract

The paper aims to analysis the accommodation feature, basin boundaries and basement properties of the Taiwan forearc basin, and probe into the sequence basic configuration, main controlling factors and evolution stage of the Taiwan forearc basin. Based on the orogenic events, such as the initial and normal subduction of the South China Sea Plate, slabs under plating, accretion, exhumation, uplift and denudation of the accretionary prism and the series of volcanic activities of the North Luzon Island Arc, combined with the sequence configuration analysis of the seismic profiles, this paper will study the basin character, boundary nature and evolutionary stages of the Taiwan forearc basin in more depth. The evolution history of Taiwan forearc basin can be divided into three stages: "rectangular rift basin in the spreading period", "wedge-shaped forearc basin in the initial collision period" and "sheet (residual) forearc basin stage in the arc-continental collision period". The initially eastern boundary of the rectangular rift basin is the South China Sea oceanic crust and later the North Luzon Island Arc, the western boundary is the Philippine Sea oceanic crust, and the basement is forearc split mantle. The eastern and western boundaries of the wedge-shaped forearc basin are the North Luzon Arc and the subducted South China Sea Plate margin which is thickened by the under platings labs respectively, and part of the north Luzon Island Arc gradually evolved into the basement of the forearc basin. The eastern boundary of the deformed residual forearc basin is the North Luzon Island Arc, and the western boundary is the Taiwan accretionary wedge that has been exhumed and continuously uplifted this period.
- sequence configuration,
- seismic sequence,
- forearc basin,
- Taiwan Orogen,
- The North Luzon Island Arc,
- Taiwan,
- tectonics

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The Evolution of the Taiwan Forearc Basin Constrained by the Volcanic Activities of the North Luzon Island Arc and the Orogenic Events of the Taiwan Orogen Belt

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