南海白云-荔湾深水区同扩张期岩浆活动特征及构造意义

朱筱曦; 赵中贤; 卓海腾; 庞雄; 郑金云; 孙龙涛; 孙珍

doi:10.3799/dqkx.2021.171

Volume 48 Issue 10

Oct. 2023

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Article Navigation > Earth Science > 2023 > 48(10): 3781-3798

Zhu Xiaoxi, Zhao Zhongxian, Zhuo Haiteng, Pang Xiong, Zheng Jinyun, Sun Longtao, Sun Zhen, 2023. Characteristics of Syn-Spread Magmatism and Its Implication for Tectonic Evolution in Baiyun-Liwan Deep-Water Area of Pearl River Mouth Basin. Earth Science, 48(10): 3781-3798. doi: 10.3799/dqkx.2021.171

Citation:

Zhu Xiaoxi, Zhao Zhongxian, Zhuo Haiteng, Pang Xiong, Zheng Jinyun, Sun Longtao, Sun Zhen, 2023. Characteristics of Syn-Spread Magmatism and Its Implication for Tectonic Evolution in Baiyun-Liwan Deep-Water Area of Pearl River Mouth Basin. Earth Science, 48(10): 3781-3798. doi: 10.3799/dqkx.2021.171

Citation:

Zhu Xiaoxi, Zhao Zhongxian, Zhuo Haiteng, Pang Xiong, Zheng Jinyun, Sun Longtao, Sun Zhen, 2023. Characteristics of Syn-Spread Magmatism and Its Implication for Tectonic Evolution in Baiyun-Liwan Deep-Water Area of Pearl River Mouth Basin. Earth Science, 48(10): 3781-3798. doi: 10.3799/dqkx.2021.171

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Characteristics of Syn-Spread Magmatism and Its Implication for Tectonic Evolution in Baiyun-Liwan Deep-Water Area of Pearl River Mouth Basin

doi: 10.3799/dqkx.2021.171

Zhu Xiaoxi^{1, 2, 3
,
,},
Zhao Zhongxian^{1, 2, 4
,
,
,},
Zhuo Haiteng⁵,
Pang Xiong⁶,
Zheng Jinyun⁶,
Sun Longtao^{1, 2},
Sun Zhen^{1, 2, 4
,
,
,}

1.
Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
2.
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China
4.
China-Pakistan Joint Research Center on Earth Sciences, Islamabad 45320, Pakistan
5.
School of Marine Sciences, Sun Yat-sen University, Zhuhai 519082, China
6.
CNOOC Deepwater Development Limited, Shenzhen 518054, China

Received Date: 2021-08-23
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

The syn-rift and syn-spread magmatism occurs in the deep-water area of the continental margin of the South China Sea in different extents, but it is still controversial regarding its spatial and temporal distribution, the amount, and the mechanism. In this paper, the high-resolution and comprehensive covered three-dimensional (3D) seismic data were used to reveal the characteristics and scale of magmatic activities in the Baiyun-Liwan deep-water area. Under the constraints of drilling, it utilized the seismic reflection characteristics, contact relationship and seismic volcano-stratigraphy comprehensively to interpret 19 high-resolution 3D multichannel reflection seismic data. On this basis, the intrusive and eruptive igneous build-ups in the sedimentary layers had been systematically studied. The results show follows: (1) More than 100 igneous bodies and structures related to magmatic activities were identified from shallow to deep in the study area, which are subdivided into 3 seismic facies and 11 subfacies. The 3 facies include volcanic, intrusive and gas-hydro facies. (2) The magmatic activities can be divided into three stages: 33.9-23.0 Ma, 23.0-19.1 Ma and 19.1-16.0 Ma, and the amount of the magmatic activities gradually decreased. (3) In the spatial distribution, the magmatic activities decrease from the southwest to the northeast, and the ages become younger from the south to the north. Moreover, the magmatic activities are mostly distributed on the surrounding uplift. The magmatism in the study area migrated northward as the spreading ridge jumped southward at 23.6 Ma. It is speculated that the upwelling mantle material in the early stage of rifting-spreading stage may be affected by ridge suction, which caused the upwelling magma to be dragged toward the spreading ridge. After a southward ridge jump, the ridge suction reduced and part if not all of the upwelling mantle retreated northward, resulting in the northward migration of magmatic activities after 23 Ma. The alkalinity of magmatism increased during post-spreading stage (< 17 Ma) suggested that the source of magmatic material may become deeper.
- northern margin of South China Sea,
- Baiyun-Liwan deep-water area,
- magmatism,
- spatial and temporal distribution,
- amount of magmatism,
- geophysics,
- tectonics

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References(93)

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Characteristics of Syn-Spread Magmatism and Its Implication for Tectonic Evolution in Baiyun-Liwan Deep-Water Area of Pearl River Mouth Basin

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