Effects of differential tectonic activities on overpressure evolution in the deep water area of the Qiongdongnan Basin: Implications for gas hydrate accumulation

IF 2.6 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of the Geological Society Pub Date : 2024-01-31 DOI:10.1144/jgs2023-122
Litao Xu, Ren Wang, Jinfeng Ren, Wanzhong Shi, Xiangyang Xie, Yulin He, A. Busbey, Hao Du, Tingna Zuo, Xiaofeng Xu
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Abstract

The lack of data on the complex tectonics of the Qiongdongnan Basin has thus far restricted the understanding of overpressure, deep hydrocarbon, and shallow gas hydrate distribution. In this study, integrated seismic, well, and borehole-test data were combined with basin models to clarify the relationship between tectonic activity and overpressure evolution, as well as potential effects of sub-surface pressure on gas hydrate accumulation. The results show differences in tectonic activity and pressure characteristics between the eastern and western basins. Since the Late Miocene (∼10.5 Ma), large amounts of faults and magmatic intrusions developed in the post-rift layer of the eastern basin (Baodao to Changchang sub-basins), while they seldom formed in the western basin (Lengdong to Lingshui sub-basins). Correspondingly, the eastern basin was characterized by lower overpressures (up to 40 MPa) and the western basin displayed higher overpressures (up to 110 MPa). The results indicated that the tectonic activity since ∼10.5 Ma caused the overpressure relief in the eastern basin. In stark contrast, the overpressure in the western basin increased significantly due to the lack of structural conduits and rapid sedimentation of the thick Pliocene and Quaternary. Numerical models reveal that faults and gas chimneys associated with intrusions constituted shallow plumbing systems through which deep natural gas was able to migrate upward. The formation of gas hydrates relied on the migration of deep gas to the hydrate stability zone below the seafloor. Therefore, the relatively lower overpressured zones due to pressure relief in the eastern basin are considered the next areas potentially favorable to the formation of gas hydrates. Thematic collection: This article is part of the Emerging knowledge on the tectonics of the South China Sea collection available at: https://www.lyellcollection.org/topic/collections/south-china-sea
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不同构造活动对琼东南盆地深水区超压演化的影响:对天然气水合物积聚的影响
迄今为止,由于缺乏有关琼东南盆地复杂构造的数据,限制了对超压、深层油气和浅层天然气水合物分布的了解。本研究将地震、油井和钻孔测试综合数据与盆地模型相结合,阐明了构造活动与超压演化之间的关系,以及地下压力对天然气水合物聚集的潜在影响。结果显示,东部盆地和西部盆地的构造活动和压力特征存在差异。自晚中新世(∼10.5Ma)以来,东部盆地(宝岛至昌昌子盆地)的后断裂层中发育了大量的断层和岩浆侵入体,而西部盆地(冷东至陵水子盆地)则很少形成断层和岩浆侵入体。相应地,东部盆地的超压较低(不超过 40 兆帕),而西部盆地的超压较高(不超过 110 兆帕)。结果表明,自 10.5 Ma 以来的构造活动导致了东部盆地超压的缓解。与此形成鲜明对比的是,由于缺乏构造导管以及上新世和第四纪厚层的快速沉积,西部盆地的超压显著增加。数值模型显示,与侵入体相关的断层和天然气烟囱构成了浅层管道系统,深层天然气能够通过这些管道向上迁移。天然气水合物的形成依赖于深层天然气向海底以下的水合物稳定区迁移。因此,东部盆地因压力释放而形成的相对较低的超压区被认为是下一个可能有利于天然气水合物形成的区域。 专题集:本文是《南海构造新知》文集的一部分,可从以下网址获取:https://www.lyellcollection.org/topic/collections/south-china-sea。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of the Geological Society
Journal of the Geological Society 地学-地球科学综合
CiteScore
6.00
自引率
3.70%
发文量
68
审稿时长
6-12 weeks
期刊介绍: Journal of the Geological Society (JGS) is owned and published by the Geological Society of London. JGS publishes topical, high-quality recent research across the full range of Earth Sciences. Papers are interdisciplinary in nature and emphasize the development of an understanding of fundamental geological processes. Broad interest articles that refer to regional studies, but which extend beyond their geographical context are also welcomed. Each year JGS presents the ‘JGS Early Career Award'' for papers published in the journal, which rewards the writing of well-written, exciting papers from early career geologists. The journal publishes research and invited review articles, discussion papers and thematic sets.
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