首页|主动大陆边缘典型地区流体运移体系对天然气水合物成藏的影响研究

主动大陆边缘典型地区流体运移体系对天然气水合物成藏的影响研究

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天然气水合物在主动大陆边缘普遍发育,其形成分布与流体运移体系密切相关,对深水油气勘探、海底灾害和全球气候变化研究等具有重要意义.本文选取主动大陆边缘典型地区(马克兰增生楔、郁陵盆地和卡斯卡迪亚增生楔),系统总结各地区流体运移体系特点,旨在探讨流体运移体系对天然气水合物成藏的影响.研究结果表明,同为主动大陆边缘,受制于局部构造环境和沉积条件的影响,不同地区流体运移体系发育模式、水合物成藏类型具有较大差异.马克兰增生楔流体运移体系以泥底辟、断层为主导,形成了"泥底辟型"、"阶梯式增生楔型"水合物藏;郁陵盆地流体运移体系以气烟囱为主导,形成了"扩散型"水合物藏;卡斯卡迪亚增生楔流体运移体系以泥底辟、气烟囱及断裂组合为主导,形成了"渗漏型"水合物藏.尽管前人对主动大陆边缘典型海域的天然气水合物进行了大量的地球物理调查,归纳了多种水合物成藏类型,但由于技术手段限制,缺乏不同运移体系下对流体通量的定量研究及不同运移体系的时空演化过程分析,因此建议将地球物理、地质和地球化学等多学科的研究方法和技术相结合,进行多尺度、多参数的综合研究.
Study on the effect of fluid migration system on natural gas hydrate accumulation in typical areas along active continental margin
The natural gas hydrates widely distribute along the active continental margin.The formation and distribution of gas hydrates are intimately connected to fluid migration systems,holding significant implications for deepwater oil and gas exploration,researches on submarine disasters,and global climate change.This study focuses on selected active continental margin regions,namely the Makran accretion wedge,Ulleung Basin,and Cascadia accretion wedge,to provide a systematic summary of the distinct characteristics exhibited by fluid migration systems on wedge,Ulleung Basin,and Cascadia accretion wedge,to provide a systematic summary of the distinct characteristics exhibited by fluid migration systems in each region,aiming to investigate the influence of fluid migration systems on gas hydrate accumulation.Findings reveal that variations in local tectonic environments and sedimentary conditions give rise to diverse development models for fluid migration systems and hydrate accumulation types across different regions.The fluid migration system within the Makran accretion wedge is predominantly governed by mud diapirs and faults,resulting in the formation of"mud diapir"and"multi-stepped accretionary wedge"type hydrate reservoir.In the Ulleung Basin,the fluid migration system is dominated by gas chimneys,leading to the formation of a diffused hydrate reservoir.In the Cascadia accretion wedge,the fluid migration system is characterized by a combination of mud diapirs,gas chimneys,and fractures,giving rise to a leaky hydrate reservoir.While extensive geophysical surveys have been conducted on gas hydrates in typical sea areas of active continental margins,and various hydrate accumulation types have been identified,there remains a dearth of quantitative studies on fluid flux under different migration systems and analyses of spatio-temporal evolution processes associated with different migration systems.Therefore,it is recommended to integrate research methodologies and techniques from disciplines such as geophysics,geology,and geochemistry to undertake a comprehensive,multi-scale,and multi-parameter study.

Active continental marginsFluid migration systemsNatural gas hydrate

傅钰、童思友、贾雪倩、陈江欣

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中国海洋大学海洋地球科学学院,青岛 266100

海底科学与探测技术教育部重点实验室,中国海洋大学,青岛 266100

中国地质调查局青岛海洋地质研究所,青岛 266237

主动大陆边缘 流体运移体系 天然气水合物

国家自然科学基金项目泰山学者建设工程项目

42074140

2024

地球物理学进展
中国科学院地质与地球物理研究所 中国地球物理学会

地球物理学进展

CSTPCD北大核心
影响因子:1.761
ISSN:1004-2903
年,卷(期):2024.39(3)