中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Gas hydrates associated with gas chimneys in fine-grained sediments of the northern South China Sea

文献类型:期刊论文

作者Sun, Yunbao1,2; Wu, Shiguo1; Dong, Dongdong1; Ludmann, Thomas3; Gong, Yuehua4
刊名MARINE GEOLOGY
出版日期2012-05-15
卷号311页码:32-40
关键词gas chimney gas hydrate system fine-grained sediment South China Sea
ISSN号0025-3227
通讯作者Wu, SG (reprint author), Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, 7 Nanhai Rd, Qingdao 266071, Peoples R China.
英文摘要Drilling for gas hydrates at the northern continental margin of the South China Sea (SCS) provides a unique insight into the formation of the gas hydrate system in fine-grained sediments, even though most high concentrations of hydrates are found in coarse sediments. Detailed studies of 3D seismic data from a deep-water basin (Baiyun Depression) of this region reveal the presence of overpressured fluid flow, mostly manifested in gas chimneys. Gas chimneys are commonly characterized by disrupted reflections (DR), dim amplitude anomalies (DA), and enhanced reflections (ER) on conventional seismic profiles. Gas chimneys are also characterized by chaotic, low-continuity and low-frequency on instantaneous frequency and instantaneous amplitude profiles. Gas hydrates and a prominent BSR were discovered in the region of gas chimney occurrence. Logging data and sample analyses from drill holes over the chimney structures indicate close relationships between active fluid flow and the formation and accumulation of gas hydrates. Our results document that gas chimneys consisting of a connected network of fractures provide a passageway along which fluids ascend beneath the gas hydrate stability zone (GHSZ) for hydrate formation in fine-grained sediments of the northern South China Sea. Fluids accumulate in uppermost part of the slope where they are trapped beneath the prograding submarine delta sequence, which is not permeable enough for fluids to migrate through. Gas-charged fluids may originate from deep-seated hydrocarbon reservoirs, which are indicated by the molecular and isotopic signatures of gases in gas hydrates occurrence zone. We suppose that the fractures extend into the GHSZ, creating a space for hydrate condensation in the fine-grained sediments of the slope. Gas chimneys may account for the overpressured fluid activity and, most likely, the gas hydrate enrichment in the northern SCS. (C) 2012 Elsevier B.V. All rights reserved.
学科主题Geosciences, Multidisciplinary ; Oceanography
收录类别SCI
原文出处10.1016/j.margeo.2012.04.003
语种英语
WOS记录号WOS:000306035200003
公开日期2013-09-24
源URL[http://ir.qdio.ac.cn/handle/337002/12502]  
专题海洋研究所_海洋地质与环境重点实验室
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Qingdao Inst Marine Geol, Minist Land & Resources, Key Lab Marine Hydrocarbon Resources & Environm G, Qingdao 266071, Peoples R China
3.Univ Hamburg, Inst Biogeochem & Marine Chem, D-20146 Hamburg, Germany
4.MLR, Guangzhou Marine Geol Survey, Guangzhou 510760, Guangdong, Peoples R China
推荐引用方式
GB/T 7714
Sun, Yunbao,Wu, Shiguo,Dong, Dongdong,et al. Gas hydrates associated with gas chimneys in fine-grained sediments of the northern South China Sea[J]. MARINE GEOLOGY,2012,311:32-40.
APA Sun, Yunbao,Wu, Shiguo,Dong, Dongdong,Ludmann, Thomas,&Gong, Yuehua.(2012).Gas hydrates associated with gas chimneys in fine-grained sediments of the northern South China Sea.MARINE GEOLOGY,311,32-40.
MLA Sun, Yunbao,et al."Gas hydrates associated with gas chimneys in fine-grained sediments of the northern South China Sea".MARINE GEOLOGY 311(2012):32-40.

入库方式: OAI收割

来源:海洋研究所

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