海底滑坡典型特征及石油地质学意义

海底滑坡是一种由于重力失稳导致的广泛发生在外陆架-上陆坡-深海平原的沉积物搬运体,是海底沉积物重要的搬运过程,具有较强的侵蚀能力和搬运能力,可将大量陆架沉积物搬运至深海,为深海带来丰富的沉积物。再沉积后的滑坡体因其特殊的内部结构,对海洋油气成藏有重要影响。综合国内外研究,对海底滑坡空间展布特征和垂向结构特征进行总结,对滑坡体岩石物理特征进行梳理,揭示海底滑坡边界特征、内部结构以及岩石物理特征。结合海底滑坡特征,从提供物源、储层、盖层、改变海底温压等方面分析海底滑坡对海底油气藏的积极意义,从破坏盖层、改变海底土体温压环境等方面分析海底滑坡对海底油气藏的负面影响。最后结合国内外研究现状,指出未来应...

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Published inHăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 43; no. 1; pp. 94 - 104
Main Authors ZHANG, Yunshan, WU, Nan, JIA Yonggang, Jiangong, WEI
Format Journal Article
LanguageChinese
Published Beijing Marine Geology and Quaternary Geology 01.01.2023
南方海洋科学与工程广东省实验室(广州) ,广州 511458
中国海洋大学山东省海洋环境地质工程重点实验室,青岛 266100
中国海洋大学三亚海洋研究院,三亚 572000%同济大学海洋地质国家重点实验室,上海 200092%中国海洋大学山东省海洋环境地质工程重点实验室,青岛 266100
青岛海洋科学与技术国家实验室,海洋地质过程与环境功能实验室,青岛 266237%中国地质调查局广州海洋地质调查局三亚南海地质研究所,三亚 572000
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ISSN0256-1492
DOI10.16562/j.cnki.0256-1492.2022052001

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Abstract 海底滑坡是一种由于重力失稳导致的广泛发生在外陆架-上陆坡-深海平原的沉积物搬运体,是海底沉积物重要的搬运过程,具有较强的侵蚀能力和搬运能力,可将大量陆架沉积物搬运至深海,为深海带来丰富的沉积物。再沉积后的滑坡体因其特殊的内部结构,对海洋油气成藏有重要影响。综合国内外研究,对海底滑坡空间展布特征和垂向结构特征进行总结,对滑坡体岩石物理特征进行梳理,揭示海底滑坡边界特征、内部结构以及岩石物理特征。结合海底滑坡特征,从提供物源、储层、盖层、改变海底温压等方面分析海底滑坡对海底油气藏的积极意义,从破坏盖层、改变海底土体温压环境等方面分析海底滑坡对海底油气藏的负面影响。最后结合国内外研究现状,指出未来应对海底滑坡微尺度特征识别、进一步开展海底滑坡与海底油气藏联系以及加强海洋油气开发致灾风险等方面进行深入研究。
AbstractList P736; 海底滑坡是一种由于重力失稳导致的广泛发生在外陆架-上陆坡-深海平原的沉积物搬运体,是海底沉积物重要的搬运过程,具有较强的侵蚀能力和搬运能力,可将大量陆架沉积物搬运至深海,为深海带来丰富的沉积物.再沉积后的滑坡体因其特殊的内部结构,对海洋油气成藏有重要影响.综合国内外研究,对海底滑坡空间展布特征和垂向结构特征进行总结,对滑坡体岩石物理特征进行梳理,揭示海底滑坡边界特征、内部结构以及岩石物理特征.结合海底滑坡特征,从提供物源、储层、盖层、改变海底温压等方面分析海底滑坡对海底油气藏的积极意义,从破坏盖层、改变海底土体温压环境等方面分析海底滑坡对海底油气藏的负面影响.最后结合国内外研究现状,指出未来应对海底滑坡微尺度特征识别、进一步开展海底滑坡与海底油气藏联系以及加强海洋油气开发致灾风险等方面进行深入研究.
海底滑坡是一种由于重力失稳导致的广泛发生在外陆架-上陆坡-深海平原的沉积物搬运体,是海底沉积物重要的搬运过程,具有较强的侵蚀能力和搬运能力,可将大量陆架沉积物搬运至深海,为深海带来丰富的沉积物。再沉积后的滑坡体因其特殊的内部结构,对海洋油气成藏有重要影响。综合国内外研究,对海底滑坡空间展布特征和垂向结构特征进行总结,对滑坡体岩石物理特征进行梳理,揭示海底滑坡边界特征、内部结构以及岩石物理特征。结合海底滑坡特征,从提供物源、储层、盖层、改变海底温压等方面分析海底滑坡对海底油气藏的积极意义,从破坏盖层、改变海底土体温压环境等方面分析海底滑坡对海底油气藏的负面影响。最后结合国内外研究现状,指出未来应对海底滑坡微尺度特征识别、进一步开展海底滑坡与海底油气藏联系以及加强海洋油气开发致灾风险等方面进行深入研究。
Author Jiangong, WEI
JIA Yonggang
ZHANG, Yunshan
WU, Nan
AuthorAffiliation 中国海洋大学山东省海洋环境地质工程重点实验室,青岛 266100;中国海洋大学三亚海洋研究院,三亚 572000%同济大学海洋地质国家重点实验室,上海 200092%中国海洋大学山东省海洋环境地质工程重点实验室,青岛 266100;青岛海洋科学与技术国家实验室,海洋地质过程与环境功能实验室,青岛 266237%中国地质调查局广州海洋地质调查局三亚南海地质研究所,三亚 572000;南方海洋科学与工程广东省实验室(广州) ,广州 511458
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Keywords 结构特征
岩石物理特性
海底滑坡
海洋油气
Language Chinese
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南方海洋科学与工程广东省实验室(广州) ,广州 511458
中国海洋大学山东省海洋环境地质工程重点实验室,青岛 266100
中国海洋大学三亚海洋研究院,三亚 572000%同济大学海洋地质国家重点实验室,上海 200092%中国海洋大学山东省海洋环境地质工程重点实验室,青岛 266100
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Snippet 海底滑坡是一种由于重力失稳导致的广泛发生在外陆架-上陆坡-深海平原的沉积物搬运体,是海底沉积物重要的搬运过程,具有较强的侵蚀能力和搬运能力,可将大量陆架沉积物搬...
P736; 海底滑坡是一种由于重力失稳导致的广泛发生在外陆架-上陆坡-深海平原的沉积物搬运体,是海底沉积物重要的搬运过程,具有较强的侵蚀能力和搬运能力,可将大量陆架沉积物...
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SubjectTerms Continental shelves
Continental slope
Deep sea
Deep sea environments
Deep water
Distribution
Geology
Geophysics
Gravity
Hydrocarbons
Landslides
Landslides & mudslides
Marine geology
Natural gas industry
Ocean floor
Offshore operations
Oil
Oil reservoirs
Outer continental shelf
Petroleum geology
Reservoirs
Sediment
Sediment transport
Sediments
Shelf dynamics
Spatial distribution
Transport processes
Vertical distribution
Vertical profiles
Title 海底滑坡典型特征及石油地质学意义
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