北黄海盆地东部坳陷构造演化与油气地质特征

龚承林, 雷怀彦, 王英民, 刘振湖, 官宝聪, 胡小强, 陆金波

龚承林, 雷怀彦, 王英民, 刘振湖, 官宝聪, 胡小强, 陆金波. 北黄海盆地东部坳陷构造演化与油气地质特征[J]. 海洋地质与第四纪地质, 2009, 29(1): 79-86. DOI: 10.3724/SP.J.1140.2009.01079
引用本文: 龚承林, 雷怀彦, 王英民, 刘振湖, 官宝聪, 胡小强, 陆金波. 北黄海盆地东部坳陷构造演化与油气地质特征[J]. 海洋地质与第四纪地质, 2009, 29(1): 79-86. DOI: 10.3724/SP.J.1140.2009.01079
GONG Chenglin, LEI Huaiyan, WANG Yingmin, LIU Zhenhu, GUAN Baocong, HU Xiaoqiang, LU Jinbo. HYDROCARBON GEOLOGIC CHARACTERS AND STRUCTURAL EVOLUTION IN THE EASTERN DEPRESSION OF NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 79-86. DOI: 10.3724/SP.J.1140.2009.01079
Citation: GONG Chenglin, LEI Huaiyan, WANG Yingmin, LIU Zhenhu, GUAN Baocong, HU Xiaoqiang, LU Jinbo. HYDROCARBON GEOLOGIC CHARACTERS AND STRUCTURAL EVOLUTION IN THE EASTERN DEPRESSION OF NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 79-86. DOI: 10.3724/SP.J.1140.2009.01079

北黄海盆地东部坳陷构造演化与油气地质特征

基金项目: 

国家自然科学基金项目(40472156)

详细信息
    作者简介:

    龚承林(1983-),男,硕士生,研究方向为海洋油气地质和层序地层学,E-mail:gongchenlin@sohu.com

  • 中图分类号: P736.1

HYDROCARBON GEOLOGIC CHARACTERS AND STRUCTURAL EVOLUTION IN THE EASTERN DEPRESSION OF NORTH YELLOW SEA BASIN

  • 摘要: 北黄海盆地是我国近海海域惟一没有形成工业油气流的含油气盆地,东部坳陷是北黄海盆地勘探潜力最好的一个区域,该坳陷的油气地质特征和勘探方向研究成为实现这一盆地油气勘探突破的关键。通过对已取得的勘探成果和现有资料的综合研究,指出东部坳陷存在三套生、储、盖组合,其中下白垩统生、储、盖组合最具勘探潜力。
    Abstract: The North Yellow Sea Basin is the only oil and gas-bearing basin, which does not form industrial oil-gas flow. The Eastern Depression is one of the most potential areas of the North Yellow Sea Basin,and the study of hydrocarbon geologic characters and structural evolution is the key to the exploration. Based on the analysis and researches of the former achievements and latest data, the hydrocarbon geologic characters and pool formation condition of Eastern Depression are advanced. In addition, three source-reservoir-cap rock assemblages are identified.Among them, late Jurassic source-reservoir-cap rock assemblage is the most potential one.
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出版历程
  • 收稿日期:  2008-09-09
  • 修回日期:  2009-01-10

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