北黄海盆地西部坳陷地层与沉积特征

王立飞, 王衍棠, 胡小强. 北黄海盆地西部坳陷地层与沉积特征[J]. 海洋地质与第四纪地质, 2010, 30(3): 97-104. doi: 10.3724/SP.J.1140.2010.03097
引用本文: 王立飞, 王衍棠, 胡小强. 北黄海盆地西部坳陷地层与沉积特征[J]. 海洋地质与第四纪地质, 2010, 30(3): 97-104. doi: 10.3724/SP.J.1140.2010.03097
WANG Lifei, WANG Yantang, HU Xiaoqiang. STRATIGRAPHY AND SEDIMENTARY CHARACTERS OF THE WESTERN DEPRESSION,NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2010, 30(3): 97-104. doi: 10.3724/SP.J.1140.2010.03097
Citation: WANG Lifei, WANG Yantang, HU Xiaoqiang. STRATIGRAPHY AND SEDIMENTARY CHARACTERS OF THE WESTERN DEPRESSION,NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2010, 30(3): 97-104. doi: 10.3724/SP.J.1140.2010.03097

北黄海盆地西部坳陷地层与沉积特征

详细信息
    作者简介: 王立飞(1969-),女,高工,主要从事海洋石油地质调查研究,E-mail:wlfniu@163.com
  • 中图分类号: P736.1

STRATIGRAPHY AND SEDIMENTARY CHARACTERS OF THE WESTERN DEPRESSION,NORTH YELLOW SEA BASIN

  • 西部坳陷位于北黄海盆地西部,是盆地6个彼此分割的二级构造单元之一。从实际地震资料出发,结合区域地质及盆地东部钻井资料,运用地震地层学、层序地层学等方法,对西部坳陷的地层发育及分布特征、沉积环境及沉积相等进行了初步分析,认为本坳陷具东西双断的三层结构特征,发育上侏罗统、下白垩统、始新统、渐新统、新近系等地层,中新生代沉积巨厚,最厚达10 200 m,以河-湖-三角洲等陆相沉积为主,具有较好的油气条件及资源前景。
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出版历程
收稿日期:  2009-12-03
修回日期:  2010-04-06

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