方正断陷方4井区宝泉岭组二段沉积相研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
以依舒地堑方正断陷方4井区宝泉岭组二段为研究对象,以钻井、测井和地震资料为基础,综合运用沉积学、地球物理学等理论,开展方正断陷宝泉岭组二段的沉积相模式和沉积相展布特征研究.研究结果表明,方正断陷宝泉岭组二段沉积相类型主要为扇三角洲相、湖泊相、湖底扇相.根据地震相与沉积相之间的相应关系,确定了研究区宝泉岭组二段为横向水系比较发育的扇三角洲-滨浅湖-半深湖沉积体系.
Based on the drill hole, logging and seismic data, the styles and distribution of the sedimentary facies of the second member of Baoquanling Formation in Fangzheng faulted depression are studied with sedimentological and geophysical theories. The results show that the sedimentary facies types are mainly fan delta facies, lacustrine facies and sublacustrine fan facies. According to the correlation between sedimentary facies and seismic facies, it is identified that the second member of Baoquanling Formation belongs to the fan delta-shore shallow lake-semi-deep lake sedimentary system with developed horizontal drainage.
引文
[1]曹成润,王子文.佳-伊地堑方正断陷的断裂控盆效应[J].大庆石油学院学报,1996,20(3):1—4.
    [2]何星,杨建国,李映雁.依-舒地堑方正断陷古近系构造演化与沉积相带展布特征[J].中国地质,2008(5):902—910.
    [3]刘绍平.巴彦浩特盆地的构造类型[J].西南石油学院学报,2003,24(3):24—27.
    [4]马新博.方正断陷三维区宝一段沉积特征研究[D].大庆:东北石油大学,2012.
    [5]王大庆.方正断陷白垩系—古近系层序地层学研究[D].大庆:大庆石油学院,2009.
    [6]朱筱敏.沉积岩石学[M].北京:石油工业出版社,2012.
    [7]黄智辉.地球物理测井资料在分析沉积环境中的应用[M].北京:地质出版社,1986.
    [8]孙家振,李兰斌.地震地质综合解释教程[M].武汉:中国地质大学出版社,2002.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心