准噶尔盆地春光区块沙湾组一段第3砂层组地震相特征研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
通过地震反射的外部形态,内部结构以及地震反射参数的分析,对春光区块沙湾组一段第三砂层组的地震相进行了划分命名。在研究区我们共识别出前积地震相,丘状体,复合丘状体,下凹和充填状等类型。结合钻井资料将地震相转化为沉积相,对沙一段第三砂层组的沉积相进行分析,对预测岩性圈闭有着非常重大的意义。
Based on the analysis of seismic reflection external shape,internal reflection texture and seismic reflection parameters,seismic facies of the third sand set in 1st member of Shawan formation were divided and named.Four types of seismic facies in the research area were recognized,including foreset,moundy,multiple moundy and filling seismic facies.Combined with drilling and seismic data,seismic facies can be transformed into sedimentary facies.Then the lithologic trap can be identified based on the sediment system analysis of the third sand set in 1st member of Shawan formation,which is very significant.
引文
[1]杨勇,陈世悦,王桂萍,等.准噶尔盆地车排子地区古近系沉积相研究[J].油气地质与采收率,2011,18(3).
    [2]王牧.准噶尔盆地春光区块沙湾组一段第三砂层组圈闭预测研究[D].成都理工大学,2011.
    [3]马宗晋,曲国胜,陈新发.准噶尔盆地构造格架及分区[J].新疆石油地质,2008,29(1).
    [4]汪彩云.地震技术在车排子地区岩性油藏勘探中的应用[J].勘探地球物理进展,2009,32(4):280-285.
    [5]徐国强,李小刚,等.春光区块沉积相及沉积微相研究[D].成都理工大学,2011.

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