绥滨坳陷中生界层序地层特征及油气勘探远景
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
详细分析三江盆地绥滨坳陷的钻井资料,并结合地震解释剖面,将绥滨坳陷中生界划分为4个二级层序、8个三级层序,其中二级层序底部的三级层序发育低位体系域,其余不发育低位体系域。平衡剖面和米兰科维奇旋回分析结果表明,绥滨坳陷中生界三级以上层序主要受构造控制,米兰科维奇旋回只对高频层序(体系域)有控制作用。在上述分析基础上建立了绥滨坳陷中生界二级层序地层模式,该模式具有典型的三分性:早期的盆地充填(低位体系域),中期的盆地扩展(水进体系域)和晚期的盆地萎缩(高位体系域)。并指出,二级层序发育的低位体系域上覆的水进体系域可以作为很好的封盖层,同时又可能是烃源岩,因而低位体系域应成为下一步油气勘探的目标。
According to the detailed analysis of drilling data,together with the interpretation of seismic section,the Mesozoic of Suibin Depression is divided into four second-order sequences and eight third-order sequences.The third-order sequences at the bottom of the second-order sequences develop low-stand systems tracts(LSTs),and the other sequences do not.The analysis result of the balanced section and Milankovitch cycle indicates that the Mesozoic sequences above third-order in the Suibin Depression are mainly controlled by structure,and that the Milankovitch cycle only controlls high frequency sequences(systems tracts).Base on the above analyses,the second-order sequence stratigraphy model of the Mesozoic of Suibin Depression is established.The model is of typical tripartition,the early basin fill(LST),the middle basin expansion(TST) and the late basin abortion(HST).The transgressive systems tracts(TSTs) overlying the LSTs in the second-order sequences may be good seal and source rock,so the LSTs have the potential for oil and gas.
引文
[1]解习农,李思田.陆相盆地层序地层研究特点[J].地质科技情报,1993,12(1):22-26.
    [2]纪友亮,张世奇.陆相断陷湖盆层序地层学[M].北京:石油工业出版社,1996.
    [3]贾承造,刘德来,赵文智,等.层序地层学研究新进展[J].石油勘探与开发,2002,29(5):1-4.
    [4]顾家裕,郭彬程,张兴阳.中国陆相盆地层序地层格架及模式[J].石油勘探与开发,2005,32(5):11-15.
    [5]冯有良.断陷盆地层序格架中岩性地层油气藏分布特征[J].石油学报,2005,26(4):17-22.
    [6]郭少斌.陆相断陷盆地层序地层模式[J].石油勘探与开发,2006,33(5):548-552.
    [7]邱桂强,刘军锷,帅萍.米氏旋回基本原理及其在陆相湖盆分析中的应用前景[J].油气地质与采收率,2001,8(5):5-9.
    [8]胡受权,陈国能,王英民,等.Fischer图解及其沉积响应的计算机模拟——以泌阳断陷下第三系核三上段为例[J].石油与天然气地质,1999,20(1):70-75.
    [9]Brown L F,Benson J M Jr,Brink G J,et al.Sequence stratigraphyin offshore South African divergent basins-an atlas on explorationfor Cretaceous lowstand traps[A].AAPG Studies in Geology 41[C].Tulsa:AAPG,1995.1-182.

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