通南巴地区上二叠统长兴组储层特征及预测
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
川东北地区大量发育较好的海相碳酸盐岩储层,而海相碳酸盐岩储层在发育及油气成藏等方面表现复杂。本文通过野外调查,以蟠龙洞、通江铁厂河和羊鼓洞地区长兴组典型生物礁露头为代表并结合室内研究,在以往研究的基础之上结合现有地震资料得出长兴组沉积模式和沉积体系,认为长兴组为台盆对称沉积模式,主要发育台缘礁滩沉积体系、开阔台地(缓坡)沉积体系、浅滩-蒸发坪及盆地沉积体系,且通南巴地区广泛存在台地边缘礁滩相带,进而对长兴组储层区域进行了预测。
Large amount of good sea facies carbonate reservoir developed in northeastern Sichuan area,and showed great complexity in reservoir development and gas-oil reservoiring.This paper has concluded the sedimentary pattern and sedimentary systems by investigating outside and researching inside based on the former research,seismic information and several key biological reef outcrops of Chang Xing formation in Pan Long dong,Tie Chang he and Yang Gu dong areas,Thinking that Chang Xing formation developed mesa-basin symmetrical sedimentary pattern, including mesa fringe reef-shoal facies sedimentary system,open mesa sedimentary system,shoal-vaporizing level ground sedimentary system and basin sedimentary system.Mesa fringe reef-shoal facies belt exists largely in Tongnanba area and we have made further prediction for Chang Xing formation reservoir.
引文
[1]牟传龙,马永生等.四川通江-南江-巴中地区长兴组-飞仙关组沉积模式.地质学报,2007,81(6):820~826.
    [2]郑荣才,胡忠贵等.川东北地区长兴组白云岩储层的成因研究.矿物岩石,2007,27(4):78~84.
    [3]刘殊,唐建明等.川东北地区长兴组--飞仙关组礁滩相储层预测.石油与天然气地质,2006,27(3):332~339.
    [4]黄红涛.川东北地区上二叠系长兴组生物礁特征及分布规律.科协论坛,2008,4(下):102.
    [5]倪新锋,陈洪德等.川东北地区长兴组-飞仙关组沉积格局及成藏控制意义.石油与天然气地质,2007,28(4):458~465.
    [6]汪晴川,李瑞.川东长兴组生物礁分布地震识别技术研究.物探化探计算技术,2008,30(4):282~287.
    [7]陈宗清.四川盆地长兴组生物礁气藏及天然气勘探.石油勘探与开发,2008,35(2):148~156.

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