孤北洼陷砂岩超压带分布特征及主控因素
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党雪维(1992—),女,陕西合阳人,在读硕士研究生,从事石油地质、成藏动力学方面的研究。联系电话:13871352467,E-mail: dangxw9231@163.com。

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国家科技重大专项“渤海湾盆地精细勘探关键技术”(2011ZX05006-003),高等学校学科创新引智计划资助项目(B14031)。


Distribution characteristics and controlling factors of the overpressure zone in sandstone reservoir of Gubei sag
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    孤北洼陷油气资源丰富,超压带发育。实测地层压力显示,孤北洼陷砂岩超压带主要分布深度为2 800~3 800 m。由于砂岩和泥岩声波时差均与超压有很好的响应关系,且变化幅度和变化趋势一致,故采用Eaton法预测砂岩超压带分布范围,结合实测地层压力进一步分析砂岩超压带分布特征及主控因素。分析结果表明:纵向上,孤北洼陷发育沙一段—东营组底部和沙四段—沙三段2个超压带,其中,沙四段—沙三段为主要超压带;平面上,超压带集中分布于东、西2个次洼,自洼陷中心向凸起及边界断层超压幅度逐渐变小。超压带分布主要受断裂作用、泥岩厚度和含量及烃源岩生油作用等因素控制。

    Abstract:

    Gubei sag has abundant hydrocarbon resources,and the overpressure zones are widely developed in this area.According to the drilling stem test data,present-day overpressure commonly occurs at the depth ranging from 2 800 to 3 800 m. As the sonic transit times have obvious responses to overpressure in both sandstone and mudstone with similar range of variation and trend,the Eaton method was used to predict overpressure in sandstone reservoir. In addition,the distribution characteristics and the controlling factors of the pressure distribution were analyzed combining the drilling stem test data. On the whole,two overpressure systems were identified in the vertical including an upper system distributed in lower Ed and Es1 and a lower system in Es3 and Es4 which is also the main overpressure zone. In plane,overpressure distributes in the east and the west subsags,and it decreases gradually from the center to the uplift and boundary faults. The distribution pattern of reservoir overpressure is mainly influenced by faulting,mudstone thickness and content and hydrocarbon generation of source rock.

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党雪维,何生,王永诗,郝雪峰,张君立.孤北洼陷砂岩超压带分布特征及主控因素[J].油气地质与采收率,2016,23(3):47~52

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  • 在线发布日期: 2016-06-02
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