渤中凹陷428构造中生界火山岩优质储层主控因素

    Main controlling factors of high-quality Mesozoic volcanic rock reservoirs in the Structure 428 of Bozhong Sag

    • 摘要: 渤海湾盆地中生界火山岩广泛发育,岩性变化快,储层非均质性强,优质储层主控因素认识不清。为探索火山岩优质储层控制因素,充分利用岩芯、薄片、实验等数据,系统分析了研究区火山岩储层岩性特征、储集空间特征及储层控制因素。分析表明:研究区火山岩主要发育安山岩、玄武岩、火山角砾岩和凝灰岩4种岩石类型,储集空间类型为“裂缝-孔隙型”。火山岩优质储层主要受岩性岩相、旋回界面和构造运动共同控制,其中岩性岩相控制了火山岩优质储层的纵向分布,旋回界面控制了火山岩优质储层的垂向分布,构造运动可以对火山岩储层进行再改造。

       

      Abstract: The Mesozoic volcanic rocks, characterized by sharp lithological change, strong reservoir heterogeneity and variable controlling factors, are widely distributed in the Bohai Bay basin. In order to explore the controlling factors of the high-quality volcanic reservoirs, cores, thin sections and laboratory testing data are fully used to reveal lithological characteristics, reservoir space characteristics so as to clarify the controlling factors of the volcanic reservoirs. The data shows that the volcanic rocks in the study area are mainly composed of andesite, basalt, volcanic breccia and tuff, and the reservoir space is dominated by dissolution pores and fractures. The high-quality volcanic reservoirs are mainly controlled by lithology, lithofacies, cyclic interface and structural displacement and deformation. Lithology and lithofacies control the longitudinal distribution of high-quality volcanic reservoirs, cyclic interface controls the vertical distribution of high-quality volcanic reservoirs, and structural displacement and deformation control the reformation of the reservoirs in later stages.

       

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