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Deep strata geologic structure and tight sandy conglomerate gas exploration in Songliao Basin, East China

机译:华东松辽盆地深层地质构造与致密砂砾岩气勘探

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The geologic structure of deep formations, basic geologic pattern of fault depressions, geologic conditions of Lower Cretaceous Shahezi Formation tight gas reservoir, and the exploration direction in the next step in the Songliao Basin are examined based on a comprehensive and comparative analysis of the outcrop, drilling, seismic and geochemical data. Systematic comparison analysis shows that the geologic structure of deep formations in the basin is characterized by a double-layer structure with fault depression in the lower layer and depression in the upper layer. In the deep fault depression (DFD) stage, fault depressions bounded by faults or onlaps and uplifts, developed independently. The faults related to the formation and evolution of the fault depressions can be divided into regional discordogenic fault, basement depression controlling fault, and secondary fault inside depression, and their actions in the evolution of the fault depression groups are presented in the paper. Based on analysis of regional tectonics and basin evolution features, three exploration fields, tight conglomerate gas, volcanic rocks and basement buried hills are pointed out, and it is concluded the tight conglomerate gas in the Shahezi Formation is currently a new strategic field with the most promising exploration prospect. Based on comprehensive analysis of basic oil geologic features of Shahezi Formation, it is proposed that conglomerate is the main category of clastic reservoir in Shahezi Fromation, and parent rock composition, sedimentary structure and facies, and diagenesis are the main factors affecting the distribution of conglomerate reservoirs. Furthermore, the gas reservoirs in Shahezi Formation, all source and reservoir in one, include two types, lithologic and structural types. Favorable sedimentary facies belts in the gentle slope and steep slope control the distribution of the reservoirs, formation of lithologic traps and gas reservoir scale; while secondary faults inside fault depressions control the formation of structural traps and enrichment of natural gas. Finally, seven fault depressions in Shahezi Formation with the most promising prospect of tight gas have been sorted out through comprehensive evaluation.
机译:在对松辽盆地露头进行了综合比较分析的基础上,研究了深层地层的地质结构,断层凹陷的基本地质模式,下白垩统沙河子组致密气藏的地质条件以及下一步的勘探方向,钻井,地震和地球化学数据。系统比较分析表明,盆地深层地层的地质构造为双层构造,下部为断陷,上部为凹陷。在深层断陷(DFD)阶段,以断层或上覆隆升为界的断层凹陷是独立发展的。与断层凹陷的形成和演化有关的断层可分为区域性不发育断层断层,基底凹陷控制断层和凹陷内部次生断层,并介绍了它们在断层凹陷组演化中的作用。在分析区域构造和盆地演化特征的基础上,指出了致密砾岩气,火山岩和地下埋山这三个勘探领域,认为沙河子组致密砾岩气是目前最具发展潜力的新战略气田。勘探前景广阔。在综合分析沙河子组基本石油地质特征的基础上,提出砾岩是沙河子组碎屑岩储层的主要类别,母岩组成,沉积构造和相,成岩作用是影响砾岩分布的主要因素。水库。此外,沙河子组的气藏,气藏和气藏都集中在一个岩性和构造性两种类型中。缓坡和陡坡有利的沉积相带控制了储层的分布,岩性圈闭的形成和气藏规模。断层凹陷内部的次生断层控制构造圈闭的形成和天然气的富集。最后,通过综合评价选出了沙河子组的七个断层凹陷,致密气前景最为广阔。

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