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Analysis of continental shale gas accumulation conditions in a rifted basin: A case study of Lower Cretaceous shale in the southern Songliao Basin, northeastern China

机译:大裂盆地大陆物流储气条件分析 - 以中国东北部南部松辽盆地下白垩纪页岩案例研究

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The analysis of shale gas accumulation conditions is the basis of shale gas exploration. Previous research has mainly focused on the Upper Cretaceous shale in the Songliao Basin of northeastern China, and few studies have analyzed the Lower Cretaceous shale in this area. Based on an integrated analysis of the sedimentary facies, shale samples and seismic interpretation from the Lower Cretaceous Shahezi, Yingcheng and Denglouku Formations of the Fulongquan Depression in the Songliao Basin, the distribution of the shale and the generation, accumulation and preservation conditions of the shale gas are evaluated and discussed. Core observations and sedimentary facies analysis show that the sedimentary facies types in the Shahezi, Yingcheng and Denglouku Formations are mainly fan delta, braided river delta, sublacustrine fan and lacustrine facies. The semideep lake, shallow lake and delta front sedimentary subfacies are favorable for the deposition of shale. The study of the shale distribution indicates that the shale was mainly deposited near the maximum flooding surface of the third-order sequences, and the shales in the Shahezi and Yingcheng Formations are darker and thicker than those in the Denglouku Formation. In addition, the shale in this study area is laterally distributed in the depression belt and the steep slope belt near the boundary faults of the basin. According to the geochemistry tests, rock properties and mineral constituents, the shales in the Shahezi and Yingcheng Formations have favorable gas generation potential. Compared with the properties of the major gas-producing shales in China and the United States, the shales in the Shahezi and the Yingcheng Formations are thick and have a favorable organic matter type, high average organic matter abundance, high organic matter thermal maturity that reached a high maturation stage, high porosity and high gas contents; these properties meet the standards of industrial exploitation, and these shales can therefore be considered favorable targets for unconventional energy exploration.
机译:页岩气累积条件分析是页岩气勘探的基础。以前的研究主要集中在中国东北部松辽盆地的上白垩纪页岩上,少数研究分析了该地区的下白垩纪页岩。根据沉积相,页岩样本和震荡沉积的综合分析,从宋寮盆地的富孔洼坳陷阜流坳陷,页岩的分布以及页岩的发电,积累和保存条件的综合分析评估和讨论气体。核心观测和沉积相分析表明,沙发,盈城和邓禄楼的沉积相类型主要是范三角洲,编织河三角洲,苏布鲁斯风扇和湖泊面。 Semideep湖,浅湖和三角洲前沉积物底饼码头有利于页岩的沉积。对页岩分布的研究表明,页岩主要沉积在三阶序列的最大洪水表面附近,而Shahezi和Yingheng地层的Shales比Denglouku的形成更暗,更厚。此外,该研究区域中的页岩横向分布在凹陷带中,靠近盆的边界断层附近的陡坡带。根据地球化学测试,岩石性质和矿物成分,沙河子和繁成地层的股位有良好的气体发生潜力。与中国和美国的主要生气生产子所的性质相比,沙河子和繁成地层中的罗斯厚,有良好的有机质类型,高平均有机质丰富,高有机物质热成熟度达到了高成熟阶段,高孔隙率和高气体含量;这些物业符合工业开发标准,因此这些页岩因此可以被认为是非传统能源勘探的有利目标。

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