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The forming mechanism of high quality glutenite reservoirs in Baikouquan formation at the Eastern slope of Mahu sag of the Junggar basin, China

机译:中国君武盆地马乌凹陷东坡中高品质谷蛋白水库的成型机制

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摘要

By combining the cores, thin sections, physical properties, and the mercury injection curves, forming mechanism of high quality glutenite reservoirs in Baikouquan Formation at the eastern slope of Mahu Sag is studied. It is a fan-delta sedimentary system of coarse debris gravity flow deposits, with glutenite as the dominant reservoir lithology and dissolution pores as the main reservoir space. High quality reservoirs is primarily controlled by the sedimentary facies and diagenesis. The fan-delta front facies provides material basis, while the dissolution during diagenesis constitutes the primary development mechanism.
机译:通过组合核心,薄段,物理性质和汞注射曲线,研究了在马虎的东部坡度在马虎凹陷的Baikouquan地层中的形成机制。 它是粗碎屑重力流量沉积物的粉丝δ沉积体系,用谷蛋白作为主要的储层岩性和溶出孔作为主储层空间。 高质量的储层主要由沉积相和成岩作用控制。 风扇δ前面部提供了物质的基础,同时成岩作用期间的溶解构成了主要发育机制。

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