首页> 外文期刊>Turkish journal of earth sciences >Diagenesis and diagenetic facies distribution prediction of Chang 8 tight oil reservoir in Maling area, Ordos Basin, NW China
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Diagenesis and diagenetic facies distribution prediction of Chang 8 tight oil reservoir in Maling area, Ordos Basin, NW China

机译:西北鄂尔多斯盆地马陵地区长8致密油储层成岩作用与成岩相分布预测

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In this study, characteristics of Chang 8 tight sandstone pore structure and diagenesis are analyzed. A classification standard for sandstone diagenetic facies is established. Combined with the probabilistic neural network method, logging curves are used to predict the distribution of diagenetic facies. The following results are found the Chang 8 reservoir has low porosity-low permeability characteristics, and the pore-throat structures have strong microscopic heterogeneity; both compaction and siliceous and carbonate cementation promote reservoir densification; chlorite cement lining, hydrocarbon emplacement, and the dissolution of feldspar and rock fragments have constructive effects on reservoir development; and two favorable diagenetic facies, a weakly compacted and chlorite-authigenic quartz cementation facies and an intensely compacted-dissolution facies, are developed in the middle of the thick sandstone and are a good match in their horizontal distribution with distributary channel sands. The Chang 81 member has a much larger area that is more favorable for the development of reservoir diagenetic facies than the Chang 82
机译:本研究分析了长8致密砂岩孔隙结构特征及成岩作用。建立了砂岩成岩相分类标准。结合概率神经网络方法,测井曲线被用来预测成岩相的分布。结果表明,长8储层孔隙度低,渗透率低,孔喉结构微观非均质性强。压实和硅质碳酸盐胶结作用都促进了储层的致密化;亚氯酸盐水泥衬里,碳氢化合物的沉积以及长石和岩石碎片的溶解对储层发育具有建设性影响;在厚砂岩的中部发育了两个有利的成岩相,即弱压实和绿泥石自生石英胶结相和强烈压实的溶解相,它们在水平分布上与分布河道砂岩非常匹配。与长82相比,长81成员的面积大得多,更有利于储层成岩相的发展。

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