首页> 外文期刊>Oil & gas science and technology >Prediction of Diagenetic Facies using Well Logs: Evidences from Upper Triassic Yanchang Formation Chang 8 Sandstones in Jiyuan Region, Ordos Basin, China
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Prediction of Diagenetic Facies using Well Logs: Evidences from Upper Triassic Yanchang Formation Chang 8 Sandstones in Jiyuan Region, Ordos Basin, China

机译:利用测井曲线预测成岩相:鄂尔多斯盆地济源地区上三叠统延长组长8砂岩的证据

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摘要

The eighth member of Upper Triassic Yanchang Formation (Chang 8) is the major oil reservoir unit in Jiyuan oil field, though with the high potential for oil exploration. The Chang 8 sandstones are characterized with low porosity, low permeability and strong microscopic heterogeneities due to the complex deep-burial diagenetic history. Detailed petrological studies by thin section, X-ray diffraction, scanning electron microscopy, core analysis have been used to investigate the lithogology characteristics, diagenesis, diagenetic minerals and their coupling impacts on reservoir property. The results show that Chang 8 sandstones comprise fine to medium-grained subarkoses, feldspathic litharenites. The pore systems are dominated by remaining primary intergranular pores, secondary dissolution porosity and micropores. Then, five diagenetic facies were divided in Chang 8 sandstones based on the type and degree of diagenesis, diagenetic minerals assemblages and their coupling effects on the reservoir quality. They consist of grain-coating chlorite weak dissolution facies, unstable component dissolution facies, tight compaction facies, clay minerals filling facies and carbonate cementation facies.
机译:上三叠统延长组八段(长8)是济源油田的主要储油单元,尽管具有很高的勘探潜力。由于深埋成岩作用复杂,长8砂岩的孔隙度低,渗透率低,微观异质性强。通过薄片,X射线衍射,扫描电子显微镜,岩心分析等详细的岩石学研究已用于研究岩性,成岩作用,成岩矿物及其对储层性质的耦合影响。结果表明,长8砂岩由细粒至中等粒度的亚黑石,长石质锂辉石组成。孔隙系统以剩余的主要粒间孔隙,次要溶解孔隙度和微孔为主。然后,根据成岩作用的类型和程度,成岩矿物组合及其对储层质量的耦合作用,在长8砂岩中划分出5个成岩相。它们由包衣亚氯酸盐弱溶解相,不稳定组分溶解相,致密压实相,粘土矿物填充相和碳酸盐胶结相组成。

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