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Controls on Reservoirs Quality of the Upper Jurassic Mengyin Formation Sandstones in Dongying Depression, Bohai Bay Basin, Eastern China

机译:东营坳陷上侏罗纪蒙阴地区砂岩储层质量的控制,渤海湾盆地渤海湾盆地

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摘要

The Upper Jurassic Mengyin Formation sandstones are important targets for petroleum exploration in Dongying Depression of Bohai Bay Basin, Eastern China. Although the current burial depth of the Upper Jurassic Mengyin Formation sandstones is shallow (900−2500 m), the reservoir rocks are characterized by low porosity and low permeability due to the complex diagenetic modifications after deposition. Experimental tests and statistical methods, such as thin section, scanning electron microscopy (SEM), cathodoluminescence (CL), high pressure mercury injection (HPMI) and fluid inclusion analysis are conducted to delineate the mineralogical, petrographic and petro-physical characteristics. Results show that physical and chemical processes, including burial depth, burial and thermal history and pore fluid evolution, are both important for the diagenetic modifications that result in a variety changes in pore system and reservoir quality. According to numerical simulation of porosity evolution during lengthy burial and thermal history, porosity loss due to the early deep burial process under the high paleo-geothermal gradient can reach about 20%. Moreover, the burial history (effective stress and temperature) has a better guidance to reservoir quality prediction compared with current burial depth. The extensive compaction in sandstones also resulted in extremely low pore fluid flow during subsequent diagenetic processes, thus, the reaction products of dissolution cannot be removed, which would be precipitated as carbonate cements during stable reburial phase. Dissolution resulted from uncomformity-related meteoric flushing have been the most important porosity-enhancing factor in Mengyin Formation sandstones in spite of low thin section porosity averaged out to 3.22%. Secondary pores derived from dissolution of unstable silicates are more likely to develop in sandstones near the regional unconformity. The oil source fault activities may enhance the heterogeneity of reservoir rocks and control the reservoir quality by inducing micro-fractures and providing the main pathways for hydrocarbon migration.
机译:上侏罗统地层蒙阴砂岩是中国东部渤海湾盆地东营凹陷油气勘探的重要目标。虽然上侏罗纪蒙阴地层砂岩的当前埋藏深度浅(900-2500米),储集岩由于沉积后的复成岩修改的特征在于低的孔隙率和低透气性。实验测试和统计方法,如薄片,扫描电子显微镜(SEM),阴极发光(CL),高压汞灯注射(HPMI)和流体夹杂物分析被进行划定矿物学,岩相和石油物理特性。结果表明,物理和化学过程,包括埋藏深度,埋葬和热历史和孔隙流体演化,都为成岩修改重要的是导致孔隙系统和储集层质量的各种变化。根据长时间的埋藏和热史,孔隙度降低过程中孔隙演化的数值模拟由于高古地温梯度下的早期深埋处理可达到20%左右。此外,埋藏历史(有效应力和温度)具有当前埋藏深度相比储层质量预测的更好的指导。在砂岩广泛压实也导致在随后的成岩过程极低孔隙流体流,从而,溶解的反应产物不能被移除,这将被沉淀为期间稳定再掩埋相碳酸盐胶结。溶解造成的不整合有关的流星冲洗一直在蒙阴组砂岩中最重要的孔隙度提高的因素,尽管低薄款孔隙率的平衡到3.22%。从不稳定的硅酸盐的溶解衍生的次级毛孔更容易在区域不整合附近的砂岩发展。油源故障的活动可以提高储集岩的异质性和通过诱导微骨折和提供用于烃迁移主要途径控制储层质量。

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