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Shale pore characteristics of Shahejie Formation: Implication for pore evolution of shale oil reservoirs in Dongying sag, north China

机译:沙河街组页岩孔隙特征:对华北东营凹陷页岩油藏孔隙演化的启示

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摘要

The pore characteristics of shale reservoirs in the lower submember of Member 3 to upper submember of Member 4 of Shahejie Formation in Dongying sag are analyzed,influences of mineral content and organic matter content on porosity and pore size are also investigated,and through the diagenetic thermal simulation experiment,the main pore evolution is further discussed.The results show that the pore structure of shale reservoirs is complex,the micron-nanometer pores can storage liquid hydrocarbons,and the free-phase crude oil is mainly distributed in intergranular dissolution pores of calcite,recrystallized intergranular pores,intergranular shrinkage fractures of clay mineral which have large pore size.Framework minerals and organic matter content directly influence porosity and pore size of shale reservoirs,relationship between porosity and content of feisic mineral as well as content of organic matter content is linear and positive,while relationship between content of carbonated mineral is negative.At the buried depth from 2500 to 3500 m,concentration of organic acid from hydrocarbon generation and expulsion of organic matter,increasing range of pressure coefficient,are well corresponding to highporosity intervals;pore formation in shale oil reservoirs are almost controlled by diagenetic evolution of clay minerals;framework storage spaces formed by carbonate grain crystals as well as intergranular and intergranular dissolution pores of carbonate increases porosity of shale oil reservoirs;local increase of porosity at the depth of 3500-3800 m is mainly caused by coupling of hydrocarbon-generating overpressure and dissolution,and size,distribution and connectivity of pores are enhanced obviously.
机译:分析了东营凹陷沙河街组三段下段至四段上段页岩储层的孔隙特征,研究了矿物含量和有机质含量对孔隙度和孔隙度的影响,并通过成岩热模拟实验,进一步讨论了主要孔隙演化过程。研究结果表明,页岩储层孔隙结构复杂,微米级孔隙可以储藏液态烃,游离相原油主要分布在方解石的粒间溶蚀孔隙中。孔隙大小的粘土矿物的重结晶,晶间孔隙,晶间收缩裂缝。骨架矿物和有机质含量直接影响页岩储层的孔隙度和孔隙度,孔隙度与含铁矿物含量以及有机质含量之间的关系为碳酸盐矿物质含量之间存在线性和正相关关系l为负值。在2500至3500 m的埋深下,烃生成和有机物排出的有机酸浓度,压力系数的增大范围与高孔隙度间隔很好对应;页岩油藏的孔隙形成几乎受控制粘土矿物的成岩演化;碳酸盐晶粒晶体形成的骨架储藏空间以及碳酸盐岩的粒间和粒间溶解孔增加了页岩油储层的孔隙度; 3500-3800 m深度局部孔隙度的增加主要是由于烃类耦合引起的-产生超压和溶解,孔的尺寸,分布和连通性明显增强。

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  • 来源
    《石油研究(英文)》 |2019年第002期|113-124|共12页
  • 作者单位

    Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257022, China;

    Postdoctor Scientific Research Stations, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257000, China;

    Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257022, China;

    Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257022, China;

    Petroleum Development Center of Shengli Oilfield, Shandong, Dongying, 227022, China;

    Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257022, China;

    Postdoctor Scientific Research Stations, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257000, China;

    Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257022, China;

    Postdoctor Scientific Research Stations, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257000, China;

    Petroleum Development Center of Shengli Oilfield, Shandong, Dongying, 227022, China;

    Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257022, China;

    Research Institute of Petroleum Exploration and Development, Sinopec Shengli Oilfield Company, Shandong, Dongying, 257022, China;

    Petroleum Development Center of Shengli Oilfield, Beijing, 100007, China;

    Chongqing Gas Field of PetroChina Southwest Oil & Gasfield Company, Chongqing, 400021, China;

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  • 入库时间 2022-08-19 04:29:04
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