鄂尔多斯盆地延安气田山西组致密砂岩气有效储层开发模式

Jinsong Zhou , Xiangyang Qiao , Ruogu Wang , Xiao Yin , Jun Cao , Binfeng Cao , Yuhong Lei , Kun Tian , Zidan Zhao , Bolun Zhugeng
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引用次数: 5

摘要

通过大量岩石薄片显微观察、扫描电镜分析和流体包裹体均一温度测量,对鄂尔多斯盆地东南部延安气田山西组致密储层岩性组成进行了研究,划分了岩相类型,并结合埋藏史、热演化史、热演化史等研究了不同类型岩石的成岩演化。并对油气充注过程进行了时间匹配,分析了关键油气充注期与储层致密化的时间匹配关系。研究表明,纯石英砂岩和富石英低塑性岩屑砂岩主要发育机械压实、次生溶蚀和高岭石沉淀。两种必需烃未充注前,孔隙度为15.8% ~ 31.5%,为典型的中、高渗透储层岩石。高凝灰质非均质石英砂岩、富塑性粒状岩屑砂岩和碳酸盐致密胶结砂岩孔隙度在4.6% ~ 10.8%之间,表明储层在第一次关键油气充注前为超低孔-低孔储层。后期烃类很难充注。因此,在油气充注早期保持高孔隙度和渗透率的纯石英砂岩和富石英低塑性粒状岩屑砂岩的成岩作用受到抑制,储层物性较好。它们是晚期天然气的主要运移通道和聚集空间。这构成了致密砂岩气藏的甜点。研究成果对认识储层致密与成藏耦合关系、阐明有效储层形成机制、预测甜点分布具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effective reservoir development model of tight sandstone gas in Shanxi Formation of Yan'an Gas Field, Ordos Basin, China

Through a large number of rock thin section microscopic observations, scanning electron microscopy analysis, and fluid inclusion homogenization temperature measurement, the lithological composition of tight reservoirs in the Shanxi Formation of the Yan'an Gas Field in the southeast of the Ordos Basin was studied, lithofacies types were classified, and the diagenetic evolution of different types of rocks was combined with the burial history, thermal history, and hydrocarbon charging process to analyze the time matching relationship between the key oil and gas charging period and reservoir densification. Studies have shown that pure quartz sandstone and quartz-rich low-plasticity lithic sandstone mainly develop mechanical compaction, secondary dissolution, and kaolinite precipitation. Before the two essential hydrocarbons are charged, the porosity is 15.8%–31.5%, which is typical of medium and high permeability reservoir rocks. The porosity of the high tuffaceous heterogeneous quartz sandstone, plastic-rich granular lithic sandstone, and carbonate tight cemented sandstone ranges from 4.6% to 10.8%, indicating that the reservoir is ultra-low porosity-low porosity reservoirs before the first key hydrocarbon charge. It is difficult to charge the hydrocarbons in the later stage. Therefore, the diagenesis of pure quartz sandstone and quartz-rich low-plastic granular lithic sandstone that maintained high porosity and permeability during early oil and gas charging has been inhibited, and the physical properties of the reservoir are relatively good. They are the primary migration channels and accumulation spaces for late-natural gas. This constitutes a sweet spot in tight sandstone gas reservoirs. The research findings are critical for understanding the coupling relationship between reservoir densification and accumulation, clarifying the formation mechanism of effective reservoir rocks, and predicting the distribution of sweet spots.

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