鄂尔多斯盆地上石炭统本溪组低渗透砂岩气藏有利产区优选

Yu Lei , Fei Shixiang , Zhao Changhu , Chen Guowei , Cui Yuehua
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引用次数: 0

摘要

近年来,随着天然气勘探开发力度的加大,在鄂尔多斯盆地中东部地区发现了几个上石炭统本溪组高产气藏。多口气井的无阻流量超过1.0 × 106 m3,开发潜力巨大。但是,高产气井(日产气量5.0 × 104 m3)所占比例总体偏低,且地域分布不均匀。因此,识别本溪组气藏高产出的富集因素,加强针对性开发是当前急需解决的问题。本文以位于盆地中东部的衡山-子洲地区本溪组气藏为研究对象。通过对本溪组气藏形成条件和运移规律的认识,系统分析了本溪组气藏的沉积环境、烃源岩特征、储层条件和盖层类型。根据天然气成藏过程,建立了本溪组储层有利区评价标准,为优选优选目标区提供指导。研究表明:①鄂尔多斯盆地中东部本溪组煤层烃源岩广泛发育,为本溪组乃至整个古生界储层提供了充足的气源。②本溪组属于自生自储型天然气储层,本溪组顶部煤层烃源岩生成的天然气优先向下伏低渗透砂岩扩散运移,聚集成藏。③本溪组砂岩储层平均孔隙度为6.27%,平均渗透率为1.5mD。以ⅰ、ⅱ类储层为主,储层性能良好。④上覆直接覆盖层与本溪组煤层和储层形成泥-煤砂、石灰-煤砂、砂-煤砂3种储层组合。石灰石提供了最好的密封条件,其次是泥岩。本研究为鄂尔多斯盆地中东部本溪组天然气勘探开发指明了方向,并对目标区进行了优化评价,为下一阶段天然气规模化开发提供了重要的指导和参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Optimal selection of favorable production areas for low-permeability sandstone gas reservoirs in the Benxi Formation of the Upper Carboniferous in Ordos Basin
In recent years, as natural gas exploration and development have intensified, several high-product gas reservoirs of the Upper Carboniferous Benxi Formation have been discovered in the central and eastern parts of the Ordos Basin. Multiple gas wells have recorded open flow capacity exceeding 1.0 × 106 m3, indicating significant development potential. However, the proportion of high-product gas wells (daily gas production >5.0 × 104 m3) remains generally low, with an uneven geographical distribution. Therefore, identifying the enrichment factors contributing to high product in the Benxi Formation gas reservoirs and enhancing targeted development are critical issues that need to be urgently addressed. The article focus on the Benxi Formation gas reservoir in the Hengshan Zizhou area, located in the central-eastern part of the basin. By enhancing the understanding of the formation conditions and migration patterns of the Benxi Formation gas reservoir, it systematically analyzes the sedimentary environment, source rock characteristics, reservoir conditions, and cap rock types. Evaluation criteria for favorable areas within the Benxi Formation reservoir are established based on the natural gas accumulation process, providing guidance for selecting optimal target areas for production. Research has shown that: ① The coal seam source rocks of the Benxi Formation in the central and eastern parts of the Ordos Basin are widely developed, providing sufficient gas source for the Benxi Formation and even the entire Paleozoic reservoir. ② The Benxi Formation belongs to a self-generating and self-storing natural gas reservoir, where gas generated from the coal seam source rocks at the top of the formation preferentially diffuses and migrates into the underlying low-permeability sandstone, accumulating to form the reservoir. ③ The average porosity of the Benxi Formation sandstone reservoir is 6.27 %, with an average permeability of 1.5mD. It is primarily composed of Class I and II reservoirs, exhibiting good reservoir performance. ④ The overlying direct cover layer forms three reservoir combinations with the Benxi Formation coal seam and reservoir: mud-coal-sand, lime-coal-sand, and sand-coal-sand. Limestone provides the best sealing conditions, followed by mudstone. This research has clarified the direction for natural gas exploration and development in the Benxi Formation of the central and eastern Ordos Basin, and has optimized and evaluated target areas for production, offering significant guidance and reference for the next stage of natural gas scale development.
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