首页|鄂尔多斯盆地环江地区长81亚段东西部储层对比研究

鄂尔多斯盆地环江地区长81亚段东西部储层对比研究

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鄂尔多斯盆地环江地区三叠系延长组长81亚段东西部储层储集性能差异明显,造成环江地区东西部油藏富集规律不同.通过岩心观察、测井曲线对比、岩石薄片鉴定以及压汞曲线分析等方法,厘清了环江地区三叠系延长组长81亚段东西部储层基本特征,进而分析了研究区储层致密成因和东西部储层差异主控因素.结果显示:①环江地区长81亚段东西部储层以岩屑长石砂岩和长石岩屑砂岩为主,粒度西部粗于东部,储集空间类型以剩余原生粒间孔为主,次生长石溶孔次之,填隙物含量较高;②东西部物性差异明显,西部山城-罗山川地区孔隙度和渗透率分别为10.71%、6.44 mD,发育低孔-特低渗储层,有相当一部分地区能达到中孔低渗,东部大巴咀-涝池口至洪德以东地区孔隙度和渗透率分别为5.63%、0.13 mD,基本为特低孔-超低渗致密储层;③物源供给、沉积作用和古地形是研究区西部储层物性好于东部的先天地质因素,其中沉积作用和古地形控制着储层砂体厚度和空间展布等宏观特征,物源供给影响储层沉积岩石粒度大小分布和填隙物分布等微观特征.成岩作用是降低研究区东西部储层整体物性的关键因素.
Comparative study of the eastern and western Chang 81 submember in Huanjiang area,Ordos Basin
There are obvious differences in reservoir properties between the eastern and western parts of Chang 81 submember of the Triassic Yanchang Formation in Huanjiang area,Ordos Basin,which results in different oil reservoir enrichment regularity between the eastern and western parts of Huanjiang area.By means of core observation,logging curve comparison,rock thin section identification and mercury injection curve analysis,this paper has clarified the basic reservior characteristics of the eastern and western Chang 81 submember of the Triassic Yanchang Formation in Huanjiang area,and then analyzed the tight genesis of the reservoirs in the studied area and the main controlling factors of the different properties between the eastern and western reservoirs.The research results showed that:① The eastern and western rocks of Chang 8i submember in Huanjiang area are mainly composed of lithic arkose and feldspathic lithic sandstones.The grain size in the west is coarser than that in the east.The pores are dominated by the remaining primary intergranular pores,followed by secondary feldspar dissolved pores,with high content of matrix.②Reservoir properties between the eastern and western parts are huge.The porosity and permeability in western Shancheng and Luoshanchuan area are 10.71%and 6.44 mD,developeing the low porosity and ultra-low permeability reservoirs,in which a considerable part can reach medium porosity and low permeability.In the estern studied area,the porosity and permeability of Dabazui-Laochikou to Hongde area are 5.63%and 0.13 mD,which are basically ultra-low porosity and ultra-low permeability tight reservoirs.③Sediment source supply,sedimentation and paleotopography are the inborn factors that the reservoir physical properties in the western part of the studied area are better than those in the eastern part.Among them,sedimentation and paleotopography control the macroscopic characteristics of reservoir sand body thickness and spatialdistribution,andsedimentsourcesupplyaffectsthemicroscopiccharacteristics of reservoir sedimentary rock particle size distribution and interstitial material distribution.And diagenesis is a key factor to reduce the eastern and western areas overall reservoir physical properties.

reservoir characteristicsmain controlling factorsreservoir differencestight sandstoneYanchang formationHuanjiang areaOrdos Basin

罗顺社、黄文广、王西强、淡卫东、张严

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非常规油气省部共建协同创新中心(长江大学),湖北武汉 430100

长江大学地球科学学院,湖北武汉 430100

中国石油长庆油田分公司第七采油厂,陕西西安 710200

中国石油长庆油田分公司勘探开发研究院,陕西西安 710200

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储层特征 主控因素 储层差异 致密砂岩 延长组 环江地区 鄂尔多斯盆地

国家自然科学基金项目

41672099

2024

长江大学学报(自科版)
长江大学

长江大学学报(自科版)

影响因子:0.335
ISSN:1673-1409
年,卷(期):2024.21(2)
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