首页|鄂尔多斯盆地西峰东部长8致密砂岩储层特征研究

鄂尔多斯盆地西峰东部长8致密砂岩储层特征研究

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[目的]为明确鄂尔多斯盆地西峰地区东部长8致密储层特征及其控制因素,基于多种储层特征参数进行综合研究.[方法]采用测井曲线分析、岩石薄片观察、高压压汞及扫描电镜等方法,研究长8致密砂岩储层的沉积相标志、岩石碎屑物及填隙物特征、孔隙及物性等特征,并分析复杂成岩作用对储集砂岩致密化的影响.[结果]研究表明:西峰东部地区长8致密砂岩储层多为(中)细粒岩屑长石砂岩及长石岩屑砂岩,多见孔隙、压嵌-孔隙胶结及线接触,残余粒间孔和长石溶孔发育,多见细-微孔细喉道或微孔细喉道型孔隙结构.[结论]强压实作用和方解石胶结是储集砂岩致密化的主要因素,铁方解石的胶结作用和交代作用、绿泥石薄膜及溶蚀作用是优质储层发育的主要因素.
Study on Characteristics of Chang 8 Tight Sandstone Reservoir in Eastern Xifeng Area,Ordos Basin
[Purposes]In order to clarify the characteristics of the Chang 8 tight reservoir and its control-ling factors in the eastern Xifeng of Ordos Basin,this paper is based on various reservoir characteristic parameters.[Methods]The paper uses various analytical tests such as log curve analysis,rock sheet ob-servation,high-pressure mercury intrusion method and scanning electron microscope microscopy to ana-lyze the sedimentary phase signatures of the Chang 8 reservoir sandstone in the study area,the character-istics of rock debris and filler,pore characteristics and physical properties,and to explore the influence of complex diagenesis on the reservoir characteristics.Finally,the influence of complex diagenesis on reservoir characteristics was also discussed.[Findings]The study shows that the quality reservoir lithol-ogy in the Chang 8 tight reservoir in the eastern Xifeng is dominated by(medium)fine-grained rock chip feldspathic sandstone and feldspathic rock chip sandstone.Pores,inlay-pore cementation and line con-tact are common.Residual intergranular pores and feldspar dissolved pores are developed,and fine-micropore fine throat or micropore fine throat pore structure is common.[Conclusions]Compaction and calcite cementation are the main factors of reservoir densification,while the cementation and accounting of iron calcite,chlorite film and dissolution are the main factors for the development of high-quality res-ervoirs.

Ordos BasinChang 8 reservoirreservoir characteristicsdiagenesis

刘浪、王琳、蔡永吉、路敏、吴雨风

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中国石油长庆油田公司采油二厂,甘肃 庆阳 744100

长安大学资源学院,陕西 西安 710054

鄂尔多斯盆地 长8储层 储层特征 成岩作用

2024

河南科技
河南省科学技术信息研究院

河南科技

影响因子:0.615
ISSN:1003-5168
年,卷(期):2024.51(1)
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