Characteristics of low permeability reservoir of Chang 2 reservoir in Xirengou area, Ordos Basin

  • QI Yalin ,
  • YIN Peng ,
  • ZHANG Dongyang ,
  • LI Jihong ,
  • LU Wei ,
  • BAI Chang’e
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  • 1. Institute of Shaanxi Yanchang Petroleum (Group) Co. Ltd., Xi’an 710075, China; 2. Dingbian Oil Production Plant, Yanchang Oilfield Corporation, Yulin 718600, Shaanxi, Chin

Online published: 2014-02-05

Abstract

Chang 2 reservoir in Xirengou area is typical low permeability reservoir. The sedimentary characteristics, lithology characteristics, reservoir properties, diagenesis types, pore texture and pore types of Chang 2 reservoir in Xirengou area were studied through analyzing the core, thin sections, scanning electronic microscope and physical properties. The result shows that Chang 2 reservoir developed in distributary channel has the characteristics of ultra-fined grain size of the deposits and low maturity, the pore types are mainly primary intergranular pores and secondary d issolved pores, and structural-lithologic trap is the main type of traps. A large number of arenopelitic and calcarenaceous interlayer that developed in the reservoir led to poor vertical differentiation of oil and water, and further separated reservoir, which makes the in-layer heterogeneity become stronger in single oil reservoir. The macro distribution of Chang 2 reservoir is controlled by local structure, reservoir lithology and physical properties.

Cite this article

QI Yalin , YIN Peng , ZHANG Dongyang , LI Jihong , LU Wei , BAI Chang’e . Characteristics of low permeability reservoir of Chang 2 reservoir in Xirengou area, Ordos Basin[J]. Lithologic Reservoirs, 2014 , 26(1) : 80 -85 . DOI: 10.3969/j.issn.1673-8926.2014.01.012

References

[1] 赵靖舟,吴少波,武富礼.论低渗透储层的分类与评价标准———以鄂尔多斯盆地为例[J].岩性油气藏,2007,19(3):28-31.
[2] 窦伟坦,侯明才,陈洪德,等.鄂尔多斯盆地三叠系延长组油气成藏条件及主控因素研究[J].成都理工大学学报,2008,35(6):686-692.
[3] 李德生.重新认识鄂尔多斯盆地油气地质学[J].石油勘探与开发,2004,31(6):1-7.
[4] 李忠,刘嘉庆.沉积盆地成岩作用的动力机制与时空分布研究若干问题及趋向[J].沉积学报,2009,27(5):837-848.
[5] 李文厚,庞军刚,曹红霞,等.鄂尔多斯盆地晚三叠世延长期沉积体系及岩相古地理演化[J].西北大学学报:自然科学版,2009,39(3):501-506.
[6] 李道品.低渗透油田开发概论[J].大庆石油地质与开发,1997,16(3):33-37.
[7] Gao C,Wang Z L,Deng J,et al. Physical property and origin of lowly permeable sandstone reservoirin Chang 2 division,Zhang-Han oilfield,Ordos Basin[J]. Energy Exploration & Exploitation,2009,27(5):367-389.
[8] 李彦婧,高潮,邓杰,等.东-韩地区延长组长2 油层组储层孔隙结构特征[J].岩性油气藏,2012,24(1):52-56.
[9] 李得路,赵卫卫.鄂尔多斯盆地下寺湾龙咀沟地区长2 油层组成岩作用及对储层的影响[J].岩性油气藏,2013,25(3):77-81.
[10] Ajdukiewicz J M,Nicholson P H,Esch W L. Prediction of deep reservoir quality using early diagenetic process models in the Jurassic Norphlet Formation,Gulf of Mexico [J]. AAPG Bulletin,2010,94(8):1189-1227.
[11] Dutton S P. Calcite cement in Permian deep-water sandstones,Delaware Basin,west Texas:Origin,distribution,and effect on reservoir properties[J]. AAPG Bulletin,2009,93(5):765-787.
[12] 陈全红,李文厚,高永祥,等.鄂尔多斯盆地上三叠统延长组深湖沉积与油气聚集意义[J].中国科学D 辑:地球科学,2007,37(增刊1):39-48.
[13] 赵靖舟,王永东,孟祥振,等. 鄂尔多斯盆地陕北斜坡东部三叠系长2 油藏分布规律[J].石油勘探与开发,2007,34(1):23-27.
[14] 朱国华.陕甘宁盆地西南部上三盛系延长统低渗透砂体和次生孔隙砂体的形成[J].沉积学报,1985,3(2),1-20.
[15] 邓秀芹,刘新社,李士祥. 鄂尔多斯盆地三叠系延长组超低渗透储层致密史与油藏成藏史[J].石油与天然气地质,2009,30(2):156-161.
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