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S77山2^3段储层特征及分类评价

Reservoir Characteristics and Classification Evaluation of the Palaeozoic Shan 2~3 in s77 Formation Uniform graceful
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摘要 苏里格气田东区北端上古生界山西组山23段是天然气的主力产层之一。储层段主要发育辫状河沉积,其中心滩微相为最有利的沉积相带。通过铸体薄片、储层物性、压汞及扫描电镜等资料对储层特征进行分析,研究结果表明:储层岩石类型以石英砂岩为主,有矿物成熟度高而结构成熟度低的岩石学特点,孔隙类型以粒间溶孔和晶间孔为主,总体物性较差,属于典型的低孔低渗储层。研究区较强的压实作用、胶结作用是形成低孔低渗的主要因素;溶蚀作用改善储层物性起到积极作用。综上分析可将研究区储层段分为4类,其中以Ⅱ类储层较发育。 Shan 23section of Neopaleozoic Shansi group is one of the principal natural gas producing formation in the northern Sulige gas field of eastern area.Braided fluvial deposition mainly develop in the reservoir,among which batture microfacies are the most favorable sedimentary facies zone.Through data analysis of cast slice, reservoir properties, mercury penetration and scanning electron microscope,the results show that quartzy sandstone predominates in the lithology which has characteristics of high maturity minerals and low textural maturity lithology, and pore types are mainly interparticle dissolution pore and Inter-crystalline pore. The overall physical property is poor and belongs to low porosity and permeability reservoir.Compacting action and cementation are the key factors to form low porosity and permeability reservoir in the area while chemical erosion has positive effect on improving the physical property of reservoirs.From above analysis the reservoirs in the study area can be divided into 4 kinds. Reservoirs grow relatively well in Type II formation.
作者 齐婷婷
出处 《国外测井技术》 2013年第5期21-24,3,共4页 World Well Logging Technology
关键词 苏里格气田 山23 沉积微相 储层特征 储层评价 Sulige gas field Shan 23 sedimentary microfacies reservoir characteristic reservoir evaluation
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  • 1陈传平,梅博文,毛治超.二元羧酸对硅酸盐矿物溶解的实验初步研究[J].矿物岩石,1993,13(1):103-107. 被引量:19
  • 2内蒙古地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社,1985..
  • 3WALDERHAUG O A. Fluid inclusion study of Quart-Cemented sandstones from offshore Mid-Narway possible evidence for contiued quartz cementation during oil emplacement[ J]. Journat of Sedimentory Petrology, 1990,60 (2):203-210.
  • 4LUNDEGARD P D. Sandstone porosity loss-a "big picture"view of the importance of compaction [ J ]. Joural of Sedimentary Petrography, 1992,62 (2): 250-260.
  • 5SURDAM R C. Organic-inorganic interactions and sandsones diagenesis [ J ]. AAPG, 1989,73 ( 1 ): 1-23.
  • 6SIEBERT R M,MONCURE G K.A theory of framework grain dissolution in sandstones[J].AAPG Memoir,1984,37:163-175.
  • 7MESHRI I D. On the reactivity of sarbonic and organic aeids and generation of of secondary porosity [ J ]. SEPM,1986,38( 1 ) :123-128.
  • 8STOESELL R K,PITTMAN E D. Secondary porosity revisited; the chemistry of feldspar dissolution by carboxylic acids and anions[J]. AAPG,1990,74(12) :1 795-1 805.
  • 9李文厚,魏红红,赵虹,刘锐娥,马振芳,周树勋.苏里格庙地区二叠系储层特征及有利相带预测[J].西北大学学报(自然科学版),2002,32(4):335-340. 被引量:67
  • 10刘锐娥,孙粉锦,拜文华,马成华,黄月明.苏里格庙盒8气层次生孔隙成因及孔隙演化模式探讨[J].石油勘探与开发,2002,29(4):47-49. 被引量:74

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