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川北地区须四段致密砂岩储层特征及成岩演化
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  • 英文篇名:Characteristics and diagenesis of tight sandstone reservoirs in the 4~(th) member of Xujiahe Formation,northern Sichuan Basin
  • 作者:周林 ; 陈波 ; 凡睿 ; 郝景宇 ; 汪鑫
  • 英文作者:Zhou Lin;Chen Bo;Fan Rui;Hao Jingyu;Wang Xin;Exploration and Production Research Institute,SINOPEC Jianghan Oilfield Company;Hubei Cooperative Innovation Center of Unconventional Oil and Gas,Yangtze University;SINOPEC Exploration Company;Oil and Gas Development Department of Center Tarim,PetroChina Tarim Oilfield Company;
  • 关键词:储层特征 ; 成岩演化 ; 致密砂岩 ; 须四段 ; 川北地区
  • 英文关键词:reservoir characteristics;;diagenetic evolution;;tight sandstone;;Xujiahe Formation;;northern Sichuan Basin
  • 中文刊名:SYYT
  • 英文刊名:Oil & Gas Geology
  • 机构:中国石化江汉油田分公司勘探开发研究院;长江大学非常规油气湖北省协同创新中心;中国石化勘探分公司;中国石油塔里木油田分公司塔中油气开发部;
  • 出版日期:2017-06-28
  • 出版单位:石油与天然气地质
  • 年:2017
  • 期:v.38
  • 基金:国家科技重大专项(2011ZX05013-006-008)
  • 语种:中文;
  • 页:SYYT201703014
  • 页数:9
  • CN:03
  • ISSN:11-4820/TE
  • 分类号:129-136+146
摘要
通过薄片、扫描电镜、压汞及测录井资料分析,结合野外剖面调查和岩心观测等手段,对四川盆地北部须家河组四段致密砂岩储层特征及成岩演化规律进行了研究。结果表明:研究区西部主要发育钙屑砂岩储层,北部主要发育岩屑砂岩储层,东部主要发育长石岩屑砂岩储层,岩石类型的分区性与盆地北部周缘三物源体系分布息息相关;储层物性表现为特低孔、特低渗的特征,孔隙类型以次生溶孔和微裂缝为主,以小孔、细吼为主要特征;储层成岩作用类型复杂,主要有压实压溶作用、胶结作用、溶蚀作用、交代蚀变作用和破裂作用。多种类型的成岩作用在特低渗透致密砂岩储层形成过程中扮演着重要角色。其中,压实作用是造成原生孔隙损失的最主要因素,使储层孔隙度损失77.52%左右;胶结作用破坏储层物性,使孔隙度损失30%左右;溶蚀作用形成次生孔隙,增加孔隙度3.28%;后期构造作用对储层有建设性影响,进而形成现今以次生溶孔-裂缝为主要储集空间的致密砂岩储层。
        Analyses based on thin section,SEM,mercury intrusion and logging data were combined with outcrop and core observations to study the characteristics and diagenesis of tight sandstone reservoirs in the fourth member of the Xujiahe Formation in northern Sichuan Basin. The results show a calcareous sandstone-dominated west part,a lithic sandstonedominated north part and a feldspar/lithic sandstone-dominated east part,in the area of interest. The rock type zoning was found to be closely linked to the distribution of the three provenances at the periphery of northern basin. Physical properties can be summarized as ultra-low porosity and permeability. Types of pores were mainly secondary solution pores with small diameter and fine throat and micro fractures. Diagenesis were complicated and varied from compaction and pressure solution,to cementation,dissolution,replacement and alteration as well as fracturing. And all the processes had once played important roles in the formation of ultra-low permeability tight sandstone reservoirs. Compaction caused loss of primary pores by 77. 52% and cementation destroyed reservoir properties through porosity reduction by 30%. Dissolution generated secondary pores and increased porosity by 3. 28%. Later tectonic activities also helped shaping the reservoirs with secondary solution pores-fractures being the main accumulation space.
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