收稿日期: 2013-03-21
修回日期: 2013-04-17
网络出版日期: 2013-08-10
Diagenesis and Diagenetic Facies of Reservoir in He8 Section of Shihezi Formation in East Ⅱ Part of Sulige Gas Field
Received date: 2013-03-21
Revised date: 2013-04-17
Online published: 2013-08-10
通过借助偏光显微镜、扫描电镜、阴极发光等分析测试手段,结合流体包裹体的分析测试结果,以前人的研究为依据,对苏里格气田东二区盒8段储层成岩作用和成岩相进行研究。通过对成岩序列和孔隙演化的分析,将成岩演化划分为4个阶段6个期次,其中早成岩B晚期—中成岩B早期的酸性溶蚀、溶解作用促使次生孔隙发育,是形成建设性成岩相的关键时期。综合岩石学和成岩作用特征,将苏里格气田东二区盒8段储层成岩相划分为:低孔渗净砂岩不稳定组分溶蚀相、特低孔渗净砂岩不稳定组分溶蚀—胶结相、特低孔渗净砂岩不稳定组分溶蚀—较强压实相、致密净砂岩胶结相与致密中细粒(杂)砂岩压实相5种成岩相类型,并建立了每种成岩相的测井曲线特征。通过单井成岩相分析,成岩相在垂向上表现为以下部溶蚀相,上部压实相为主的特征;在平面上表现为其分布受控于沉积相的展布。低孔渗净砂岩不稳定组分溶蚀相作为最有利的成岩相类型,呈孤岛状分布。
王秀平,牟传龙 . 苏里格气田东二区盒8段储层成岩作用与成岩相研究[J]. 天然气地球科学, 2013 , 24(4) : 678 -689 . DOI: 10.11764/j.issn.1672-1926.2013.04.678
According to the results of experimental methods such as polarizing microscope,scan electron microscope and cathode luminescent,and previous published research results,the characteristics of diagenesis and diagenetic facies of reservoir in He8 section of Shihezi Formation in east Ⅱ part of Sulige Gas Field were studied.Meanwhile,the test results of fluid inclusions were also considered.The diagenetic evolution was divided into four stages including six phases.In the process of diagenetic evolution,the dissolution in late period B of early diagenetic stage to early period B of middle diagenetic stage is so important that produces lots of secondary pores,and because of the dissolution,this stage is the key time to form constructive diagenetic facies.According to the study of petrology and diagenesis,there were five diagenetic facies types,and the logging characteristics of each diagenetic facies were set up.After analyzing the diagenetic facies of single well,diagenetic facies in vertical are characterized by dissolution facies in the below and compaction facies in the upper,and the plane distribution is confined by sedimentary facies.The dissolution facies of unstable components of sandstone with low pore and permeability are the most constructive facies which distribute isolatedly.
Key words: Diagenesis; Porosity evolution; Diagenetic facies; Permian System; Sulige Gas Field
[1]Hu Jiangnai,Zhang Shaonan,Li Demin,et al.The influence of diagenesis on reservoir quality in Shihezi-Shanxi Formation in northern Ordos Basin[J].Journal of Chengdu University of Technology,2001,28(2):169-173.[胡江柰,张哨楠,李德敏,等.鄂尔多斯盆地北部下石盒子组—山西组成岩作用与储层的关系[J].成都理工学院学报,2001,28(2):169-173.]
[2]Wen Guohua,Zheng Rongcai,Gao Hongcan,et al.Sedimentary facies of the 8th Member of lower Shihezi Formation in Su6 area,Sulige Gas Field[J].Acta Sedimentologica Sinica,2007,25(1):90-96.[文华国,郑荣才,高红灿,等.苏里格气田苏6井区下石盒子组盒8段沉积相特征[J].沉积学报,2007,25(1):90-96.]
[3]Wang Xiaomei,Zhao Jingzhou,Liu Xinshe,et al.Occurrence state and production mechanism of formation water in tight sandstone reservoirs of Sulige area,Ordos Basin[J].Petroleum Geology and Experiment,2012,34(4):400-405.[王晓梅,赵靖舟,刘新社.苏里格地区致密砂岩地层水赋存状态和产出机理探讨[J].石油实验地质,2012,34(4):400-405.]
[4]Wang Feng,Tian Jingchun,Chen Rong,et al.Sedimentary characteristics and provrnance analysis of the 8th Member of Xiashihezi Formation in the northern Ordos Basin[J].Computing Techniques for Geophysical and Geochemical Exploration,2010,32(1):41-47.[王峰,田景春,陈蓉,等.鄂尔多斯盆地北部下石盒子组盒8物源分析及沉积特征[J].物探化探计算技术,2010,32(1):41-47.]
[5]Tian Leng,He Shunli,Gu Daihong.The use of 3-D reservoir geological modeling in Sulige Gas Field[J].Natural Gas Geoscience,2004,15(6):593-596.[田冷,何顺利,顾岱鸿.苏里格气田储层三维地质建模技术研究[J].天然气地球科学,2004,15(6):593-596.]
[6]Fan Aiping,Zhao Juan,Yang Renchao,et al.Pore structure of reservoir rocks in Shan1 and He8 Member,the east Ⅱ block of Sulige Gas Field[J].Natural Gas Geoscience,2011,22(3):482-487.[樊爱萍,赵娟,杨仁超,等.苏里格气田东二区山1段、盒8段储层孔隙结构特征[J].天然气地球科学,2011,22(3):482-487.]
[7]Hou Mingcai,Dou Weitan,Chen Hongde,et al.Study on diagenesis of the He8 Member in Sulige Gas Field Ordos Basin[J].Mineral Petrol,2009,29(4):66-74.[侯明才,窦伟坦,陈洪德,等.鄂尔多斯盆地苏里格气田北部盒8、山1段成岩作用及有利储层分布[J].矿物岩石,2009,29(4):66-74.]
[8]Wang Feng,Tian Jingchun,Li Fengjie,et al.Diagenesis of reservoirs in the Upper Paleozoic Member 8 Formation in the Sulige area[J].Tournal of Lanzhou University:Natural Science,2009,45(4):18-29.[王峰,田景春,李凤杰,等.苏里格地区上古生界盒8储层成岩作用[J].兰州大学学报:自然科学版,2009,45(4):18-29.]
[9]Zhang Minglu,Da Shipan,Chen Diaosheng.Diageneses and pore evolution of P1h81,reservoir in Sulige Gas Field[J].Natural Gas Industry,2002,22(6):13-16.[张明禄,达世攀,陈调胜.苏里格气田二叠系盒8段储集层的成岩作用及孔隙演化[J].天然气工业,2002,22(6):13-16.]
[10]Zhu Xiaomin,Sun Lei,Liu Chenglin,et al.Reservoir diagenesis and fluid-rock interaction simulation of the Sulige Gas Field in the Ordos Basin[J].Geology in China,2007,34(2):276-282.[朱筱敏,孙超,刘成林,等.鄂尔多斯盆地苏里格地区储层成岩作用与模拟[J].中国地质,2007,34(2):276-282.]
[11]Zou Caineng,Tao Shizhen,Zhou Hui,et al.Genesis,classification and evaluation method of diagenetic facies[J].Petroleum Exploration and Development,2008,35(5):526-540.[邹才能,陶士振,周慧,等.成岩相的形成、分类与定量评价方法[J].石油勘探与开发,2008,35(5):526-540.]
[12]Zhang Xiangxiang,Zou Caineng,Tao Shizhen,et al.Diagenetic facies types and semiquantitative evaluation of low porosity and permeability sandstones of the fourth Member Xujiahe Formation Guangan area,Sichuan Basin[J].Acta Sedimentologica Sinica,2010,28(1):50-57.[张响响,邹才能,陶士振,等.四川盆地广安地区上三叠统须家河组四段低孔渗砂岩成岩相类型划分及半定量评价[J].沉积学报,2010,28(1):50-57.][HJ1.6mm]
[13]He Zixin,Fu Jin hua,Xi Shengli,et al.Geological features of reservoir formation of Sulige Gas Field[J].Acta Petrolei Sinica,2003,23(2):6-12.[何自新,付金华,席胜利,等.苏里格大气田成藏地质特征[J].石油学报,2003,24(2):6-12.]
[14]Li Haiyan,Peng Shimi.Characteristics of diagenetic reservoir facies of low-permeability reservoir in Sulige Gas Field[J].Acta Petrolei Sinica,2007,28(3):100-104.[李海燕,彭仕宓.苏里格气田低渗透储层成岩储集相特征[J].石油学报,2007,28(3):100-104.]
[15]Lin Wenji,Tang Dazhen,Xu Fengyin,et al.Diagenesis facies type of He8 reservoir in Sulige Gas Field and its logging identification marker[J].Journal of Oil and Gas Technology,2010,32(2):271-273.[林文姬,汤达祯,徐凤银,等.苏里格气田盒8段成岩相类型及其测井标志[J].石油天然气学报:江汉石油学报,2010,32(2):271-273.]
[16]He Dongbo,Jia Ailin,Tian Changbing,et al.Diagenesis and genesis of effective sandstone reservoirs in the Sulige Gas Field[J].Petroleum exploration and development,2004,31(3):69-71.[何东博,贾爱林,田昌炳,等.苏里格气田储集成岩作用及有效储集层成因[J].石油勘探与开发,2004,31(3):69-71.]
[17]Chen Quanhong,Li Wenhou,Hu Xiaolin.Tectonic setting and provenance analysis of Late Paleozoic sedimentary rocks in the Ordos Basin[J].Acta Geologica Sinica,2012,86(7):1150-1162.[陈全红,李文厚,胡孝林.鄂尔多斯盆地晚古生代沉积岩源区构造背景及物源分析[J].地质学报,2012,86(7):1150-1162.]
[18]Li Xiangbo,Wang Jianwei.The formation and evolution of volcanic dust fillings of sandstone in coal measures strata of Ordos Basin[J].Acta Petrologica et Mineralogical,2007,26(1):42-48.[李向博,王建伟.煤系地层中砂岩火山尘填隙物的成岩作用特征——以鄂尔多斯盆地天然气储层为例[J].岩石矿物学杂志,2007,26(1):42-48.]
[19]Yang Renchao,Wang Xiuping,Fan Aiping,et al.Diagenesis of sandstone and genesis of compaction reservoir in the east Ⅱ part of Sulige Gas Field,Ordos Basin[J].Acta Sedimentologica Sinica,2012,30(1):111-119.[杨仁超,王秀平,樊爱萍,等.苏里格气田东二区砂岩成岩作用与致密储层成因[J].沉积学报,2012,30(1):111-119.]
[20]Beard D C,Weyl P K.Influence of texture on porosity and permeability of unconsolidated sand[J].AAPG Bulletin,1973,57(2):349-369.
[21]Taylor T R,Giles MR,Hathon L A,et al.Sandstone diagenesis and reservoir quality prediction:Models,myths and reality[J].AAPG Bulletin,2010,94(8):1093-1132.
[22]Ajdukiewicz J M,Lander R H,Sandstone reservoir quality prediction:The state of the art[J].AAPG Bulletin,2010,94(8):1083-1091.
[23]Surdam R C,Crossey L J,Sven H E,et al.Organic-inorganic interactions and sandstone diagenesis[J].AAPG Bulletin,1989,73(1):1-23.
[24]Surdam R C,Crossey L J.Integrated diagenetic modeling:a process-oriented approach for clastic system[J].Annual Review of Earth and Planetary Sciences,1987,15:141-170.
[25]Li Xiaoqing,Guo Qintao,Qiu Dongzhou.Diagenesis and division of diagenetic phases of the reservoirs in the north Weifang Oil Field[J].Sedimentary Geology and Tethyan Geology,2001,21(4):28-33.[李晓清,郭勤涛,丘东洲.淮北油田的成岩作用及成岩相划分[J].沉积与特提斯地质,2001,21(4):28-33.]
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