苏里格气田东南部碳酸盐岩储层特征及分类评价
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摘要
通过对岩心薄片、铸体薄片的观察以及压汞测试等技术手段,对研究区奥陶系马家沟组马五1+2和马五14亚段储层储集岩主要类型、储集空间类型、储集岩物性三方面进行了综合研究,并结合研究区碳酸盐岩储集岩孔洞缝的发育程度和组合形式、毛细管压力曲线特征、含气饱和度、有效厚度及残丘发育程度等多方面参数对储层进行了归类与划分,发现桃2区块的溶蚀孔洞状白云岩、泥—粉晶白云岩、颗粒白云岩及角砾状白云岩是储集岩的主要类型;储集空间类型主要以晶间孔、晶间溶孔、溶洞为主,膏膜孔和微裂缝次之;研究区碳酸盐岩储层可划分为Ⅰ类(好)、Ⅱ类(较好)、Ⅲ类(中等)、Ⅳ类(非或差)四种类型,其中马五31和马五14储层较马五21和马五22好,Ⅰ类储层主要发育于马五31和马五14亚段中,Ⅱ类储层在各亚段小层中均有分布,马五1+2和马五14亚段则主要发育Ⅳ和Ⅲ类储层。结果表明:研究区储集岩物性较差,平均孔隙度为2. 86%,平均渗透率为0. 358 4 m D,孔隙度与渗透率之间不存在正相关关系,总体表现为非均质性较强,且低孔、低渗的特征。
The reservoir rock types,reservoir space types and reservoir rock property in Ordovician Majiagou formation M51 + 2 and M514 formation was studied by the observation of the core chip,the casting thin sections,mercury injection test and other technical means. According to the development degree of pore-seams,the combination of pore-seams,the characteristics of capillary pressure curves,gas saturation,effective thickness and the degree of residual hillock development in the carbonate reservoir rocks in the study area,the reservoirs are classified and divided into categories. It is pointed that the types of reservoir rocks in Tao 2 area mainly include dissolved cave-shaped dolomite,mud-powdered dolomite,particulate dolomite and brecciated dolomite; the storage space type mainly consists of intergranular pores,intercrystalline pores and karst caves,the paste pores as well as micro-cracks are secondary. The carbonate reservoirs can be divided into four types which are ClassⅠ( good),ClassⅡ( better),ClassⅢ( medium),ClassⅣ( worse). Among them,M531 and M514 reservoirs are superior than M521 and M522 reservoirs,ClassⅠreservoirs are mainly distributed in M531 and M514 reservoirs; Class Ⅱ reservoirs are distributed in all reservoirs; M51 + 2 and M514 sub-reservoirs are mainly Class Ⅳ and Class Ⅲreservoirs. The results indicate that the reservoir rock property in the study area is poor,the average porosity is 2. 86%,and the mean permeability is 0. 358 4 m D,and there is no positive correlation between porosity and permeability. The overall is characterized by strong heterogeneity,low porosity and low permeability.
The reservoir rock types,reservoir space types and reservoir rock property in Ordovician Majiagou formation M51 + 2 and M514 formation was studied by the observation of the core chip,the casting thin sections,mercury injection test and other technical means. According to the development degree of pore-seams,the combination of pore-seams,the characteristics of capillary pressure curves,gas saturation,effective thickness and the degree of residual hillock development in the carbonate reservoir rocks in the study area,the reservoirs are classified and divided into categories. It is pointed that the types of reservoir rocks in Tao 2 area mainly include dissolved cave-shaped dolomite,mud-powdered dolomite,particulate dolomite and brecciated dolomite; the storage space type mainly consists of intergranular pores,intercrystalline pores and karst caves,the paste pores as well as micro-cracks are secondary. The carbonate reservoirs can be divided into four types which are ClassⅠ( good),ClassⅡ( better),ClassⅢ( medium),ClassⅣ( worse). Among them,M531 and M514 reservoirs are superior than M521 and M522 reservoirs,ClassⅠreservoirs are mainly distributed in M531 and M514 reservoirs; Class Ⅱ reservoirs are distributed in all reservoirs; M51 + 2 and M514 sub-reservoirs are mainly Class Ⅳ and Class Ⅲreservoirs. The results indicate that the reservoir rock property in the study area is poor,the average porosity is 2. 86%,and the mean permeability is 0. 358 4 m D,and there is no positive correlation between porosity and permeability. The overall is characterized by strong heterogeneity,low porosity and low permeability.
引文
[1]雷卞军,卢涛,王东旭,等.靖边气田马五1-4亚段沉积微相和成岩作用研究[J].沉积学报,2010,28(6):1153-1164.LEI Bian-jun,YANG Cheng-yun,WANG Dong-xu,et al. Research on the sedimentary microfacies and digenesis of Ma51-4submember in Jingbian Gas Field[J]. Acta Sedimentologica Sinica,2010,28(6):1153-1164.
[2]包洪平,杨承运.鄂尔多斯东部奥陶系马家沟组微相分析[J].古地理学报,2000(1):31-42.BAO Hong-ping,YANG Cheng-yun. Study on microfacies of Majiagou Formation,Lower Ordovician,eastern Ordos,north China[J]. Journal of Palaeo Geography,2000,2(1):31-42.
[3]邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003(2):34.DI Ling-jun,ZHANG Dong-yang,WANG Hong-ke. Primary discussion on Himalayan tectonic movement and petroleum reservoir in Ordos Basin[J]. Acta Petrolei Sinica,2003,24(2):34-37.
[4]曹红霞,吴海燕,尚婷,等.延安地区马家沟组风化壳型储层孔隙结构及分类评价[J].西安科技大学学报,2018,38(3):426-434.CAO Hong-xia,WU Hai-yan,SHANG Ting,et al. Pore structure and classification evaluation of the weathered crust type reservoir of the Majiagou Formation in Yan’an Area[J]. Journal of Xi’an University of Science and Technology,2018,38(3):426-434.
[5]杨伟利,王起琮,刘佳玮,等.鄂尔多斯盆地奥陶系马家沟组标准化层序地层学研究[J].西安科技大学学报,2017,37(2):234-241.YANG Li-wei,WANG Qi-cong,LIU Jia-wei,et al.Standardization of sequence stratigraphy in Ordovician Majiagou formation,Ordos Basin[J]. Journal of Xi’an University of Science&Technology,2017,37(2):234-241.
[6]余朱宇.苏里格气田桃2区块马五段气、水分布规律及其主控因素[D].西安:西北大学,2017.YU Zhu-yu. The gas and water distribution pattern and the main controlling factors in Ma5 Member of Tao2 well area,Sulige Gas Field[D]. Xi’an:Northwest University,2017.
[7]刘占良,石万里,柳洁,等.鄂尔多斯盆地乌审旗东区马五1-4亚段碳酸盐岩储层孔隙特征与成因[J].西北大学学报(自然科学版),2016,46(1):94-104.LIU Zhan-liang,SHI Wan-li,LIU Jie,et al. The characteristics and genetisises of porosity carbonate reservoir from Ma51-4submember,eastern Wushenqi in Ordos Basi[J]. Journal of Northwest University(Natural Science Edition),2016,46(1):94-104.
[8]王起琮,赵淑萍,魏钦廉,等.鄂尔多斯盆地中奥陶统马家沟组海相碳酸盐岩储集层特征[J].古地理学报,2012,14(2):229-242.WANG Qi-cong,ZHAO Shu-ping,WEI Qin-lian,et al.Marine carbonate reservoir characteristics of the middle Ordovician Majiagou formation in Ordos Basin[J]. Journal of Palaeogeography,2012,14(2):229-242.
[9]胡明毅,朱忠德,刘秉理.鄂中地区下奥陶统碳酸盐岩成岩作用及孔隙演化[J].矿物岩石,1994(2):47-54.HU Ming-yi,ZHU Zhong-de,LIU Bing-cheng. The diagenesis and porosity evolution of lower Ordovician carbonate rocks in central Hubbei[J]. Mineral Petrol,1994(2):47-54.
[10]郭彦如,付金华,魏新善,等.鄂尔多斯盆地奥陶系碳酸盐岩成藏特征与模式[J].石油勘探与开发,2014,41(4):393-403.GUO Yan-ru,FU Jin-hua,WEI Xin-Shan,et al. Natural gas accumulation and models in Ordovician carbonates,Ordos Basin,China[J]. Petroleum Exploration and Development,2014,41(4):393-403.
[11]杨华,包洪平.鄂尔多斯盆地奥陶系中组合成藏特征及勘探启示[J].天然气工业,2011,31(12):11-20.YANG Hua,BAO Hong-ping. Characteristics of hydrocarbon accumulation in the middle Ordovician assemblages and their significance for gas exploration in the Ordos Basin.[J]. Natural Gas Industry,2011,31(12):11-20.
[12]韩波,冯乔,赵振宇,等.鄂尔多斯盆地中东部奥陶系风化壳岩溶特征及储层分析[J].海洋地质前沿,2011,27(5):24-30.HAN Bo,FENG Qiao,ZHAO Zhen-yu,et al. Ordovician karst weathering crust and reservoirs in central and eastern Ordos Basin[J]. Marine Geology Frontiers,2011,27(5):24-30.
[13]李振宏,胡健民.鄂尔多斯盆地构造演化与古岩溶储层分布[J].石油与天然气地质,2010,31(5):640-647.LI Zhen-hong,HU Jian-min. Structural evolution and distribution of paleokarst reservoirs in the Ordos Basin[J]. Oil&Gas Geology,2010,31(5):640-647.
[14]王雪莲,王长陆,陈振林,等.鄂尔多斯盆地奥陶系风化壳岩溶储层研究[J].特种油气藏,2005(3):32-35.WANG Xue-lian,WANG Chang-lu,CHEN Zhen-lin,et al. Study of ordovician weathering crust karst reservoirs in Ordos Basin[J]. Special Oil and Gas Reservoirs,2005(3):32-35.
[15]杨华,黄道军,郑聪斌.鄂尔多斯盆地奥陶系岩溶古地貌气藏特征及勘探进展[J].石油地质,2006(3):1-12.YANG Hua,HUANG Dao-jun,ZHENG Cong-bin. Characteristics of gas reservoir and exploration achievement for ordovician paleokarst landform in Ordos Basin[J].Petroleum Geology,2006(3):1-12.
[16]雷卞军,刘斌,李世临,等.致密砂岩成岩作用及其对储层的影响[J].西南石油大学学报(自然科学版),2008,30(6):57-61.LEI Bian-jun,LIU Bin,LI Shi-lin,et al. Digenesis of tight sandstone and the influence on reservoir[J]. Journal of Southwest Petroleum University(Science Technology Edition),2008,30(6):57-61.
[17]王作乾,何顺利.靖边下古生界气藏马五段碳酸盐岩储层综合评价[J].石油天然气学报,2009,31(4):180-182.WANG Zuo-qian,HE Shun-li. Integrated evaluation of carbonate reservoir for Om5 of lower Paleozoic gas reservoir in Jing bian Area[J]. Journal of Oil and Gas Technology,2009,31(4):180-192.
[18]冉新权,程启贵,屈雪峰,等.特低渗透砂岩油藏水平井井网形式研究[J].石油学报,2008(1):89-92.RAN Xin-quan,CHENG Qi-gui,QU Xue-feng,et al.Study on horizontal well pattern in ultra-low permeability sandstone reservoir[J]. Acta Petrolei Sonica,2008,29(1):89-92.
[19]赵振宇,郭彦如,王艳,等.鄂尔多斯盆地构造演化及古地理特征研究进展[J].特种油气藏,2012,19(5):15-20.ZHAO Zhen-yu,GUO Yan-ru,WANG Yan,et al. Study progress in tectonic evolution and palegeography of Ordos Basin[J]. Special Oil and Gas Reservoirs,2012,19(5):15-20.
[20]李振宏,胡健民.鄂尔多斯盆地构造演化与古岩溶储层分布[J].石油与天然气地质,2010,31(5):640-647.LI Zhen-bong,HU Jian-min. Structural evolution and distribution of paleo karst reservoirs in the Ordos Basin[J]. Oil&Gas Geology,2010,31(5):641-647.
[21]侯方浩,方少仙,何江,等.鄂尔多斯盆地靖边气田区中奥陶统马家沟组马五1~马五4亚段古岩溶型储层分布特征及综合评价[J].海相油气地质,2011,16(1):1-13.HOU Fang-hao,FANG Shao-xian,DONG Zhao-xiong,et al. Distribution characters and comprehensive evaluationof middle Ordovician Majiagou 51-54 Submembers Reservoirs in Jingbian Gas field Area[J]. Ordos Basin,2011,16(1):1-13.
[22]丁熊,谭秀成,罗冰,等.基于灰色模糊理论的多参数碳酸盐岩储层评价[J].西南石油大学学报(自然科学版),2008(5):88-92.DING Xiong,TAN Xiu-cheng,LUO Bing,et al Multi-parameter carbonate rock reservoirs evaluation based on grey fuzzy theory[J]. Journal of Southwest Petroleum University(Science Technology Edition),2008,30(5):88-92.
[23]朱兆群,林承焰,张苏杰,等.改进的模糊-灰色综合评判方法在储层定量评价中的应用—以苏里格气田苏X井区盒8下亚段低渗透气藏为例[J].石油与天然气地质,2017,38(1):197-208.ZHU Zhao-qun,LIN Cheng-yan,ZHANG Su-jie,et al.Application of improved fuzzy-grey comprehensive evaluation method to quantitative reservoir evaluation:A case study of the low-permeability gas reservoirs of the lower part of 8th member of the Shi he zi formation in Su X block of Sulige gas field[J]. Oil&Gas Geology,2017,38(1):197-208
[24]陈欢庆,丁超,杜宜静,等.储层评价研究进展[J].地质科技情报,2015,34(5):66-74.CHEN Huan-qing,DING Chao,DU Yi-jing,et al. Advances of reservoir evaluation researches[J]. Geological Science and Technology Information,2015,34(5):66-74.
[25]王小敏,樊太亮.碳酸盐岩储层渗透率研究现状与前瞻[J].地学前缘,2013,20(5):166-174.WANG Xiao-min,FAN Tai-liang. Progress of research on permeability of carbonate rocks[J]. Earth Science Hrontiers,2013,20(5):166-174.
[26]程启贵,郭少斌,王海红,等.鄂尔多斯盆地中西部长6油层组储层综合评价[J].石油实验地质,2010,32(5):415-419.CHENG Qi-gui,GUO Shao-bin,et al. Comprehensive reservoir evaluation of Chang 6 oil-bearing layers in midwest Ordos Basin[J]. Petroleum Geology&Experiment 2010,32(5):415-419.
[27]唐建云,郭艳琴,宋红霞,等.定边地区侏罗系延安组延9储层成岩作用特征[J].西安科技大学学报,2017,37(6):865-871.TANG Jian-yun,GUO Yan-Qin,SONG Hong-xia,et al.Diagenesis of Yan 9 reservoir of Yan’an Formation of the Jurassic in Dingbian area[J]. Journal of Xi’an University of Science&Technology,2017,37(6):865-871.
[28]刘秀婵,陈西泮,张添锦,等.延安南部曹凡峪油区长6油层组成岩作用研究[J].西安科技大学学报,2014,34(2):194-198.LIU Xiu-chan,CHEN Xi-pan,ZHANG Tian-jin,et al.Chang 6 sandstone diagenesis of Cao fanyu in the south of Yanan[J]. Journal of Xi’an University of Science&Technology,2014,34(02):194-198.
[29]丁熊,谭秀成,雷一文,等.基于模糊聚类分析的复杂碳酸盐岩储层定量评价[J].西安石油大学学报(自然科学版),2009,24(3):25-27.DING Xiong,TAN Xiu-cheng,LEI Yi-wen,et al. Quantitative evaluation of complex carbonate reservoir based on fuzzy cluster analysis[J]. Journal of Xi’an Shiyou University Natural Science Edition,2009,24(3):25-27.
[30]赵永刚,陈景山,李凌,等.基于残余岩溶强度表征和裂缝预测的碳酸盐岩储层评价—以塔中西部上奥陶统良里塔格组为例[J].吉林大学学报(地球科学版),2015,45(1):25-36.ZHAO Yong-gang,CHEN Jing-shan,LI Ling,et al. Evaluation of carbonate reservoir based on residual karsts intensity characterization and structural fracture prediction:a case from the upper Ordovician Liang litage formation in the west of center Trim Basin[J]. Journal of Jilin University(Earth Science Edition),2015,45(1):25-36.
[31]刘森.苏里格T2区块马家沟组主力气藏储层地质特征研究[D].西安:西安石油大学,2017.LIU Sen. The research on reservoir geological characteristics of the major gas reservoirs of Majiagou Formation in Tao2 block Sulige[D]. Xi’an:Xi’an Shiyou University,2017.
[2]包洪平,杨承运.鄂尔多斯东部奥陶系马家沟组微相分析[J].古地理学报,2000(1):31-42.BAO Hong-ping,YANG Cheng-yun. Study on microfacies of Majiagou Formation,Lower Ordovician,eastern Ordos,north China[J]. Journal of Palaeo Geography,2000,2(1):31-42.
[3]邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003(2):34.DI Ling-jun,ZHANG Dong-yang,WANG Hong-ke. Primary discussion on Himalayan tectonic movement and petroleum reservoir in Ordos Basin[J]. Acta Petrolei Sinica,2003,24(2):34-37.
[4]曹红霞,吴海燕,尚婷,等.延安地区马家沟组风化壳型储层孔隙结构及分类评价[J].西安科技大学学报,2018,38(3):426-434.CAO Hong-xia,WU Hai-yan,SHANG Ting,et al. Pore structure and classification evaluation of the weathered crust type reservoir of the Majiagou Formation in Yan’an Area[J]. Journal of Xi’an University of Science and Technology,2018,38(3):426-434.
[5]杨伟利,王起琮,刘佳玮,等.鄂尔多斯盆地奥陶系马家沟组标准化层序地层学研究[J].西安科技大学学报,2017,37(2):234-241.YANG Li-wei,WANG Qi-cong,LIU Jia-wei,et al.Standardization of sequence stratigraphy in Ordovician Majiagou formation,Ordos Basin[J]. Journal of Xi’an University of Science&Technology,2017,37(2):234-241.
[6]余朱宇.苏里格气田桃2区块马五段气、水分布规律及其主控因素[D].西安:西北大学,2017.YU Zhu-yu. The gas and water distribution pattern and the main controlling factors in Ma5 Member of Tao2 well area,Sulige Gas Field[D]. Xi’an:Northwest University,2017.
[7]刘占良,石万里,柳洁,等.鄂尔多斯盆地乌审旗东区马五1-4亚段碳酸盐岩储层孔隙特征与成因[J].西北大学学报(自然科学版),2016,46(1):94-104.LIU Zhan-liang,SHI Wan-li,LIU Jie,et al. The characteristics and genetisises of porosity carbonate reservoir from Ma51-4submember,eastern Wushenqi in Ordos Basi[J]. Journal of Northwest University(Natural Science Edition),2016,46(1):94-104.
[8]王起琮,赵淑萍,魏钦廉,等.鄂尔多斯盆地中奥陶统马家沟组海相碳酸盐岩储集层特征[J].古地理学报,2012,14(2):229-242.WANG Qi-cong,ZHAO Shu-ping,WEI Qin-lian,et al.Marine carbonate reservoir characteristics of the middle Ordovician Majiagou formation in Ordos Basin[J]. Journal of Palaeogeography,2012,14(2):229-242.
[9]胡明毅,朱忠德,刘秉理.鄂中地区下奥陶统碳酸盐岩成岩作用及孔隙演化[J].矿物岩石,1994(2):47-54.HU Ming-yi,ZHU Zhong-de,LIU Bing-cheng. The diagenesis and porosity evolution of lower Ordovician carbonate rocks in central Hubbei[J]. Mineral Petrol,1994(2):47-54.
[10]郭彦如,付金华,魏新善,等.鄂尔多斯盆地奥陶系碳酸盐岩成藏特征与模式[J].石油勘探与开发,2014,41(4):393-403.GUO Yan-ru,FU Jin-hua,WEI Xin-Shan,et al. Natural gas accumulation and models in Ordovician carbonates,Ordos Basin,China[J]. Petroleum Exploration and Development,2014,41(4):393-403.
[11]杨华,包洪平.鄂尔多斯盆地奥陶系中组合成藏特征及勘探启示[J].天然气工业,2011,31(12):11-20.YANG Hua,BAO Hong-ping. Characteristics of hydrocarbon accumulation in the middle Ordovician assemblages and their significance for gas exploration in the Ordos Basin.[J]. Natural Gas Industry,2011,31(12):11-20.
[12]韩波,冯乔,赵振宇,等.鄂尔多斯盆地中东部奥陶系风化壳岩溶特征及储层分析[J].海洋地质前沿,2011,27(5):24-30.HAN Bo,FENG Qiao,ZHAO Zhen-yu,et al. Ordovician karst weathering crust and reservoirs in central and eastern Ordos Basin[J]. Marine Geology Frontiers,2011,27(5):24-30.
[13]李振宏,胡健民.鄂尔多斯盆地构造演化与古岩溶储层分布[J].石油与天然气地质,2010,31(5):640-647.LI Zhen-hong,HU Jian-min. Structural evolution and distribution of paleokarst reservoirs in the Ordos Basin[J]. Oil&Gas Geology,2010,31(5):640-647.
[14]王雪莲,王长陆,陈振林,等.鄂尔多斯盆地奥陶系风化壳岩溶储层研究[J].特种油气藏,2005(3):32-35.WANG Xue-lian,WANG Chang-lu,CHEN Zhen-lin,et al. Study of ordovician weathering crust karst reservoirs in Ordos Basin[J]. Special Oil and Gas Reservoirs,2005(3):32-35.
[15]杨华,黄道军,郑聪斌.鄂尔多斯盆地奥陶系岩溶古地貌气藏特征及勘探进展[J].石油地质,2006(3):1-12.YANG Hua,HUANG Dao-jun,ZHENG Cong-bin. Characteristics of gas reservoir and exploration achievement for ordovician paleokarst landform in Ordos Basin[J].Petroleum Geology,2006(3):1-12.
[16]雷卞军,刘斌,李世临,等.致密砂岩成岩作用及其对储层的影响[J].西南石油大学学报(自然科学版),2008,30(6):57-61.LEI Bian-jun,LIU Bin,LI Shi-lin,et al. Digenesis of tight sandstone and the influence on reservoir[J]. Journal of Southwest Petroleum University(Science Technology Edition),2008,30(6):57-61.
[17]王作乾,何顺利.靖边下古生界气藏马五段碳酸盐岩储层综合评价[J].石油天然气学报,2009,31(4):180-182.WANG Zuo-qian,HE Shun-li. Integrated evaluation of carbonate reservoir for Om5 of lower Paleozoic gas reservoir in Jing bian Area[J]. Journal of Oil and Gas Technology,2009,31(4):180-192.
[18]冉新权,程启贵,屈雪峰,等.特低渗透砂岩油藏水平井井网形式研究[J].石油学报,2008(1):89-92.RAN Xin-quan,CHENG Qi-gui,QU Xue-feng,et al.Study on horizontal well pattern in ultra-low permeability sandstone reservoir[J]. Acta Petrolei Sonica,2008,29(1):89-92.
[19]赵振宇,郭彦如,王艳,等.鄂尔多斯盆地构造演化及古地理特征研究进展[J].特种油气藏,2012,19(5):15-20.ZHAO Zhen-yu,GUO Yan-ru,WANG Yan,et al. Study progress in tectonic evolution and palegeography of Ordos Basin[J]. Special Oil and Gas Reservoirs,2012,19(5):15-20.
[20]李振宏,胡健民.鄂尔多斯盆地构造演化与古岩溶储层分布[J].石油与天然气地质,2010,31(5):640-647.LI Zhen-bong,HU Jian-min. Structural evolution and distribution of paleo karst reservoirs in the Ordos Basin[J]. Oil&Gas Geology,2010,31(5):641-647.
[21]侯方浩,方少仙,何江,等.鄂尔多斯盆地靖边气田区中奥陶统马家沟组马五1~马五4亚段古岩溶型储层分布特征及综合评价[J].海相油气地质,2011,16(1):1-13.HOU Fang-hao,FANG Shao-xian,DONG Zhao-xiong,et al. Distribution characters and comprehensive evaluationof middle Ordovician Majiagou 51-54 Submembers Reservoirs in Jingbian Gas field Area[J]. Ordos Basin,2011,16(1):1-13.
[22]丁熊,谭秀成,罗冰,等.基于灰色模糊理论的多参数碳酸盐岩储层评价[J].西南石油大学学报(自然科学版),2008(5):88-92.DING Xiong,TAN Xiu-cheng,LUO Bing,et al Multi-parameter carbonate rock reservoirs evaluation based on grey fuzzy theory[J]. Journal of Southwest Petroleum University(Science Technology Edition),2008,30(5):88-92.
[23]朱兆群,林承焰,张苏杰,等.改进的模糊-灰色综合评判方法在储层定量评价中的应用—以苏里格气田苏X井区盒8下亚段低渗透气藏为例[J].石油与天然气地质,2017,38(1):197-208.ZHU Zhao-qun,LIN Cheng-yan,ZHANG Su-jie,et al.Application of improved fuzzy-grey comprehensive evaluation method to quantitative reservoir evaluation:A case study of the low-permeability gas reservoirs of the lower part of 8th member of the Shi he zi formation in Su X block of Sulige gas field[J]. Oil&Gas Geology,2017,38(1):197-208
[24]陈欢庆,丁超,杜宜静,等.储层评价研究进展[J].地质科技情报,2015,34(5):66-74.CHEN Huan-qing,DING Chao,DU Yi-jing,et al. Advances of reservoir evaluation researches[J]. Geological Science and Technology Information,2015,34(5):66-74.
[25]王小敏,樊太亮.碳酸盐岩储层渗透率研究现状与前瞻[J].地学前缘,2013,20(5):166-174.WANG Xiao-min,FAN Tai-liang. Progress of research on permeability of carbonate rocks[J]. Earth Science Hrontiers,2013,20(5):166-174.
[26]程启贵,郭少斌,王海红,等.鄂尔多斯盆地中西部长6油层组储层综合评价[J].石油实验地质,2010,32(5):415-419.CHENG Qi-gui,GUO Shao-bin,et al. Comprehensive reservoir evaluation of Chang 6 oil-bearing layers in midwest Ordos Basin[J]. Petroleum Geology&Experiment 2010,32(5):415-419.
[27]唐建云,郭艳琴,宋红霞,等.定边地区侏罗系延安组延9储层成岩作用特征[J].西安科技大学学报,2017,37(6):865-871.TANG Jian-yun,GUO Yan-Qin,SONG Hong-xia,et al.Diagenesis of Yan 9 reservoir of Yan’an Formation of the Jurassic in Dingbian area[J]. Journal of Xi’an University of Science&Technology,2017,37(6):865-871.
[28]刘秀婵,陈西泮,张添锦,等.延安南部曹凡峪油区长6油层组成岩作用研究[J].西安科技大学学报,2014,34(2):194-198.LIU Xiu-chan,CHEN Xi-pan,ZHANG Tian-jin,et al.Chang 6 sandstone diagenesis of Cao fanyu in the south of Yanan[J]. Journal of Xi’an University of Science&Technology,2014,34(02):194-198.
[29]丁熊,谭秀成,雷一文,等.基于模糊聚类分析的复杂碳酸盐岩储层定量评价[J].西安石油大学学报(自然科学版),2009,24(3):25-27.DING Xiong,TAN Xiu-cheng,LEI Yi-wen,et al. Quantitative evaluation of complex carbonate reservoir based on fuzzy cluster analysis[J]. Journal of Xi’an Shiyou University Natural Science Edition,2009,24(3):25-27.
[30]赵永刚,陈景山,李凌,等.基于残余岩溶强度表征和裂缝预测的碳酸盐岩储层评价—以塔中西部上奥陶统良里塔格组为例[J].吉林大学学报(地球科学版),2015,45(1):25-36.ZHAO Yong-gang,CHEN Jing-shan,LI Ling,et al. Evaluation of carbonate reservoir based on residual karsts intensity characterization and structural fracture prediction:a case from the upper Ordovician Liang litage formation in the west of center Trim Basin[J]. Journal of Jilin University(Earth Science Edition),2015,45(1):25-36.
[31]刘森.苏里格T2区块马家沟组主力气藏储层地质特征研究[D].西安:西安石油大学,2017.LIU Sen. The research on reservoir geological characteristics of the major gas reservoirs of Majiagou Formation in Tao2 block Sulige[D]. Xi’an:Xi’an Shiyou University,2017.