莺歌海盆地东方区黄流组高温超压砂岩储集层发育机理
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摘要
莺歌海盆地东方区黄流组砂岩具有明显的高温超压环境成岩特征。通过岩石薄片、阴极发光、扫描电镜、包裹体测温和X衍射等研究手段,对黄流组砂岩在高温超压下的成岩特征进行了研究,并分析了成岩作用对储集性能的影响。高温超压下黄流组砂岩具有弱压实、强溶蚀的特点,并结晶了菱铁矿、重晶石和金红石等热液成因的自生矿物。高温超压环境下不仅原生孔隙被大量保存,而且高温热流体对长石类矿物的溶蚀也有利于大量次生孔隙的形成。菱铁矿、铁方解石和铁白云石的胶结和自生高岭石的充填使储集层孔隙度降低,而蒙脱石向伊利石的快速转化是储集层渗透率急剧下降的主要因素。研究结果表明,高温超压不仅对于砂岩储集层原生孔隙起到保护作用,也导致了不稳定矿物的大量溶蚀。高温超压下储集层发育机理的研究对于砂岩中"甜点"储集层的预测具有重要意义。
The sandstone of Huangliu formation in Dongfang area of Yinggehai basin is characterized by obvious high-temperature and overpressure diagenetic environment. By means of thin section,cathodeluminescence,SEM,enclosure,X-ray,etc,this paper studied the diagenetic characteristic of Huangliu sand under high-temperature and overpressure and its effect on the reservoir quality. This sandstone with poor compaction and strong corrosion has crystallized with such authigenic minerals of hydrothermal origin as siderite,barite and rutile,etc. Under the high-temperature and overpressure,the primary porosity was not only preserved mostly,but also favorable to forming a great amount of secondary pores for dissolution of the high temperature hydrothermal fluid on feldspathic mineral. The cementing of siderite,ferrocalcite and ferrodolomite and the filling of authigenic kaolinite were resulted in lower porosity of the reservoir,while the rapid smectite-illite conversion could be the main reason for quick decline of the reservoir permeability. The studied result shows that the hightemperature and overpressure could not only preserve the primary porosity in this reservoir,but also result in a great amount of corrosion of unstable minerals. Conducting research of the reservoir development mechanism under high-temperature and overpressure is of great significance for prediction of"dessert"in the sandstone reservoir.
The sandstone of Huangliu formation in Dongfang area of Yinggehai basin is characterized by obvious high-temperature and overpressure diagenetic environment. By means of thin section,cathodeluminescence,SEM,enclosure,X-ray,etc,this paper studied the diagenetic characteristic of Huangliu sand under high-temperature and overpressure and its effect on the reservoir quality. This sandstone with poor compaction and strong corrosion has crystallized with such authigenic minerals of hydrothermal origin as siderite,barite and rutile,etc. Under the high-temperature and overpressure,the primary porosity was not only preserved mostly,but also favorable to forming a great amount of secondary pores for dissolution of the high temperature hydrothermal fluid on feldspathic mineral. The cementing of siderite,ferrocalcite and ferrodolomite and the filling of authigenic kaolinite were resulted in lower porosity of the reservoir,while the rapid smectite-illite conversion could be the main reason for quick decline of the reservoir permeability. The studied result shows that the hightemperature and overpressure could not only preserve the primary porosity in this reservoir,but also result in a great amount of corrosion of unstable minerals. Conducting research of the reservoir development mechanism under high-temperature and overpressure is of great significance for prediction of"dessert"in the sandstone reservoir.
引文
[1]王华,朱伟林,王彦.莺歌海盆地充填史及中-深层储层特征[J].石油与天然气地质,1999,20(1):55-57.Wang Hua,Zhu Weilin,Wang Yan.Characteristics of medium-deep reservoir and sedimentary history in Yinggehai basin[J].Oil&Gas Geology,1999,20(1):55-57.
[2]彭伟欣,叶丛英.中国近海油气资源开发现状及前景[J].海洋石油,1999,10(3):21-26.Peng Weixin,Ye Congying.Review and prospects of petroleum exploitation,the offshore of China[J].Offshore Oil,1999,10(3):21-26.
[3]朱芳冰.莺歌海盆地地层压力特征及石油地质意义[J].中国海上油气(地质),2000,14(4):248-252.Zhu Fangbing.Characteristics of geopressure in Yinggehai basin and its significance in petroleum geology[J].China Offshore Oil and Gas(Geology),2000,14(4):248-252.
[4]何家雄,夏斌,张树林,等.莺歌海盆地泥底辟成因、展布特征及其与天然气运聚成藏关系[J].中国地质,2006,33(6):1 336-1344.He Jiaxiong,Xia Bin,Zhang Shulin,et al.Origin and distribution of mud diapirs in the Yinggehai basin and their relation to the migration and accumulation of natural gas[J].Geology in China,2006,33(6):1 336-1 344.
[5]李纯泉,张健.莺歌海盆地流体底辟构造及其成藏贡献[J].天然气勘探与开发,2000,23(3):35-39.Li Cunquan,Zhang Jian.The fluid diapirs structure and accumulation contribution in Yinggehai basin[J].Natural Gas Exploration and Development,2000,23(3):35-39.
[6]解习农,李思田,胡祥云,等.莺歌海盆地底辟带热流体输导系统及其成因机制[J].中国科学D辑:地球科学,1999,29(3):247-255.Xie Xinong,Li Sitian,Hu Xiangyun,et al.The hot fluid conduction system and contributing factor in diapirs zone of Yinggehai Basin[J].Science in China(Series D):Earth Sciences,1999,29(3):247-255.
[7]谢玉洪,刘平,黄志龙.莺歌海盆地高温超压天然气成藏地质条件及成藏过程[J].天然气工业,2012,32(4):19-23.Xie Yuhong,Liu Ping,Huang Zhilong.Geological conditions and pooling process of high-temperature and overpressure natural gas reseviors in the Yinggehai basin[J].Natural Gas Industry,2012,32(4):19-23.
[8]谢玉洪,张迎朝,李绪深,等.莺歌海盆地高温超压气藏控藏要素与成藏模式[J].石油学报,2012,33(4):601-609.Xie Yuhong,Zhang Yingchao,Li Xushen,et al.Main controlling factors and formation models of natual gas reservoirs with high temperature and overpressure in Yinggehai basin[J].Acta Petrolei Sinica,2012,33(4):601-609.
[9]张国华.南海西部大气区烃源潜力[J].天然气工业,1999,19(1):18-21.Zhang Guohua.Hydrocarbon resources in the giant gas area in the western South China Sea[J].Natural Gas Industry,1999,19(1):18-21.
[10]孟凡晋,肖丽华,谢玉洪,等.莺海盆地粘土矿物异常转化及其地质意义[J].沉积学报,2012,30(3):469-476.Meng Fanjin,Xiao Lihua,Xie Yuhong,et al.Abnormal transformation of the clay minerals in the Yinggehai basin and its significances[J].Acta Sedimentologica Sinica,2012,30(3):469-476.
[11]张伙兰,裴健翔,张迎朝,等.莺歌海盆地东方区中深层黄流组超压储集层特征[J].石油勘探与开发,2013,40(3):284-293.Zhang Huolan,Pei Jianxiang,Zhang Yingchao,et al.Overpressure reservoirs in the mid-deep Huangliu formation of Dongfang area,Yinggehai basin,South China Sea[J].Petroleum Exploration and Development,2013,40(3):284-293.
[12]Gluyas J,Cade C A.Prediction of porosity in compacted sands[C].AAPG Memoir 69:Reservoir quality prediction in sandstones and carbonates.Tulsa:AAPG,1997.
[13]董伟良.南海西部莺-琼盆地天然气勘探领域分析[J]天然气工业,1999,19(1):7-11.Dong Weiliang.An analysis of the the natural gas exploration areas in Yingqiong basin in western South China Sea[J].Natural Industry,1999,19(1):7-11.
[14]郝怡纯,陈平富,万晓樵,等.南海北部莺歌海-琼东南盆地晚第三纪层序地层与海平面变化[J].现代地质,2000,14(3):237-245.Hao Yichun,Chen Pingfu,Wan Xiaoqiao,et al.Late Tertiary sequence stratigraphy and sea level changes in Yinggehai-Qiongdongnan basin[J].Geoscience,2000,14(3):237-245.
[15]钟志洪,王良斌,夏斌,等.莺歌海成因及其大地构造[J].地质学报,2004,78(3):237-245.Zhong Zhihong,Wang Liangbin,Xia Bin,et al.The dynamics of Yinggehai basin formation and its tectonic significance[J].Acta Geologica Sinica,2004,78(3):237-245.
[16]谢玉洪.构造活动型盆地层序地层分析及天然气成藏模式——以莺歌海盆地为例[M].北京:地质出版社,2009:32,55-58.Xie Yuhong.The analysis of sequence of strata in structure tectonic activity basin and accumulation style—taking Yinggehai basin as an example[M].Beijing:Geology Press,2009:32,55-58.
[17]吕明.莺-琼盆地含气区储层特征[J].天然气工业,1999,19(1):20-24.LüMing.Reservior characteristics of gas-bearing area in YingQiong basin[J].Natural Gas Industry,1999,19(1):20-24.
[18]谢玉洪,范彩伟.莺歌海盆地黄流组储层成因新认识[J].中国海上油气,2010,22(6):355-399.Xie Yuhong,Fan Caiwei.Some new knowledge about the origin of Huangliu Formation reservoirs in Dongfang area,Yinggehai basin[J].China Offshore Oil and Gas,2010,22(6):355-399.
[19]王振峰,胡代圣.莺歌海盆地中央泥拱构造带大气田勘探方向[J].天然气工业,1999,19(1):28-30.Wang Zhenfeng,Hu Daisheng.Prospecting for giant gas fields in the central mud diapis structure belt in Yinggehai basin[J].Natural Gas Industry,1999,19(1):28-30.
[20]赵艳,吴胜和,徐樟有,等.川西新场气田上三叠统须家河组二段致密砂岩优质储层控制因素[J].中国石油大学学报:自然科学版,2010,34,(4):1-4.Zhao Yan,Wu Shenghe,Xu Zhangyou,et al.Control factors of compacted high-quality sandstone reservoirs of member 2 of Xujiahe formation,Upper Triassic in Xinchang gasfield of western Sichuan depression[J].Journal of China University of Petroleum,2010,34,(4):1-4.
[21]黄思静,黄培培,王庆东,等.胶结作用在深埋藏砂岩孔隙保存中的意义[J].岩性油气藏,2007,19(3):7-12.Huang Sijing,Huang Peipei,Wang Qingdong,et,al.The significance of cementation in porosity preservation in deep buried sandstones[J].Lothologic Reserviors,2007,19(3):7-12.
[22]刘晓峰,解习农.储层超压流体系统的成因机制述评[J].地质科技情报,2003,22(3):56-59.Liu Xiaofeng,Xie Xinong.Review of formation mechanism of the reservoirs overpressure fuild system[J].Geological Science and Technology Information,2003,22(3):56-59.
[23]Bloch S,Helmod K P.Approaches to predicting reservoir quality of sandstones[J].AAPG Bulletin,1995,79(1):97-144.
[24]Perry E A.Hower J.Late-stage dehydration in deeply buried pelitic sediments[J].AAPG Bulletin,1972,56(10):2 013-2 021.
[25]Colten-Bradley V A.Role of pressure in smectite dehydration;effects on geopressure and smectite-to-illite transformation[J].AAPG Bulletin,1987,71(11):1 414-1 472.
[26]孟元林,魏巍,王维安,等.超压背景下黏土矿物转化的优化模型[J].吉林大学学报:地球科学版,2012,42(增刊1):145-152.Meng Yuanlin,Wei Wei,Wang Weian,et al.An optimization model of clay mineral transformation under overpressure setting[J].Journal of Jilin University:Earth Science Edition,2012,42(suppl1):145-152.
[27]孟元林,刘德来,贺如,等.歧北凹陷沙二段超压背景下的成岩场分析与储层孔隙度预测[J].沉积学报,2005,23(3):389-396.Meng Yuanlin,Liu Delai,He Ru,et al.Diagenetic field analysis and porosity prediction of the Shaer member(Es2)in overpressure setting in the Qibei depression[J].Acta Sedimentologica Sinica2005,23(3):389-396.
[28]Nordgard Bolas H M,Hermanrud C,Teige G M G.Origin of overpressures in shales:constraints from basin modeling[J].AAPG Bulletin,2004,88(2):193-211.
[29]史基安,王琪.影响碎屑岩天然气储层物性的主要控制因素[J].沉积学报,1995,13(2):128-139.Shi Ji’an,Wang Qi.A disscussion on main controlling factors on the properties of clastic gas reservoirs[J].Acta Sedimentologica Sinica,1995,13(2):128-139.
[30]刘得光.准噶尔盆地马桥凸起异常高压成因及油气成藏模式[J].石油勘探与开发,1998,25(1):21-25.Liu Deguang.Over pressure origin and hydrocarbon pool forming mode of Maqiao uplift in Junggar basin[J].Petroleum Exploration and Development,1998,25(1):21-25.
[31]赵永刚,王萌,蒋裕强,等.公山庙地区沙一段低渗砂岩储层成岩作用及其对储层的影响[J].西安石油大学学报:自然科学版,2010,25(6):17-20.Zhao Yonggang,Wang Meng,Jiang Yuqiang,et al.Diagenesis of the low-permeability sandstone reservoir of the first member of Shahejie formation in Gongshanmiao area and its influence on the reservoir property[J].Journal of Xi’an Shiyou University:Natural Science Edition,2010,25(6):17-20.
[32]孟元林,李亚光,牛嘉玉,等.渤海湾盆地北部深层碎屑岩储层孔隙度影响因素探讨[J].中国海上油气,2007,19(3):154-158.Meng Yuanlin,Li Yaguang,Niu Jiayu,et al.A discussion on factors to control porosity of deep-buried clastic reservoirs in the northern Bohai Bay basin[J].China Offshore Oil and Gas,2007,19(3):154-158.
[33]张惠良,张荣虎,王月华,等.粘土膜对砂岩储集性能的影响——以塔里木盆地群6井区泥盆系东河塘组下段为例[J].石油实验地质,2006,28(5):493-496.Zhang Huiliang,Zhang Ronghu,Wang Yuehua,et al.Influence of clay minerals membrane on sandstone reservoirs—A case study on the lower Donghetang reservoirs of the Devonian of Well Qun6 in Tarim basin[J].Petroleum Geology&Experiment,2006,28(5):493-496.
[34]朱平,黄思静,李德敏,等.粘土矿物绿泥石对碎屑储集岩孔隙的保护[J].成都理工大学学报:自然科学版,2004,31(2):153-158.Zhu Ping,Huang Sijing,Li Demin,et al.Effect and protection of chlorite on clastic reservoir rocks[J].Journal of Chengdu University of Technology:Natural Science Edition,2004,31(2):153-158.
[35]伏美燕,张哨楠,丁晓琪,等.松辽盆地松科1井明水组砂岩粘土膜特征及油气地质意义[J].石油实验地质,2012,34(6):587-590.Fu Meiyan,Zhang Shaonan,Ding Xiaoqi,et al.Characteristics and petroleum geologic significances of clay rims in sandstones of Mingshui formation,Well Songke 1,Songliao basin[J].Petroleum Geology&Experiment,2012,34(6):587-590.
[36]丁晓琪,张哨楠.镇泾地区延长组碎屑岩古风化壳研究[J].西南石油大学学报:自然科学版,2010,32(4):16-20.Ding Xiaoqi,Zhang Shaonan.Study on the weathered crust of conglomerate in Upper Triassic Yanchang formation of Zhenjing field[J].Journal of Southwest Petroleum University:Natural Science Edition,2010,32(4):16-20.
[37]王新民,郭彦如,付金华,等.鄂尔多斯盆地延长组长8段相对高孔渗砂岩储集层的控制因素分析[J].石油勘探与开发,2005,32(2):35-40.Wang Xinmin,Guo Yanru,Fu Jinhua,et al.Controlling factors for forming higher porosity and permeability sandstone reservoirs in Chang 8 member of Yanchang formation,Ordos basin[J].Petroleum Exploration and Development,2005,32(2):35-40.
[2]彭伟欣,叶丛英.中国近海油气资源开发现状及前景[J].海洋石油,1999,10(3):21-26.Peng Weixin,Ye Congying.Review and prospects of petroleum exploitation,the offshore of China[J].Offshore Oil,1999,10(3):21-26.
[3]朱芳冰.莺歌海盆地地层压力特征及石油地质意义[J].中国海上油气(地质),2000,14(4):248-252.Zhu Fangbing.Characteristics of geopressure in Yinggehai basin and its significance in petroleum geology[J].China Offshore Oil and Gas(Geology),2000,14(4):248-252.
[4]何家雄,夏斌,张树林,等.莺歌海盆地泥底辟成因、展布特征及其与天然气运聚成藏关系[J].中国地质,2006,33(6):1 336-1344.He Jiaxiong,Xia Bin,Zhang Shulin,et al.Origin and distribution of mud diapirs in the Yinggehai basin and their relation to the migration and accumulation of natural gas[J].Geology in China,2006,33(6):1 336-1 344.
[5]李纯泉,张健.莺歌海盆地流体底辟构造及其成藏贡献[J].天然气勘探与开发,2000,23(3):35-39.Li Cunquan,Zhang Jian.The fluid diapirs structure and accumulation contribution in Yinggehai basin[J].Natural Gas Exploration and Development,2000,23(3):35-39.
[6]解习农,李思田,胡祥云,等.莺歌海盆地底辟带热流体输导系统及其成因机制[J].中国科学D辑:地球科学,1999,29(3):247-255.Xie Xinong,Li Sitian,Hu Xiangyun,et al.The hot fluid conduction system and contributing factor in diapirs zone of Yinggehai Basin[J].Science in China(Series D):Earth Sciences,1999,29(3):247-255.
[7]谢玉洪,刘平,黄志龙.莺歌海盆地高温超压天然气成藏地质条件及成藏过程[J].天然气工业,2012,32(4):19-23.Xie Yuhong,Liu Ping,Huang Zhilong.Geological conditions and pooling process of high-temperature and overpressure natural gas reseviors in the Yinggehai basin[J].Natural Gas Industry,2012,32(4):19-23.
[8]谢玉洪,张迎朝,李绪深,等.莺歌海盆地高温超压气藏控藏要素与成藏模式[J].石油学报,2012,33(4):601-609.Xie Yuhong,Zhang Yingchao,Li Xushen,et al.Main controlling factors and formation models of natual gas reservoirs with high temperature and overpressure in Yinggehai basin[J].Acta Petrolei Sinica,2012,33(4):601-609.
[9]张国华.南海西部大气区烃源潜力[J].天然气工业,1999,19(1):18-21.Zhang Guohua.Hydrocarbon resources in the giant gas area in the western South China Sea[J].Natural Gas Industry,1999,19(1):18-21.
[10]孟凡晋,肖丽华,谢玉洪,等.莺海盆地粘土矿物异常转化及其地质意义[J].沉积学报,2012,30(3):469-476.Meng Fanjin,Xiao Lihua,Xie Yuhong,et al.Abnormal transformation of the clay minerals in the Yinggehai basin and its significances[J].Acta Sedimentologica Sinica,2012,30(3):469-476.
[11]张伙兰,裴健翔,张迎朝,等.莺歌海盆地东方区中深层黄流组超压储集层特征[J].石油勘探与开发,2013,40(3):284-293.Zhang Huolan,Pei Jianxiang,Zhang Yingchao,et al.Overpressure reservoirs in the mid-deep Huangliu formation of Dongfang area,Yinggehai basin,South China Sea[J].Petroleum Exploration and Development,2013,40(3):284-293.
[12]Gluyas J,Cade C A.Prediction of porosity in compacted sands[C].AAPG Memoir 69:Reservoir quality prediction in sandstones and carbonates.Tulsa:AAPG,1997.
[13]董伟良.南海西部莺-琼盆地天然气勘探领域分析[J]天然气工业,1999,19(1):7-11.Dong Weiliang.An analysis of the the natural gas exploration areas in Yingqiong basin in western South China Sea[J].Natural Industry,1999,19(1):7-11.
[14]郝怡纯,陈平富,万晓樵,等.南海北部莺歌海-琼东南盆地晚第三纪层序地层与海平面变化[J].现代地质,2000,14(3):237-245.Hao Yichun,Chen Pingfu,Wan Xiaoqiao,et al.Late Tertiary sequence stratigraphy and sea level changes in Yinggehai-Qiongdongnan basin[J].Geoscience,2000,14(3):237-245.
[15]钟志洪,王良斌,夏斌,等.莺歌海成因及其大地构造[J].地质学报,2004,78(3):237-245.Zhong Zhihong,Wang Liangbin,Xia Bin,et al.The dynamics of Yinggehai basin formation and its tectonic significance[J].Acta Geologica Sinica,2004,78(3):237-245.
[16]谢玉洪.构造活动型盆地层序地层分析及天然气成藏模式——以莺歌海盆地为例[M].北京:地质出版社,2009:32,55-58.Xie Yuhong.The analysis of sequence of strata in structure tectonic activity basin and accumulation style—taking Yinggehai basin as an example[M].Beijing:Geology Press,2009:32,55-58.
[17]吕明.莺-琼盆地含气区储层特征[J].天然气工业,1999,19(1):20-24.LüMing.Reservior characteristics of gas-bearing area in YingQiong basin[J].Natural Gas Industry,1999,19(1):20-24.
[18]谢玉洪,范彩伟.莺歌海盆地黄流组储层成因新认识[J].中国海上油气,2010,22(6):355-399.Xie Yuhong,Fan Caiwei.Some new knowledge about the origin of Huangliu Formation reservoirs in Dongfang area,Yinggehai basin[J].China Offshore Oil and Gas,2010,22(6):355-399.
[19]王振峰,胡代圣.莺歌海盆地中央泥拱构造带大气田勘探方向[J].天然气工业,1999,19(1):28-30.Wang Zhenfeng,Hu Daisheng.Prospecting for giant gas fields in the central mud diapis structure belt in Yinggehai basin[J].Natural Gas Industry,1999,19(1):28-30.
[20]赵艳,吴胜和,徐樟有,等.川西新场气田上三叠统须家河组二段致密砂岩优质储层控制因素[J].中国石油大学学报:自然科学版,2010,34,(4):1-4.Zhao Yan,Wu Shenghe,Xu Zhangyou,et al.Control factors of compacted high-quality sandstone reservoirs of member 2 of Xujiahe formation,Upper Triassic in Xinchang gasfield of western Sichuan depression[J].Journal of China University of Petroleum,2010,34,(4):1-4.
[21]黄思静,黄培培,王庆东,等.胶结作用在深埋藏砂岩孔隙保存中的意义[J].岩性油气藏,2007,19(3):7-12.Huang Sijing,Huang Peipei,Wang Qingdong,et,al.The significance of cementation in porosity preservation in deep buried sandstones[J].Lothologic Reserviors,2007,19(3):7-12.
[22]刘晓峰,解习农.储层超压流体系统的成因机制述评[J].地质科技情报,2003,22(3):56-59.Liu Xiaofeng,Xie Xinong.Review of formation mechanism of the reservoirs overpressure fuild system[J].Geological Science and Technology Information,2003,22(3):56-59.
[23]Bloch S,Helmod K P.Approaches to predicting reservoir quality of sandstones[J].AAPG Bulletin,1995,79(1):97-144.
[24]Perry E A.Hower J.Late-stage dehydration in deeply buried pelitic sediments[J].AAPG Bulletin,1972,56(10):2 013-2 021.
[25]Colten-Bradley V A.Role of pressure in smectite dehydration;effects on geopressure and smectite-to-illite transformation[J].AAPG Bulletin,1987,71(11):1 414-1 472.
[26]孟元林,魏巍,王维安,等.超压背景下黏土矿物转化的优化模型[J].吉林大学学报:地球科学版,2012,42(增刊1):145-152.Meng Yuanlin,Wei Wei,Wang Weian,et al.An optimization model of clay mineral transformation under overpressure setting[J].Journal of Jilin University:Earth Science Edition,2012,42(suppl1):145-152.
[27]孟元林,刘德来,贺如,等.歧北凹陷沙二段超压背景下的成岩场分析与储层孔隙度预测[J].沉积学报,2005,23(3):389-396.Meng Yuanlin,Liu Delai,He Ru,et al.Diagenetic field analysis and porosity prediction of the Shaer member(Es2)in overpressure setting in the Qibei depression[J].Acta Sedimentologica Sinica2005,23(3):389-396.
[28]Nordgard Bolas H M,Hermanrud C,Teige G M G.Origin of overpressures in shales:constraints from basin modeling[J].AAPG Bulletin,2004,88(2):193-211.
[29]史基安,王琪.影响碎屑岩天然气储层物性的主要控制因素[J].沉积学报,1995,13(2):128-139.Shi Ji’an,Wang Qi.A disscussion on main controlling factors on the properties of clastic gas reservoirs[J].Acta Sedimentologica Sinica,1995,13(2):128-139.
[30]刘得光.准噶尔盆地马桥凸起异常高压成因及油气成藏模式[J].石油勘探与开发,1998,25(1):21-25.Liu Deguang.Over pressure origin and hydrocarbon pool forming mode of Maqiao uplift in Junggar basin[J].Petroleum Exploration and Development,1998,25(1):21-25.
[31]赵永刚,王萌,蒋裕强,等.公山庙地区沙一段低渗砂岩储层成岩作用及其对储层的影响[J].西安石油大学学报:自然科学版,2010,25(6):17-20.Zhao Yonggang,Wang Meng,Jiang Yuqiang,et al.Diagenesis of the low-permeability sandstone reservoir of the first member of Shahejie formation in Gongshanmiao area and its influence on the reservoir property[J].Journal of Xi’an Shiyou University:Natural Science Edition,2010,25(6):17-20.
[32]孟元林,李亚光,牛嘉玉,等.渤海湾盆地北部深层碎屑岩储层孔隙度影响因素探讨[J].中国海上油气,2007,19(3):154-158.Meng Yuanlin,Li Yaguang,Niu Jiayu,et al.A discussion on factors to control porosity of deep-buried clastic reservoirs in the northern Bohai Bay basin[J].China Offshore Oil and Gas,2007,19(3):154-158.
[33]张惠良,张荣虎,王月华,等.粘土膜对砂岩储集性能的影响——以塔里木盆地群6井区泥盆系东河塘组下段为例[J].石油实验地质,2006,28(5):493-496.Zhang Huiliang,Zhang Ronghu,Wang Yuehua,et al.Influence of clay minerals membrane on sandstone reservoirs—A case study on the lower Donghetang reservoirs of the Devonian of Well Qun6 in Tarim basin[J].Petroleum Geology&Experiment,2006,28(5):493-496.
[34]朱平,黄思静,李德敏,等.粘土矿物绿泥石对碎屑储集岩孔隙的保护[J].成都理工大学学报:自然科学版,2004,31(2):153-158.Zhu Ping,Huang Sijing,Li Demin,et al.Effect and protection of chlorite on clastic reservoir rocks[J].Journal of Chengdu University of Technology:Natural Science Edition,2004,31(2):153-158.
[35]伏美燕,张哨楠,丁晓琪,等.松辽盆地松科1井明水组砂岩粘土膜特征及油气地质意义[J].石油实验地质,2012,34(6):587-590.Fu Meiyan,Zhang Shaonan,Ding Xiaoqi,et al.Characteristics and petroleum geologic significances of clay rims in sandstones of Mingshui formation,Well Songke 1,Songliao basin[J].Petroleum Geology&Experiment,2012,34(6):587-590.
[36]丁晓琪,张哨楠.镇泾地区延长组碎屑岩古风化壳研究[J].西南石油大学学报:自然科学版,2010,32(4):16-20.Ding Xiaoqi,Zhang Shaonan.Study on the weathered crust of conglomerate in Upper Triassic Yanchang formation of Zhenjing field[J].Journal of Southwest Petroleum University:Natural Science Edition,2010,32(4):16-20.
[37]王新民,郭彦如,付金华,等.鄂尔多斯盆地延长组长8段相对高孔渗砂岩储集层的控制因素分析[J].石油勘探与开发,2005,32(2):35-40.Wang Xinmin,Guo Yanru,Fu Jinhua,et al.Controlling factors for forming higher porosity and permeability sandstone reservoirs in Chang 8 member of Yanchang formation,Ordos basin[J].Petroleum Exploration and Development,2005,32(2):35-40.
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