渤海海域秦皇岛29-2东构造优质混积储层主控因素
|
摘要
中深层优质储层的发育通常制约着油气的富集程度。渤海海域秦皇岛29-2东构造钻遇物性极好的陆源碎屑和碳酸盐鲕粒、生物碎屑混积储层,对其控制因素开展研究对类似地区具有启示意义。通过岩芯观察、薄片、扫描电镜、电子探针、物性、全岩、同位素及流体包裹体等分析,系统阐述了秦皇岛29-2东混积岩的岩石学和储集空间等特征,研究结果显示:研究区沙一二段混合沉积储集层包括含陆源碎屑—碳酸盐混积岩、陆源碎屑质碳酸盐混积岩和碳酸盐质—陆源碎屑岩3类,储层类型为高孔、低—特低渗型;孔隙主要为粒间孔、生物体腔孔和次生溶蚀孔隙。并讨论了混积岩优质储层的形成机制,认为咸化湖盆滨浅湖强湖浪作用下形成的富螺混积滩相、埋藏成岩早期白云石化和成岩中后期溶蚀作用是控制该优质储层形成的重要因素。
The development of the high-quality reservoir in medium-deep sections often decides hydrocarbon enrichment. The depth of medium-deep sections in the Bohai sea is approximately greater than 3 000 m with poor reservoir physical properties. We found a mixed reservoir,including terrigenous detrital and Carbonate oolitics and bioclasts,with excellent physical properties in the 1~(st) and 2~(nd) member of the Shahejie Formation( E_3s_(1+2)) in the QHD29-2E structure,and the research of the controlling factors,which have significant implications for similar areas. The features of lithology and reservoir space were revealed by observations of core,rock thin section,scanning electronic microscope( SEM),examining the physical properties,and X ray diffraction( XRD). The isotope fluid inclusion method and reservoir forming mechanism were further addressed. We determined that the rocks in E_3s_(1+2) are composed mainly of terrigenous detrital bearing-carbonate mixed rocks,terrigenous detrital-carbonate mixed rock,and carbonate bearing-terrigenous detrital mixed rock with high porosity and low-very low permeability; for the reservoir space,primary porosity,including intergranular and body cavity pores,as well as secondary pores like moldic pores,were generally found. According to research,snail-rich mixed shoal formed due to strong lake wave action in a saline lacustrine basin. Additionally,dolomitization in the earlier stage and the latter secondary erosion are dominant factors affecting the formation of the excellent reservoirs in the QHD29-2E structure.
The development of the high-quality reservoir in medium-deep sections often decides hydrocarbon enrichment. The depth of medium-deep sections in the Bohai sea is approximately greater than 3 000 m with poor reservoir physical properties. We found a mixed reservoir,including terrigenous detrital and Carbonate oolitics and bioclasts,with excellent physical properties in the 1~(st) and 2~(nd) member of the Shahejie Formation( E_3s_(1+2)) in the QHD29-2E structure,and the research of the controlling factors,which have significant implications for similar areas. The features of lithology and reservoir space were revealed by observations of core,rock thin section,scanning electronic microscope( SEM),examining the physical properties,and X ray diffraction( XRD). The isotope fluid inclusion method and reservoir forming mechanism were further addressed. We determined that the rocks in E_3s_(1+2) are composed mainly of terrigenous detrital bearing-carbonate mixed rocks,terrigenous detrital-carbonate mixed rock,and carbonate bearing-terrigenous detrital mixed rock with high porosity and low-very low permeability; for the reservoir space,primary porosity,including intergranular and body cavity pores,as well as secondary pores like moldic pores,were generally found. According to research,snail-rich mixed shoal formed due to strong lake wave action in a saline lacustrine basin. Additionally,dolomitization in the earlier stage and the latter secondary erosion are dominant factors affecting the formation of the excellent reservoirs in the QHD29-2E structure.
引文
[1]朱光有,张水昌.中国深层油气成藏条件与勘探潜力[J].石油学报,2009,30(6):793-802.[Zhu Guangyou,Zhang Shuichang.Hydrocarbon accumulation conditions and exploration potential of deep reservoirs in China[J]. Acta Petrolei Sinica,2009,30(6):793-802.]
[2]刘志刚,周心怀,李建平,等.渤海海域石臼坨凸起东段36-3构造古近系沙二段储集层特征及控制因素[J].石油与天然气地质,2011,32(54):832-838.[Liu Zhigang,Zhou Xinhuai,Li Jianping,et al. Reservoir characteristics and controlling factors of the Paleogene Sha-2 member in 36-3 structure,eastern Shijiutuo uplift,Bohai Sea[J]. Oil&Gas Geology,2011,32(54):832-838.]
[3] Mount J F. Mixing of siliciclastic and carbonate sediments in shallow shelf environments[J]. Geology,1984,12(7):432-435.
[4] Gierlowski-Kordesch E H. Carbonate deposition in an ephemeral siliciclastic alluvial system:Jurassic Shuttle Meadow Formation,Newark Supergroup,Hartford Basin,USA[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,1998,140(1/2/3/4):161-184.
[5]马艳萍,刘立.大港滩海区第三系湖相混积岩的成因与成岩作用特征[J].沉积学报,2003,21(4):607-613.[Ma Yanping,Liu Li. Sedimentary and diagenetic characteristics of Paleogene lacustrine“Hunji”rock in Beach district,Dagang[J]. Acta Sedimentologica Sinica,2003,21(4):607-613.]
[6]董桂玉,何幼斌,陈洪德,等.惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积:以山东商河地区为例[J].沉积学报,2007,25(3):343-350.[Dong Guiyu,He Youbin,Chen Hongde,et al.Mixed sedimentation of carbonates of lagoonal facies and terrigenous clastics of the middle submember of member 1 of Shahejie Formation in Huimin sag:Taking Shanghe area in Shandong province for an example[J]. Acta Sedimentologica Sinica,2007,25(3):343-350.]
[7]冯进来,曹剑,胡凯,等.柴达木盆地中深层混积岩储层形成机制[J].岩石学报,2011,27(8):2461-2472.[Feng Jinlai,Cao Jian,Hu Kai,et al. Forming mechanism of middle-deep mixed rock reservoir in the Qaidam Basin[J]. Acta Petrologica Sinica,2011,27(8):2461-2472.]
[8]禚喜准,王琪,张瑞,等.柴达木盆地北缘下干柴沟组下段湖相混合沉积发育特征及其对储层的影响[J].沉积学报,2013,31(4):724-729.[Zhuo Xizhun,Wang Qi,Zhang Rui,et al. The characteristics of lacustrine mixed deposit in Lower Xiaganchaigou Formation and its effect on reservoir property:A case in the central areas of northern Qaidam Basin[J]. Acta Sedimentologica Sinica,2013,31(4):724-729.]
[9]徐伟,陈开远,曹正林,等.咸化湖盆混积岩成因机理研究[J].岩石学报,2014,30(6):1804-1816.[Xu Wei,Chen Kaiyuan,Cao Zhenglin,et al. Original mechanism of mixed sediments in the saline lacustrine basin[J]. Acta Petrologica Sinica,2014,30(6):1804-1816.]
[10]于海波,王德英,王军,等.渤海海域石臼坨凸起东段地层岩性油气藏类型及成藏主控因素[J].石油地质与工程,2015,29(4):34-37,62.[Yu Haibo,Wang Deying,Wang Jun,et al. Stratigraphic-lithologic reservoir type and hydrocarbon accumulation main controlling factors of Shijiutuo swell in Bohai Sea[J]. Petroleum Geology and Engineering,2015,29(4):34-37,62.]
[11]王德英,于海波,王军,等.秦南凹陷地层岩性油气藏勘探关键技术及其应用成效[J].中国海上油气,2015,27(3):16-24.[Wang Deying,Yu Haibo,Wang Jun,et al. Key exploration techniques for stratigraphic-lithologic reservoirs and their application in Qinnan sag,Bohai Sea[J]. China Offshore Oil and Gas,2015,27(3):16-24.]
[12]张宇焜,胡晓庆,牛涛,等.古地貌对渤海石臼坨凸起古近系沉积体系的控制作用[J].吉林大学学报(地球科学版),2015,45(6):1589-1596.[Zhang Yukun,Hu Xiaoqing,Niu Tao,et al.Controlling of paleogeomorphology to paleogene sedimentary system of Shijiutuo uplift in Bohai Basin[J]. Journal of Jilin University(Earth Science Edition),2015,45(6):1589-1596.]
[13]张宇焜,王晖,胡晓庆,等.少井条件下的复杂岩性储层地质建模技术:以渤海湾盆地石臼坨凸起A油田为例[J].石油与天然气地质,2016,37(3):450-456.[Zhang Yukun,Wang Hui,Hu Xiaoqing,et al. Reservoir modeling of complex lithologies with sparse wells:A case from A oilfield in Shijiutuo uplift,Bohai Bay Basin[J]. Oil&Gas Geology,2016,37(3):450-456.]
[14]高梦天,杜学斌,叶茂松,等.渤海湾盆地石臼坨凸起东缘混积岩储层特征及物性主控因素[J].油气地质与采收率,2017,24(3):50-56.[Gao Mengtian,Du Xuebin,Ye Maosong,et al.Characteristics of the mixosedimentite reservoir and its controlling factors for petrophysical properties in the eastern margin of Shijiutuo uplift,Bohai Bay Basin[J]. Petroleum Geology and Recovery Efficiency,2017,24(3):50-56.]
[15]吕正祥,宋修章,张健,等.渤海海域中部古近系深埋藏湖相高孔隙度白云岩储层特征及其成因[J].天然气工业,2016,36(12):10-17.[LüZhengxiang,Song Xiuzhang,Zhang Jian,et al.Characteristics and genesis of Paleogene deeply-buried high-porosity lacustrine dolomite reservoirs in the central Bohai Sea area[J].Natural Gas Industry,2016,36(12):10-17.]
[16]杨朝青,沙庆安.云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳酸盐的混合沉积[J].沉积学报,1990,8(2):59-66.[Yang Chaoqing,Sha Qing’an. Sedimentary environment of the Middle Devonian Qujing Formation,Qujing,Yunnan province:A kind of mixing sedimentation of terrigenous clastics and carbonate[J]. Acta Sedimentologica Sinica,1990,8(2):59-66.]
[17]张雄华.混积岩的分类和成因[J].地质科技情报,2000,19(4):31-34.[Zhang Xionghua. Classification and origin of mixosedimentite[J]. Geological Science and Technology Information,2000,19(4):31-34.]
[18]王杰琼,刘波,罗平,等.塔里木盆地西北缘震旦系混积岩类型及成因[J].成都理工大学学报(自然科学版),2014,41(3):339-346.[Wang Jieqiong,Liu Bo,Luo Ping,et al. Classification and genesis of Sinian mixosedimentite from northwest margin of Tarim Basin,China[J]. Journal of Chengdu University of Technology(Science&Technology Edition),2014,41(3):339-346.]
[19]强子同.碳酸盐岩储层地质学[M].东营:石油大学出版社,1998:1-470.[Qiang Zitong. Carbonate reservoir geology[M].Dongying:Petroleum University Press,1998:1-470.]
[20]丁一,李智武,冯逢,等.川中龙岗地区下侏罗统自流井组大安寨段湖相混合沉积及其致密油勘探意义[J].地质论评,2013,59(2):389-400.[Ding Yi,Li Zhiwu,Feng Feng,et al. Mixing of lacustrine siliciclastic—carbonate sediments and its significance for tight oil exploration in the Daanzhai Member,Ziliujing Formation,Lower Jurassic,in Longgang area,central Sichuan Basin[J]. Geological Review,2013,59(2):389-400.]
[21] Murray R C. Origin of porosity in carbonate rocks[J]. Journal of Sedimentary Petrology,1960,30(1):59-84.
[22]刘传联.东营凹陷沙河街组湖相碳酸盐岩碳氧同位素组分及其古湖泊学意义[J].沉积学报,1998,16(3):109-114.[Liu Chuanlian. Carbon and oxygen isotopic compositions of lacustrine carbonates of the Shahejie Formation in the Dongying depression and their paleolimnological significance[J]. Acta Sedimentologica Sinica,1998,16(3):109-114.]
[23]文华国,郑荣才,唐飞,等.鄂尔多斯盆地耿湾地区长6段古盐度恢复与古环境分析[J].矿物岩石,2008,28(1):114-120.[Wen Huaguo,Zheng Rongcai,Tang Fei,et al. Reconstruction and analysis of paleosalanity and paleoenvironment of the Chang 6member in the Gengwan region,Ordos Basin[J]. Journal of Mineralogy and Petrology,2008,28(1):114-120.]
[24]明承栋,侯读杰,赵省民,等.内蒙古东部索伦地区中二叠世哲斯组古环境与海平面相对升降的地球化学记录[J].地质学报,2015,89(8):1484-1494.[Ming Chengdong,Hou Dujie,Zhao Xingmin,et al. The geochemistry records of paleoenvironment and sea-level relative movement of Middle Permian Zhesi Formation in eastern Inner Mongolia[J]. Acta Geologica Sinica,2015,89(8):1484-1494.]
[25]王冠民,廖黔渝,高亮.孤北洼陷西部陡坡带沙一段混积螺滩沉积特征[J].石油天然气学报(江汉石油学院学报),2009,31(4):28-30.[Wang Guanmin,Liao Qianyu,Gao Liang. Sedimentary characteristics of mixed snail-shell beach of Es1Formation in the west of Gubei sag[J]. Journal of Oil and Gas Technology(Journal of Jianghan Petroleum Institute),2009,31(4):28-30.]
[26]孟兆鸿,冯斌,王冠民.孤北洼陷陡坡带的混合生屑浅滩沉积[J].石油地质与工程,2009,23(6):9-11.[Meng Zhaohong,Feng Bin,Wang Guanmin. Sedimentation of mixed bioclastic shallows of steep slope zone in Gubei depression[J]. Petroleum Geology and Engineering,2009,23(6):9-11.]
[27]张守鹏,蔡进功,魏魁生.胜利油气区粒屑碳酸盐岩形成机制与储油气性[J].地球科学——中国地质大学学报,2000,25(2):147-151,223.[Zhang Shoupeng,Cai Jingong,Wei Kuisheng. Sedimentary mechanism and reservoir implication of grained carbonate in Shengli oilfield[J]. Earth Science—Journal of China University of Geosciences,2000,25(2):147-151,223.]
[28]郭宏莉,王大锐.塔里木油气区砂岩储集层碳酸盐胶结物的同位素组成与成因分析[J].石油勘探与开发,1999,26(3):31-32.[Guo Hongli,Wang Darui. Stable isotopic composition and origin analysis of the carbonate cements within sandstone reservoirs of Tarim oilgas bearing area[J]. Petroleum Exploration and Development,1999,26(3):31-32.]
[29]王清斌,臧春艳,赖维成,等.渤中坳陷古近系中、深部碎屑岩储层碳酸盐胶结物分布特征及成因机制[J].石油与天然气地质,2009,30(4):438-443.[Wang Qingbin,Zang Chunyan,Lai Weicheng,et al. Distribution characteristics and origin of carbonate cements in the middle and deep clastic reservoirs of the Paleogene in the Bozhong depression[J]. Oil&Gas Geology,2009,30(4):438-443.]
[30]肖军,王华,袁立川,等.深埋藏砂岩储层中异常孔隙的保存机制探讨[J].地质科技情报,2007,26(5):49-56.[Xiao Jun,Wang Hua,Yuan Lichuan,et al. Preservation mechanisms of abnormal porosity in deeply buried sandstone reservoirs[J]. Geological Science and Technology Information,2007,26(5):49-56.]
[31]朱东亚,张殿伟,刘全有,等.多种流体作用下的白云岩储层发育过程和机制[J].天然气地球科学,2015,26(11):2053-2062.[Zhu Dongya,Zhang Dianwei,Liu Quanyou,et al. Dynamic development process and mechanism of dolomite reservoir under multi-fluid alterations[J]. Natural Gas Geoscience,2015,26(11):2053-2062.]
[32]付金华,吴兴宁,孙六一,等.鄂尔多斯盆地马家沟组中组合岩相古地理新认识及油气勘探意义[J].天然气工业,2017,37(3):9-16.[Fu Jinhua,Wu Xingning,Sun Liuyi,et al. New understandings of the lithofacies paleogeography of the middle assemblage of Majiagou Fm in the Ordos Basin and its exploration significance[J]. Natural Gas Industry,2017,37(3):9-16.]
[33] Lander R H,Walderhaug O. Predicting porosity through simulating sandstone compaction and quartz cementation[J]. AAPG Bulletin,1999,83(3):433-449.
[34]张福顺,朱允辉,王芙蓉.准噶尔盆地腹部深埋储层次生孔隙成因机理研究[J].沉积学报,2008,26(3):469-478.[Zhang Fushun,Zhu Yunhui,Wang Furong. Forming mechanism of secondary pores in deep buried reservoirs of Junggar Basin[J]. Acta Sedimentologica Sinica,2008,26(3):469-478.]
[35] Moore C H. Carbonate reservoirs:porosity evolution and diagenesis in a sequence stratigraphic framework[M]. Amsterdam:Elsevier,2001:282-290.
[36]郭彤楼.元坝气田长兴组储层特征与形成主控因素研究[J].岩石学报,2009,27(8):2381-2391.[Guo Tonglou. Reservoir characteristics and its controlling factors of the Changxing Formation reservoir in the Yuanba gas field,Sichuan Basin,China[J].Acta Petrologica Sinica,2009,27(8):2381-2391.]
[37]徐怀民,林玉祥,郗风云,等.茫崖坳陷下第三系有机酸形成演化及空间分布[J].石油勘探与开发,2000,27(6):23-25.[Xu Huaimin,Lin Yuxiang,Xi Fengyun,et al. The organic acid evolution and distribution of Eogene in Mangya depression[J]. Petroleum Exploration and Development,2000,27(6):23-25.]
[2]刘志刚,周心怀,李建平,等.渤海海域石臼坨凸起东段36-3构造古近系沙二段储集层特征及控制因素[J].石油与天然气地质,2011,32(54):832-838.[Liu Zhigang,Zhou Xinhuai,Li Jianping,et al. Reservoir characteristics and controlling factors of the Paleogene Sha-2 member in 36-3 structure,eastern Shijiutuo uplift,Bohai Sea[J]. Oil&Gas Geology,2011,32(54):832-838.]
[3] Mount J F. Mixing of siliciclastic and carbonate sediments in shallow shelf environments[J]. Geology,1984,12(7):432-435.
[4] Gierlowski-Kordesch E H. Carbonate deposition in an ephemeral siliciclastic alluvial system:Jurassic Shuttle Meadow Formation,Newark Supergroup,Hartford Basin,USA[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,1998,140(1/2/3/4):161-184.
[5]马艳萍,刘立.大港滩海区第三系湖相混积岩的成因与成岩作用特征[J].沉积学报,2003,21(4):607-613.[Ma Yanping,Liu Li. Sedimentary and diagenetic characteristics of Paleogene lacustrine“Hunji”rock in Beach district,Dagang[J]. Acta Sedimentologica Sinica,2003,21(4):607-613.]
[6]董桂玉,何幼斌,陈洪德,等.惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积:以山东商河地区为例[J].沉积学报,2007,25(3):343-350.[Dong Guiyu,He Youbin,Chen Hongde,et al.Mixed sedimentation of carbonates of lagoonal facies and terrigenous clastics of the middle submember of member 1 of Shahejie Formation in Huimin sag:Taking Shanghe area in Shandong province for an example[J]. Acta Sedimentologica Sinica,2007,25(3):343-350.]
[7]冯进来,曹剑,胡凯,等.柴达木盆地中深层混积岩储层形成机制[J].岩石学报,2011,27(8):2461-2472.[Feng Jinlai,Cao Jian,Hu Kai,et al. Forming mechanism of middle-deep mixed rock reservoir in the Qaidam Basin[J]. Acta Petrologica Sinica,2011,27(8):2461-2472.]
[8]禚喜准,王琪,张瑞,等.柴达木盆地北缘下干柴沟组下段湖相混合沉积发育特征及其对储层的影响[J].沉积学报,2013,31(4):724-729.[Zhuo Xizhun,Wang Qi,Zhang Rui,et al. The characteristics of lacustrine mixed deposit in Lower Xiaganchaigou Formation and its effect on reservoir property:A case in the central areas of northern Qaidam Basin[J]. Acta Sedimentologica Sinica,2013,31(4):724-729.]
[9]徐伟,陈开远,曹正林,等.咸化湖盆混积岩成因机理研究[J].岩石学报,2014,30(6):1804-1816.[Xu Wei,Chen Kaiyuan,Cao Zhenglin,et al. Original mechanism of mixed sediments in the saline lacustrine basin[J]. Acta Petrologica Sinica,2014,30(6):1804-1816.]
[10]于海波,王德英,王军,等.渤海海域石臼坨凸起东段地层岩性油气藏类型及成藏主控因素[J].石油地质与工程,2015,29(4):34-37,62.[Yu Haibo,Wang Deying,Wang Jun,et al. Stratigraphic-lithologic reservoir type and hydrocarbon accumulation main controlling factors of Shijiutuo swell in Bohai Sea[J]. Petroleum Geology and Engineering,2015,29(4):34-37,62.]
[11]王德英,于海波,王军,等.秦南凹陷地层岩性油气藏勘探关键技术及其应用成效[J].中国海上油气,2015,27(3):16-24.[Wang Deying,Yu Haibo,Wang Jun,et al. Key exploration techniques for stratigraphic-lithologic reservoirs and their application in Qinnan sag,Bohai Sea[J]. China Offshore Oil and Gas,2015,27(3):16-24.]
[12]张宇焜,胡晓庆,牛涛,等.古地貌对渤海石臼坨凸起古近系沉积体系的控制作用[J].吉林大学学报(地球科学版),2015,45(6):1589-1596.[Zhang Yukun,Hu Xiaoqing,Niu Tao,et al.Controlling of paleogeomorphology to paleogene sedimentary system of Shijiutuo uplift in Bohai Basin[J]. Journal of Jilin University(Earth Science Edition),2015,45(6):1589-1596.]
[13]张宇焜,王晖,胡晓庆,等.少井条件下的复杂岩性储层地质建模技术:以渤海湾盆地石臼坨凸起A油田为例[J].石油与天然气地质,2016,37(3):450-456.[Zhang Yukun,Wang Hui,Hu Xiaoqing,et al. Reservoir modeling of complex lithologies with sparse wells:A case from A oilfield in Shijiutuo uplift,Bohai Bay Basin[J]. Oil&Gas Geology,2016,37(3):450-456.]
[14]高梦天,杜学斌,叶茂松,等.渤海湾盆地石臼坨凸起东缘混积岩储层特征及物性主控因素[J].油气地质与采收率,2017,24(3):50-56.[Gao Mengtian,Du Xuebin,Ye Maosong,et al.Characteristics of the mixosedimentite reservoir and its controlling factors for petrophysical properties in the eastern margin of Shijiutuo uplift,Bohai Bay Basin[J]. Petroleum Geology and Recovery Efficiency,2017,24(3):50-56.]
[15]吕正祥,宋修章,张健,等.渤海海域中部古近系深埋藏湖相高孔隙度白云岩储层特征及其成因[J].天然气工业,2016,36(12):10-17.[LüZhengxiang,Song Xiuzhang,Zhang Jian,et al.Characteristics and genesis of Paleogene deeply-buried high-porosity lacustrine dolomite reservoirs in the central Bohai Sea area[J].Natural Gas Industry,2016,36(12):10-17.]
[16]杨朝青,沙庆安.云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳酸盐的混合沉积[J].沉积学报,1990,8(2):59-66.[Yang Chaoqing,Sha Qing’an. Sedimentary environment of the Middle Devonian Qujing Formation,Qujing,Yunnan province:A kind of mixing sedimentation of terrigenous clastics and carbonate[J]. Acta Sedimentologica Sinica,1990,8(2):59-66.]
[17]张雄华.混积岩的分类和成因[J].地质科技情报,2000,19(4):31-34.[Zhang Xionghua. Classification and origin of mixosedimentite[J]. Geological Science and Technology Information,2000,19(4):31-34.]
[18]王杰琼,刘波,罗平,等.塔里木盆地西北缘震旦系混积岩类型及成因[J].成都理工大学学报(自然科学版),2014,41(3):339-346.[Wang Jieqiong,Liu Bo,Luo Ping,et al. Classification and genesis of Sinian mixosedimentite from northwest margin of Tarim Basin,China[J]. Journal of Chengdu University of Technology(Science&Technology Edition),2014,41(3):339-346.]
[19]强子同.碳酸盐岩储层地质学[M].东营:石油大学出版社,1998:1-470.[Qiang Zitong. Carbonate reservoir geology[M].Dongying:Petroleum University Press,1998:1-470.]
[20]丁一,李智武,冯逢,等.川中龙岗地区下侏罗统自流井组大安寨段湖相混合沉积及其致密油勘探意义[J].地质论评,2013,59(2):389-400.[Ding Yi,Li Zhiwu,Feng Feng,et al. Mixing of lacustrine siliciclastic—carbonate sediments and its significance for tight oil exploration in the Daanzhai Member,Ziliujing Formation,Lower Jurassic,in Longgang area,central Sichuan Basin[J]. Geological Review,2013,59(2):389-400.]
[21] Murray R C. Origin of porosity in carbonate rocks[J]. Journal of Sedimentary Petrology,1960,30(1):59-84.
[22]刘传联.东营凹陷沙河街组湖相碳酸盐岩碳氧同位素组分及其古湖泊学意义[J].沉积学报,1998,16(3):109-114.[Liu Chuanlian. Carbon and oxygen isotopic compositions of lacustrine carbonates of the Shahejie Formation in the Dongying depression and their paleolimnological significance[J]. Acta Sedimentologica Sinica,1998,16(3):109-114.]
[23]文华国,郑荣才,唐飞,等.鄂尔多斯盆地耿湾地区长6段古盐度恢复与古环境分析[J].矿物岩石,2008,28(1):114-120.[Wen Huaguo,Zheng Rongcai,Tang Fei,et al. Reconstruction and analysis of paleosalanity and paleoenvironment of the Chang 6member in the Gengwan region,Ordos Basin[J]. Journal of Mineralogy and Petrology,2008,28(1):114-120.]
[24]明承栋,侯读杰,赵省民,等.内蒙古东部索伦地区中二叠世哲斯组古环境与海平面相对升降的地球化学记录[J].地质学报,2015,89(8):1484-1494.[Ming Chengdong,Hou Dujie,Zhao Xingmin,et al. The geochemistry records of paleoenvironment and sea-level relative movement of Middle Permian Zhesi Formation in eastern Inner Mongolia[J]. Acta Geologica Sinica,2015,89(8):1484-1494.]
[25]王冠民,廖黔渝,高亮.孤北洼陷西部陡坡带沙一段混积螺滩沉积特征[J].石油天然气学报(江汉石油学院学报),2009,31(4):28-30.[Wang Guanmin,Liao Qianyu,Gao Liang. Sedimentary characteristics of mixed snail-shell beach of Es1Formation in the west of Gubei sag[J]. Journal of Oil and Gas Technology(Journal of Jianghan Petroleum Institute),2009,31(4):28-30.]
[26]孟兆鸿,冯斌,王冠民.孤北洼陷陡坡带的混合生屑浅滩沉积[J].石油地质与工程,2009,23(6):9-11.[Meng Zhaohong,Feng Bin,Wang Guanmin. Sedimentation of mixed bioclastic shallows of steep slope zone in Gubei depression[J]. Petroleum Geology and Engineering,2009,23(6):9-11.]
[27]张守鹏,蔡进功,魏魁生.胜利油气区粒屑碳酸盐岩形成机制与储油气性[J].地球科学——中国地质大学学报,2000,25(2):147-151,223.[Zhang Shoupeng,Cai Jingong,Wei Kuisheng. Sedimentary mechanism and reservoir implication of grained carbonate in Shengli oilfield[J]. Earth Science—Journal of China University of Geosciences,2000,25(2):147-151,223.]
[28]郭宏莉,王大锐.塔里木油气区砂岩储集层碳酸盐胶结物的同位素组成与成因分析[J].石油勘探与开发,1999,26(3):31-32.[Guo Hongli,Wang Darui. Stable isotopic composition and origin analysis of the carbonate cements within sandstone reservoirs of Tarim oilgas bearing area[J]. Petroleum Exploration and Development,1999,26(3):31-32.]
[29]王清斌,臧春艳,赖维成,等.渤中坳陷古近系中、深部碎屑岩储层碳酸盐胶结物分布特征及成因机制[J].石油与天然气地质,2009,30(4):438-443.[Wang Qingbin,Zang Chunyan,Lai Weicheng,et al. Distribution characteristics and origin of carbonate cements in the middle and deep clastic reservoirs of the Paleogene in the Bozhong depression[J]. Oil&Gas Geology,2009,30(4):438-443.]
[30]肖军,王华,袁立川,等.深埋藏砂岩储层中异常孔隙的保存机制探讨[J].地质科技情报,2007,26(5):49-56.[Xiao Jun,Wang Hua,Yuan Lichuan,et al. Preservation mechanisms of abnormal porosity in deeply buried sandstone reservoirs[J]. Geological Science and Technology Information,2007,26(5):49-56.]
[31]朱东亚,张殿伟,刘全有,等.多种流体作用下的白云岩储层发育过程和机制[J].天然气地球科学,2015,26(11):2053-2062.[Zhu Dongya,Zhang Dianwei,Liu Quanyou,et al. Dynamic development process and mechanism of dolomite reservoir under multi-fluid alterations[J]. Natural Gas Geoscience,2015,26(11):2053-2062.]
[32]付金华,吴兴宁,孙六一,等.鄂尔多斯盆地马家沟组中组合岩相古地理新认识及油气勘探意义[J].天然气工业,2017,37(3):9-16.[Fu Jinhua,Wu Xingning,Sun Liuyi,et al. New understandings of the lithofacies paleogeography of the middle assemblage of Majiagou Fm in the Ordos Basin and its exploration significance[J]. Natural Gas Industry,2017,37(3):9-16.]
[33] Lander R H,Walderhaug O. Predicting porosity through simulating sandstone compaction and quartz cementation[J]. AAPG Bulletin,1999,83(3):433-449.
[34]张福顺,朱允辉,王芙蓉.准噶尔盆地腹部深埋储层次生孔隙成因机理研究[J].沉积学报,2008,26(3):469-478.[Zhang Fushun,Zhu Yunhui,Wang Furong. Forming mechanism of secondary pores in deep buried reservoirs of Junggar Basin[J]. Acta Sedimentologica Sinica,2008,26(3):469-478.]
[35] Moore C H. Carbonate reservoirs:porosity evolution and diagenesis in a sequence stratigraphic framework[M]. Amsterdam:Elsevier,2001:282-290.
[36]郭彤楼.元坝气田长兴组储层特征与形成主控因素研究[J].岩石学报,2009,27(8):2381-2391.[Guo Tonglou. Reservoir characteristics and its controlling factors of the Changxing Formation reservoir in the Yuanba gas field,Sichuan Basin,China[J].Acta Petrologica Sinica,2009,27(8):2381-2391.]
[37]徐怀民,林玉祥,郗风云,等.茫崖坳陷下第三系有机酸形成演化及空间分布[J].石油勘探与开发,2000,27(6):23-25.[Xu Huaimin,Lin Yuxiang,Xi Fengyun,et al. The organic acid evolution and distribution of Eogene in Mangya depression[J]. Petroleum Exploration and Development,2000,27(6):23-25.]