QIU Long-wei，XU Ning-ning，LIU Kui-yuan，YANG Sheng-chao，XIE Chao，SHAN Bao-jie，WU Yu-xi . Anomalous High  Porosity Zone and Formation Mechanism of  High Quality Reservoir of Es^s₄ in Bonan Sag[J]. Natural Gas Geoscience, 2015 , 26(1) : 1 -12 . DOI: 10.11764/j.issn.1672-1926.2015.01.0001

［1］Bloch S,Lander R H,Bonnell L.Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and predictability[J].AAPG Bulletin,2002,86(2):301-328.
［2］Tong Chuanxin,Meng Yuanlin,Xie Yuhong,et al.Distribution and causes analysis of the anomalously high porosity zone of the Yinggerhai Basin[J].Bulletin of Mineralogy,Petrology and Geochemistry,2013,32(6):720-727.［童传新,孟元林,谢玉洪,等.莺歌海盆地异常高孔带分布与成因分析[J].矿物岩石地球化学通报,2013,32(6):720-727.］
［3］Zhang Yunfeng,Wang Guoqiang,Fu Baoli,et al.The diagenesis and the origin of abnormal high porosity zone in the deep clastic reservoir in Changling fault depression[J].Journal of Jilin University:Earth Science Edition,2011,41(2):372-376.［张云峰,王国强,付宝利,等.长岭断陷深层碎屑岩储层成岩作用及异常高孔带成因[J].吉林大学学报:地球科学版,2011,41(2):372-376.］
［4］Meng Yuanlin,Liu Wenhui,Meng Fanjin,et al.Distribution and origin of anomalously high porosity zones of the Xujiaweizi fault depression in Songliao Basin[J].Journal of Palaeogeography,2011,13(1):75-84.［孟元林,刘文慧,孟凡晋,等.松辽盆地徐家围子断陷深层异常高孔带分布特征与成因分析[J].古地理学报,2011,13(1):75-84.］
［5］Zhang Yunfeng,Feng Yaqin,Wang Chunxiang.An analysis of abnormal high porosity zone distribution and origin in reservoir rocks in Shiwu fault depression[J].Journal of Daqing Petroleum Institute,2008,32(6):5-8.［张云峰,冯亚琴,王春香.十屋断陷异常高孔带分布特征及成因[J].大庆石油学院学报,2008,32(6):5-8.］
［6］Gu Tuan.Characteristics of abnormally high porosity zone and favorable reservoir facies prediction in deep Cenozoic horizon of Qingshui Sag[J].Natural Gas Geoscience,2008,19(3):327-333.［谷团.辽河盆地西部凹陷清水洼陷新生界深层异常高孔带特征与有利储集相预测研究[J].天然气地球科学,2008,19(3):327-333.］
［7］Cai Zhengqi,Cai Kuang,Xu Zhiming,et al.Carboniferous reservoir characteristics in Sanchaping buried structure in the east of Sichuan and pridiction for favourable exploration area[J].Natural Gas Geoscience,2005,16(6):715-718.［蔡正旗,蔡矿,徐志明,等.川东三岔坪潜伏构造石炭系储层特征及有利区预测[J].天然气地球科学,2005,16(6):715-718.］
［8］Chen Yongqiao,Yu Xinghe,Zhou Xingui,et al.Research on diagenetic evolution succession and occurrence of secondary porosity of Lower Tertiary in different structral belt of Dongying Depression[J].Natural Gas Geoscience,2004,15(1):68-74.［陈永峤,于兴河,周新桂,等.东营凹陷各构造区带下第三系成岩演化与次生孔隙发育规律研究[J].天然气地球科学,2004,15(1):68-74.］
［9］Wang Qi,Bai bin,Li Xiaoyan,et al.Diagenetic evolution characteristics of deeply-buried clasticreserviors,northern Qaidam Basin:A case study from well Kum 2[J].Natural Gas Geoscience,2008,19(2):157-164.［王琪,白斌,李小燕,等.柴达木盆地北缘深部碎屑岩储层成岩演化特征研究——以昆特依凹陷昆2井为例[J].天然气地球科学,2008,19(2):157-164.］
［10］Xu Ningning,Qiu Longwei,Yang Shengchao,et al.Research on diagenetic evolution of the upper fourth member of Shahejie Formation reservoir in Bonan step-fault zone[J].Journal of China University of Mining & Technology,2015,44(1):104-115.［徐宁宁,邱隆伟,杨生超,等.渤南断阶带沙四上亚段储层成岩演化研究[J].中国矿业大学学报,2015,44(1):104-115.］
［11］Yuan Jing,Zhao Chenglin,Zhang Shanwen.Genetic model of the deep water salt lake of the Paleogene Sha4 member in Dongying Sag[J].Acta Sedimentologica Sinica,2000,18(1):114-118.［袁静,赵澄林,张善文.东营凹陷沙四段盐湖的深水成因模式[J].沉积学报,2000,18(1):114-118.］
［12］He Hong,Cai Zhongdong.Mechanism of secondary pore in Shahejie Formation of Banan Depression[J].Journal of Oil and Gas Technology,2005,27(5):557-559.［何宏,蔡忠东.渤南洼陷沙河街组次生孔隙形成机理分析[J].石油天然气学报,2005,27(5):557-559.］
［13］Wu Fuqiang,Xian Xuefu,Li Houshu,et al.Deep reservoir forming mechanism in the upper part of the fourth member of Shahejie Formation in Bonan subsag of Shengli Oil Field[J].Acta Petrolei Sinica,2003,24(1):44-48.［吴富强,鲜学福,李后蜀,等.胜利油区渤南洼陷沙四上亚段深部储层形成机理[J].石油学报,2003,24(1):44-48.］
［14］Wu Fuqiang,Xian Xuefu,Hu Xue,et al.Discussionon the forming mechanism of secondary pores:Taking Bonan subsag in Jiyang Depression as an example[J].Petroleum Geology and Recovery Efficiency,2003,10(1):3-5.［吴富强,鲜学福,胡雪,等.次生孔隙形成机制探讨:以渤南洼陷为例[J].油气地质与采收率,2003,10(1):3-5.］
［15］Xu Xingyou,Xu Guosheng,Qin Runsen.Study on hydrocarbon migration and accumulation of member 4 of Shahejie Formation in Bonan Sag,Zhanhua Depression,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2008,35(2):113-120.［徐兴友,徐国盛,秦润森.沾化凹陷渤南洼陷沙四段油气成藏研究[J].成都理工大学学报:自然科学版,2008,35(2):113-120.］
［16］Surdam R C,Crossey L J,Hagen E S,et al.Organic-inorganic and sandstone diagenesis[J].AAPG Bulletin,1989,73(1):1-23.
［17］Jiang Min.Study on Organic Geochemistry Features of Deep Source Rocks in Dongying,Zhanhua and Weibei Sags［D］.Chengdu:Chengdu University of Techology,2011.［姜敏.东营、潍北及沾化凹陷深层烃源岩有机地球化学特征研究［D］.成都:成都理工大学,2011.］
［18］Luo Jinglan,Liu Xiaohong,Lin Tong,et al.Impact of diagenesis and hydrocarbon emplacement on sandstone reservoir quality of the Yanchang Formation(Upper Triassic)in the Ordos Basin[J].Acta Geologica Sinica,2006,80(5):664-673.［罗静兰,刘小洪,林潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[J].地质学报,2006,80(5):664-673.］
［19］Yan Jianping,Liu Chiyang,Ma Yanping.Influence of diagenesis and hydrocarbon emplacement on the quality of the Fuyang reservoir in Songliao Basin[J].Acta Sedimentologica Sinica,2009,27(2):212-220.［闫建萍,刘池阳,马艳萍.成岩作用与油气侵位对松辽盆地齐家—古龙凹陷扶杨油层物性的影响[J].沉积学报,2009,27(2):212-220.］
［20］Maast T E,Jahren J,BJφrRlykke K.Diagenetic controls on reservoir quality in Middle to Upper Jurassic sandstones in the South BJφrRlykke Viking Graben,North Sea[J].AAPG Bulletin,2011,95(11):1883-1905.
［21］Gong Xiumei,Jin Zhijun,Zeng Jianhui,et al.Resrvoiring characteristics and main controlling factors for deep hydrocarbon accumulations in Bonan sag in Jiyang Depression[J].Oil & Gas Geology,2005,26(4):473-479.［宫秀梅,金之钧,曾溅辉,等.渤南洼陷深层油气成藏特征及主控因素[J].石油与天然气地质,2005,26(4):473-479.］
［22］Xiao Lihua,Gao Yunting,Tian Weizhi,et al.The retardation of mechanical compaction in clastic rocks by overpressure and the prediction model for porosity[J].Bulletin of Mineralogy,Petrology and Geochemistry,2011,30(4):400-406.［肖丽华,高煜婷,田伟志,等.超压对碎屑岩机械压实作用的抑制与孔隙度预测[J].矿物岩石地球化学通报,2011,30(4):400-406.］
［23］Ramm M,BJφrRlykke K.Porosity/depth trends in reservoir sandstones:Assessing the quantitative effects of varying pore-pressure,temperature history and mineralogy,Norwegian Shelf data[J].Clay Minerals,1994,29(4):475-490.
［24］Hao Fang,Zou Huayao,Ni Jianhua,et al.Evolution of overpressured systems in sedimentary basins and conditions for deep oil/gas accumulation[J].Earth Science:Journal of China University of Geosciences,2002,27(5):610-615.［郝芳,邹华耀,倪建华,等.沉积盆地超压系统演化与深层油气成藏条件[J].地球科学:中国地质大学学报,2002,27(5):610-615.］
［25］Xie Xinong,Liu Xiaofeng,Zhao Shibao,et al.Fluid flow and hydrocarbon migration pathways in abnormally pressured environments[J].Earth Science:Journal of China University of Geosciences,2004,29(5):589-595.［解习农,刘晓峰,赵士宝,等.异常压力环境下流体活动及其油气运移主通道分析[J].地球科学:中国地质大学学报,2004,29(5):589-595.］
［26］Liu Hua,Jiang Youlu,Gu Guocui,et al.Pressure characteristics and formation mechanisms of Paleogene in Bonan Sag,Zhanhua Depression[J].Journal of China University of Petroleum:Edition of Natural Science,2013,37(4):46-51.［刘华,蒋有录,谷国翠,等.沾化凹陷渤南洼陷古近系压力特征及成因机制[J].中国石油大学学报:自然科学版,2013,37(4):46-51.］
［27］Wang Yanzhong,Cao Yingchang,Li Yongxin,et al.Controlling factors on the Paleogene deep effective  reservoirs in the Bonan Sag[J].Natural Gas Geoscience,2012,23(6):996-1003.［王艳忠,操应长,李永新,等.渤南洼陷古近系深层有效储层控制因素研究[J].天然气地球科学,2012,23(6):996-1003.］
［28］Wang Tianfu,Cao Yingchang,Wang Yanzhong.Characteristic and origin of the abnormal pressure in the deep Paleogene formation in Bonan Sub-sag[J].Journal of Xi′an Shiyou University:Natural Science Edition,2009,24(2):21-25.［王天福,操应长,王艳忠.渤南洼陷古近系深层异常压力特征及成因[J].西安石油大学学报:自然科学版,2009,24(2):21-25.］
［29］Qin Runsen.Hydrocarbon Distribution Based on the Characteristics of Current Pressure Field,Es₄ formation in Bonan Sag［D］.Chengdu:Chengdu Universty of Techology,2008.［秦润森.沾化凹陷渤南洼陷沙四段段现今压力场特征及其与油气分布关系［D］.成都:成都理工大学,2008.］
［30］Wu Fuqiang,Li Houshu,Hu Xue,et al.An approach to the composite petroleum systems of Es₄¹ in Bonan Sag,Shengli oil province[J].Petroleum Exploration and Development,2002,29(3):29-31.［吴富强,李后蜀,胡雪,等.渤南洼陷沙四上亚段含油气系统探讨[J].石油勘探与开发,2002,29(3):29-31.］
［31］Wang Duoyun,Zheng Ximin,Li Fengjie,et al. Forming condition of high-quality reservoir and its relative problems in low porosity and permeability enrichment zone[J].Natural Gas Geoscience,2003,14(2):87-91.［王多云,郑希民,李风杰,等.低孔渗油气富集区优质储层形成条件及相关问题[J].天然气地球科学,2003,14(2):87-91.］
［32］Yang Xiaoping,Zhao Wenzhi,Zou Caineng,et al.Origin of low-permeability reservoir and distribution of favorable reservoir[J].Acta Petrolei Sinica,2007,28(4):57-61.［杨晓萍,赵文智,邹才能,等.低渗透储层成因机理及优质储层形成与分布[J].石油学报,2007,28(4):57-61.］
［33］Zhu Guohua.Origin and evolution and prediction of porosity in clastic reservoir rocks[J].Acta Sedimentologica Sinica,1992,10(3):114-123.［朱国华.碎屑岩储集层孔隙的形成、演化和预测[J].沉积学报,1992,10(3):114-123.］
［34］Zhai Yonghong,Guo Jianhua,Liu Shengguo,et al.Study on the origine of quality clastic rocks reservoir in Carboniferous from Tazhong area[J].Journal of Mineralogy and Petrology,1996,16(2):55-61.［翟永红,郭建华,刘生国.塔中石炭系碎屑岩深埋藏优质储层成因探讨[J].矿物岩石,1996,16(2):55-61.］
［35］Gu Jiayu,Ning Congqian,Jia Jinhua.High quality reservoir features and genetie analysisof clastic rocks in the Tarim Basin[J].Geological Review,1998,44(1):83-89.［顾家裕,宁从前,贾进华.塔里木盆地碎屑岩优质储层特征及成因分析[J].地质论评,1998,44(1):83-89.］
［36］Zhong Dakang,Zhu Xiaomin,Wang Hongjun.Characteristic and formation mechanism of deep buried clastic reservoir[J].Science in China:Series D,2008,38(supplement 1):11-18.［钟大康,朱筱敏,王红军.中国深层优质碎屑岩储层特征与形成机理分析[J].中国科学:D辑,2008,38(增刊1):11-18.］
［37］Zhang Yu.The controlling role of syndepositional fault structural slope-break zone to depositional system in Bonan Sub-sag[J].Journal of Northwest University:Natural Science Edition,2010,41(5):860-865.［张宇.渤南洼陷同沉积断裂构造坡折带对沉积的控制作用[J].西北大学学报:自然科学版,2010,41(5):860-865.］
［38］Chen Zhonghong,Zha Ming.Mechanism of overpressured fluid compartment and its controlling on hydrocarbon migration and accumulation in faulted lacustrine basin:A case study from the Dongying Sag,Bohai Bay Basin[J].Chinese Journal of Geology,2008,43(1):50-64.［陈中红,查明.断陷湖盆超压封存箱形成机理与油气成藏机制——以渤海湾盆地东营凹陷为例[J].地质科学,2008,43(1):50-64.］