吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (3): 652-664.doi: 10.13278/j.cnki.jjuese.20160368

• 地质与资源 • 上一篇    下一篇

东营凹陷博兴洼陷沙四上亚段滩坝优质储层形成机理与分布特征

贾艳聪1, 操应长2, 林畅松3, 王健2   

  1. 1. 中国地质大学(北京)能源学院, 北京 100083;
    2. 中国石油大学(华东)地球科学与技术学院, 山东 青岛 266580;
    3. 中国地质大学(北京)海洋学院, 北京 100083
  • 收稿日期:2017-10-07 出版日期:2018-05-26 发布日期:2018-05-26
  • 作者简介:贾艳聪(1989-),女,博士研究生,主要从事沉积学和储层地质学方面的研究,E-mail:yancongjia1989@hotmail.com
  • 基金资助:
    国家油气重大专项(2016ZX05006-007);中央高校基本科研业务费专项(CUG170630)

Formation Mechanism and Distribution of High-Quality Reservoirs for Beach-Bar Sandstones in Upper Part of Es4 in Boxing Sag, Dongying Depression

Jia Yancong1, Cao Yingchang2, Lin Changsong3, Wang Jian2   

  1. 1. School of Energy Resources, China University of Geosciences, Beijing 100083, China;
    2. School of Geosciences, China University of Petroleum(East China), Qingdao 266580, Shandong, China;
    3. School of Ocean Sciences, China University of Geosciences, Beijing 100083, China
  • Received:2017-10-07 Online:2018-05-26 Published:2018-05-26
  • Supported by:
    Supported by National Oil & Gas Major Project of China (2016ZX05006-007) and Fundamental Research Funds for Central Universities (CUG170630)

摘要: 综合运用岩心观察、铸体薄片鉴定、扫描电镜分析、岩石物性测试以及试油结果等分析方法,对东营凹陷博兴洼陷沙四上亚段滩坝中深部储层基本特征进行了研究。结果表明:滩坝中深部储层主要为低孔低渗储层,储集空间表现为原生孔隙和次生孔隙并存发育;研究区优质储层的形成机理主要有沉积作用、地层超压、油气充注、酸性溶蚀和绿泥石颗粒包壳;坝主体和滩脊距泥岩层较远部位储层分选好,抗压实能力强,由于酸性溶解对储层的改造以及油气充注对胶结作用的抑制,中深层仍发育大量原生孔隙和次生孔隙,储层物性较好,并在异常超压和绿泥石颗粒包壳的保护下保存至今并成为有效优质储层;坝主体和滩脊距泥岩层较近部位储层,由于早期强烈的碳酸盐胶结作用并形成致密胶结壳,导致现今储层物性极差,主要发育无效储层;坝侧缘以及滩席储层原始沉积条件差,杂基含量高,在埋藏过程中以压实作用和泥质碳酸盐胶结作用为主,溶解作用微弱,现今物性差,从浅层到深层基本全为无效储层。博兴洼陷沙四上亚段滩坝优质储层主要分布在厚层坝主体和滩脊砂体的中部位置。

关键词: 优质储层, 形成机理, 滩坝, 东营凹陷, 博兴洼陷

Abstract: Based on the core observation, thin section identification, scanning electronic imaging, and petro-physical property and other technical methods, the basic reservoir characteristics of medium-deep strata of beach-bar sandstones were investigated in the upper part of Es4 (Es4s) in the Boxing sag, Dongying depression. The results indicate that the reservoirs are mainly characterized by low porosity and low permeability, and the reservoir spaces are mainly of primary and secondary pores. The formation mechanism of high-quality reservoirs is mainly consist of sedimentation, stratigraphic overpressure, hydrocarbon injection, acid dissolution,and chlorite grain coating. The reservoirs of both bar body and beach edge sub-facies that are far from mudstones are well sorted with strong anti-compacting capacity. Abundant primary and secondary porosities are developed in the medium-deep strata because of the modifications caused by acid dissolution and hydrocarbon filling. These reservoirs are protected by both stratigraphic overpressure and chlorite grain coating, and therefore become effective high-quality reservoirs. The lithofacies of both bar bodies and beach edge sub-facies adjacent to mudstones are typically characterized by the extensive carbonate cementation, which results in the extremely physical properties and invalid reservoir quality. The lithofacies of both bar edge and beach mat sub-facies were deposited under the poor depositional conditions with high contents of matrix. The reservoirs were dominated by compaction and micritic carbonate cementation with weak acidic dissolution. The present physical properties are extremely poor and characterized by invalid reservoirs from shallow to deep strata. The high-quality reservoirs of beach-bar sandstones are located at the central section of thick bar bodies and beach edges.

Key words: high-quality reservoir, formation mechanism, beach-bar, Dongying depression, Boxing sag

中图分类号: 

  • P618.13
[1] 王元君,冯明石,王峻,等.渤中凹陷石南斜坡区古近系中深层优质储层特征[J].矿物岩石,2012,32(3):77-84. Wang Yuanjun, Feng Mingshi, Wang Jun, et al. Characteristics of High-Quality Reservoir of Medium-Deep Paleogene in Shinan Slope Area, Bozhong Depression[J]. Journal of Mineral Petrology, 2012, 32(3):77-84.
[2] 韩成,潘懋,关平,等.柴达木盆地西北部碱山构造中深层储层特征及成因[J].天然气地球科学,2012,23(5):820-825. Han Cheng, Pan Mao, Guan Ping, et al. Reservoir Features and Its Genesis in the Middle-Deep Strata of the Jianshan Structure in the Northwestern Qaidam Basin[J].Natural Gas Geoscience, 2012, 23(5):820-825.
[3] 郭迎春,庞雄奇,陈冬霞,等.川西坳陷中段须二段致密砂岩储层致密化与相对优质储层发育机制[J].吉林大学学报(地球科学版),2012,42(2):21-32. Guo Yingchun, Pang Xiongqi, Chen Dongxia, et al. Densification of Tight Gas Sandstones and Formation Mechanism of Relatively High-Quality Reservoir in the Second Member of the Xujiahe Formation, Western Sichuan Depression[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(2):21-32.
[4] 罗文军,彭军,曾小英,等.川西丰谷地区须四段钙屑砂岩优质储层形成机理[J].石油实验地质,2012,34(4):412-416. Luo Wenjun, Peng Jun, Zeng Xiaoying, et al. Formation Mechanism of High-Quality Reservoir of Calcarenaceous Sandstone in Fourth Member of Xujiahe Formation, Fenggu Area, Wesern Sichuan Depression[J]. Petroleum Geology & Experiment, 2012, 34(4):412-416.
[5] 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:地球科学,2008,38(增刊Ⅰ):11-18. Zhong Dakang, Zhu Xiaomin, Wang Hongjun. Reservoir Features and Formation Mechanism of High-Quality Clastic Reservoir in Deep Strata in China[J].Science China:Earth Sciences, 2008, 38(Sup.Ⅰ):11-18.
[6] 袁海锋,徐国盛,董臣强,等.准中地区侏罗-白垩系优质储层形成机理[J].天然气工业,2008,28(5):14-17. Yuan Haifeng, Xu Guosheng, Dong Chenqiang, et al. Formation Mechanism of High Quality Jurassic-Cretaceous Reservoirs in the Central Junggar Basin[J].Natural Gas Industry, 2008, 28(5):14-17.
[7] 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. 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.
[8] 马奔奔,操应长,王艳忠,等. 车镇凹陷北带古近系中深层优质储层形成机理[J].中国矿业大学学报,2014,43(3):448-457. Ma Benben, Cao Yingchang, Wang Yanzhong, et al. Formation Mechanism of High-Quality Reservoir in the Middle-Deep Strata in Palaeogene in the North Zone of Chezhen Depression[J]. Journal of China University of Mining & Technology, 2014,43(3):448-457.
[9] 苏奥,杜江民,陈红汉,等.控制异常孔隙带发育的成岩流体类型与活动历史:以琼东南盆地东部宝岛北缘储层为例[J].天然气地球科学,2016,27(10):1837-1847. Su Ao, Du Jiangmin, Chen Honghan, et al. Diagenetic Fluid Type and Activity History of Controlling the Development of Abnormal Pore Zone:Taking the North Margin of Baodao Sag, Qiongdongnan Basin as an Example[J]. Natrual Gas Geosciences, 2016, 27(10):1837-1847.
[10] Taylor T R, Giles M R, Hathon L A, et al. Sandstone Diagenesis and Reservoir Quality Prediction:Models, Myths, and Reality[J]. AAPG Bulletin, 2010, 94:1093-1132.
[11] Nguyen B T, Jones S J, Goulty N R, et al. The Role of Fluid Pressure and Diagenetic Cements for Porosity Preservation in Triassic Fluvial Reservoirs of the Central Graben, North Sea[J].AAPG Bulletin, 2013, 97(8):1273-1302.
[12] Ajdukiewicz J M, Lander R H. Sandstone Reservoir Quality Prediction:The State of the Art[J]. AAPG Bulletin, 2010, 94:1083-1091.
[13] Bloch S, Lander R H, Bonnell L M. Anomalously High Porosity and Permeability in Deeply Buried Sandstone Reservoirs:Origin and Predictability[J]. AAPG Bulletin, 2002, 86:301-328.
[14] 王永诗,刘惠民,高永进,等. 断陷湖盆滩坝砂体成因与成藏:以东营凹陷沙四上亚段为例[J].地学前缘,2012,19(1):100-107. Wang Yongshi, Liu Huimin, Gao Yongjin, et al. Sandbody Genesis and Hydrocarbon Accumulation Mechanism of Beach-Bar Reservoir in Faulted-Lacustrine-Basins:A Case Study from the Upper of the Fourth Member of Shahejie Formation, Dongyong Sag[J].Earth Science Frontiers, 2012,19(1):100-107.
[15] 李秀华,肖焕钦,王宁. 东营凹陷博兴洼陷沙四段上亚段储集层特征及油气富集规律[J]. 油气地质与采收率,2001,8(3):21-25. Li Xiuhua, Xiao Huaqin, Wang Ning. Reservoir Characteristics and Hydrocarbon Enrichment Rules in Upper Es4 of Boxing Subsag in Dongying Sag[J].Petroleum Geology and Recover Efficiency, 2001,8(3):21-25.
[16] 操应长,王健,刘惠民,等. 东营凹陷南坡沙四上亚段滩坝砂体的沉积特征及模式[J].中国石油大学学报(自然科学版),2009,33(6):5-10. Cao Yingchang, Wang Jian, Liu Huimin, et al. Sedimentary Characteristics and Models of Beach-Bar Sandbodies in the Upper Part of the Fourth Member of Paleogene in the Southern Slope of Dongying Depression[J].Journal of China University of Petroleum, 2009,33(6):5-10.
[17] Morad S, Al-Ramadan K, Ketzer J M, et al. The Impact of Diagenesis on the Heterogeneity of Sandstone Reservoirs:A Review of the Role of Depositional Facies and Sequence Stratigraphy[J]. AAPG Bulletin, 2010, 94:1267-1309.
[18] 王健. 东营凹陷南部缓坡带薄砂体沉积特征及储层成岩改造模式[D].青岛:中国石油大学(华东),2013. Wang Jian. Sedimentary Characteristics and Reservoir Diagenetic Reconstruction Model of Thin Sandbodies of Southern Gentle Slope Belt in Dongying Depression[D].Qingdao:China University of Petroleum (Eastern China), 2013.
[19] Xie X, Bethke C M, Li S, et al. Overpressure and Petroleum Generation and Accumulation in the Dongying Depression of the Bohaiwan Basin, China[J]. Geofluids, 2001, 1:257-271.
[20] Guo X W, He S, Liu K Y, et al. Oil Generation as the Dominant Overpressure Mechanism in the Cenozoic Dongying Depression, Bohai Bay Basin, China[J]. AAPG Bulletin, 2010, 94:1859-1881.
[21] Becker S P, Eichhubl P, Laubach S E, et al. A 48 m.y. History of Fracture Opening, Temperature, and Fluid Pressure:Cretaceous Travis Peak Formation, East Texas Basin[J]. Geological Society of America Bulletin, 2010, 122:1081-1093.
[22] 苏永进,蒋有录,房新娜,等. 博兴洼陷古近系沙四上和沙三段油气成藏的差异性研究[J].中国石油大学学报(自然科学版),2006,30(2):11-15. Su Yongjin, Jiang Youlu, Fang Xinna, et al. Otherness on Pool-Forming in the Upper Es4 and Es3 of Palaeogene in Boxing Subsag[J]. Journal of China University of Petroleum, 2006,30(2):11-15.
[23] 荣启宏. 博兴洼陷东南部沙四段储层的流体史研究[J].矿物岩石,2004,24(2):61-66. Rong Qihong. Study on Fluid History of Reservoirs from Shasi Member, Southeast Boxing Depression[J]. Journal of Mineral Petrology, 2004,24(2):61-66.
[24] Saigal G C, Bjørlykke K, Larter S. The Effect of Oil Emplacement on Diagenetic Processes:Examples from the Fulmar Reservoir Sandstones, Central North Sea[J]. AAPG Bulletin, 1992, 76:1024-1033.
[25] Aase N E, Walderhaug O. The Effect of Hydro-carbons on Quartz Cementation:Diagenesis in the Upper Jurassic Sandstones of the Miller Field, North Sea, Revisited[J]. Petroleum Geoscience, 2005, 11:215-223.
[26] 谭丽娟,蒋有录,苏成义,等.东营凹陷博兴地区烃源岩和油源特征[J].石油大学学报(自然科学版),2002,26(5):1-5. Tan Lijuan, Jiang Youlu, Su Chengyi, et al. Characteristics of Hydrocarbon Source Rock and Oil-Source Correlation in Boxing Area of Dongying Depression[J]. Journal of China University of Petroleum, 2002,26(5):1-5.
[27] Surdam R C, Crossly L J, Hagen E S, et al. Organic-Inorganic Interactions and Sandstone Diagenesis[J]. AAPG Bulletin, 1989, 73(1):1-23.
[28] Bjørlykke K. Clay Mineral Diagenesis in Sedimentary Basins:A Key to the Prediction of Rock Properties:Examples from the North Sea Basin[J]. Clay Minerals, 1998, 33:15-34.
[29] Thyne G. A Model for Diagenetic Mass Transfer Between Adjacent Sandstone and Shale[J]. Marine and Petroleum Geology, 2001, 18:743-755.
[30] Ehrenberg S N. Preservation of Anomalously High Porosity in Deeply Buried Sandstones by Grain-Coating Chlorite:Example from the Norwegian Continental Shelf[J]. AAPG Bulletin, 1993, 77(7):1260-1286.
[31] 李克永,李文厚,张东阳,等.鄂尔多斯盆地安塞油田长10优质储层特征[J]地质通报,2013,32(9):1453-1460. Li Keyong, Li Wenhou, Zhang Dongyang, et al. An Analysis of Favorable Reservoir Characteristics of Chang 10 Formation in the Ansai Oilfield, Ordos Basin[J]. Geological Bulletin of China, 2013,32(9):1453-1460.
[1] 宋林珂, 刘四兵, 曾青高, 周栋, 唐大海, 王锦西.

四川盆地川中—川西过渡带中侏罗统沙溪庙组致密砂岩相对优质储层成因机制 [J]. 吉林大学学报(地球科学版), 2024, 54(2): 371-388.

[2] 陈剑平, 李兴华, 王 清, 韩 岩, 刘 经, 韩梦霞. 乾安碳酸型盐渍土的孔隙特征[J]. 吉林大学学报(地球科学版), 2023, 53(2): 491-.
[3] 陈思芮, 王卫学, 曲希玉, 纪友亮, 鲜本忠, 刘英男. 东营凹陷北带沙四上亚段砂砾岩储层物性主控因素分析[J]. 吉林大学学报(地球科学版), 2022, 52(4): 1091-.
[4] 束龙仓, 温中琦, 张岩, 李进, 马倩, 陆小明. 苏北沿海地区潜水水化学特征及形成机理[J]. 吉林大学学报(地球科学版), 2022, 52(4): 1223-.
[5] 徐春强, 张新涛, 王晨杰, 张震, 刘丰. 渤中凹陷中生界火山岩特征及优质储层控制因素[J]. 吉林大学学报(地球科学版), 2022, 52(4): 1027-.
[6] 张田田, 杨为民, 万飞鹏, . 浑河断裂带地质灾害发育特征及其成因机制[J]. 吉林大学学报(地球科学版), 2022, 52(1): 149-.
[7] 张军华, 刘震, 李琴, 任雄风, 赵杰. 东营凹陷红层地球物理特征分析及有利储层预测[J]. 吉林大学学报(地球科学版), 2021, 51(4): 1256-1267.
[8] 王鑫, 林承焰, 马存飞, 陈柄屹, 杜凯, 李志鹏. 东营凹陷北部陡坡带利563区块沙四上亚段砂砾岩扇体沉积特征及沉积模式[J]. 吉林大学学报(地球科学版), 2020, 50(3): 705-720.
[9] 赵汉卿, 陈晓明, 李超, 吴穹螈, 王迪. 渤海湾盆地垦利L油田古近系沙三上段优质储层物性控制因素[J]. 吉林大学学报(地球科学版), 2020, 50(2): 653-661.
[10] 李维禄, 高思宇, 张翼, 张金亮, 韩春花. 末端扇—滨浅湖滩坝组合沉积机制与演化分布:以东濮凹陷卫城油田沙河街组四段为例[J]. 吉林大学学报(地球科学版), 2020, 50(1): 31-40.
[11] 王夏斌, 姜在兴, 胡光义, 范廷恩, 王俊辉, 卢欢. 辽河盆地西部凹陷古近系沙四上亚段沉积相及演化[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1222-1234.
[12] 李欢, 王清斌, 庞小军, 冯冲, 刘晓健. 渤海湾盆地辽东凹陷旅大29构造沙二段近源砂砾岩体优质储层形成机理[J]. 吉林大学学报(地球科学版), 2019, 49(2): 294-309.
[13] 杨怀宇. 王家岗—八面河地区潜山残留地层发育特征及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1625-1634.
[14] 蔡来星, 卢双舫, 肖国林, 王蛟, 吴志强, 郭兴伟, 侯方辉. 论优质源储耦合关系的控藏作用:对比松南致密油与松北致密气成藏条件[J]. 吉林大学学报(地球科学版), 2018, 48(1): 15-28.
[15] 林承焰, 王杨, 杨山, 任丽华, 由春梅, 吴松涛, 吴玉其, 张依旻. 基于CT的数字岩心三维建模[J]. 吉林大学学报(地球科学版), 2018, 48(1): 307-317.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 吴远坤, 刘成林, 于春勇. 松辽盆地双城断陷深层原油成藏模式[J]. 吉林大学学报(地球科学版), 2024, 54(5): 1443 -1456 .
[2] 马荣,石建省,刘继朝. 人工内分泌网络模型在水文地质参数研究中的应用[J]. 吉林大学学报(地球科学版), 2013, 43(3): 914 -921 .
[3] 李宁, 王成文. 东北及邻区晚古生代地层接触关系与佳-蒙地块的形成和演化[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1331 -1340 .
[4] 胡大千,初凤友,姚 杰. 中太平洋YJA海山富钴结壳矿物组成与元素地球化学[J]. J4, 2006, 36(01): 32 -0037 .
[5] 姜 雪, 程日辉,于民凤. 裂谷地层的气候和构造控制:Zscape模型分析与在松辽盆地北安断陷的应用[J]. J4, 2006, 36(01): 54 -0059 .
[6] 李春柏,张新涛,刘 立,任延广,孟 鹏. 布达特群热流体活动及其对火山碎屑岩的改造作用--以海拉尔盆地贝尔凹陷为例[J]. J4, 2006, 36(02): 221 -0226 .
[7] 孟宪纲,薄万举,刘志广,刘勇,畅柳,李朝柱,王子平. 芦山7.0级地震与巴颜喀拉块体中东段的活动性[J]. 吉林大学学报(地球科学版), 2014, 44(5): 1705 -1711 .
[8] 陈欢庆, 梁淑贤, 舒治睿, 邓晓娟, 彭寿昌. 冲积扇砾岩储层构型特征及其对储层开发的控制作用——以准噶尔盆地西北缘某区克下组冲积扇储层为例[J]. 吉林大学学报(地球科学版), 2015, 45(1): 13 -24 .
[9] 贾大成,邢立新, 潘 军, M. J. van Bergen, H. van Roermund. 伊通上地幔剪切带捕虏体中富铝尖晶石的地球化学特征[J]. J4, 2006, 36(04): 497 -502 .
[10] 谢忠雷,杨佰玲,包国章,董德明. 茶园土壤不同形态镍的含量及其影响因素[J]. J4, 2006, 36(04): 599 -604 .