吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 653-661.doi: 10.13278/j.cnki.jjuese.20190264

• 油气勘探开发 • 上一篇    下一篇

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

赵汉卿, 陈晓明, 李超, 吴穹螈, 王迪   

  1. 中海石油(中国)有限公司天津分公司, 天津 300459
  • 收稿日期:2019-12-09 出版日期:2020-03-26 发布日期:2020-03-31
  • 作者简介:赵汉卿(1989-),男,工程师,主要从事油气田开发地质、沉积学等方面的研究,E-mail:zhaohq17@cnooc.com.cn
  • 基金资助:
    国家科技重大专项(2011ZX05023-006-002);中海石油(中国)有限公司科技重大专项(YXKY-2018-TJ-04)

Control Factors of High Quality Reservoir in Upper Part of the 3rd Member of Eocene Shahejie Formation in Kenli L Oilfield, Bohai Bay Basin

Zhao Hanqing, Chen Xiaoming, Li Chao, Wu Qiongyuan, Wang Di   

  1. Tianjin Branch of CNOOC Ltd., Tianjin 300459, China
  • Received:2019-12-09 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Science and Technology Major Project (40972076) and Major Science and Technology Project of CNOOC Ltd. (YXKY-2018-TJ-04)

摘要: 为明确渤海湾盆地莱州湾凹陷垦利L油田古近系沙三上段储层物性特征及影响因素,综合利用铸体薄片、扫描电镜、X衍射、孔渗测试、地层测试等多种分析测试手段,结合区域构造背景、沉积体系等相关研究成果,探讨了沙三上段储层物性控制因素,并在油田注水开发中开展了应用。研究结果表明:沙三上段储层平均孔隙度为28.9%,平均渗透率为762.7×10-3 μm2,属于高孔高渗储层,储集空间以原生粒间孔为主,可见次生粒间孔和铸模孔,微裂缝发育;微裂缝平均宽度为180 μm,微裂缝的存在提供了高效渗流通道,使地层孔渗测试结果明显优于岩心测试数据;优质储层的分布主要受体系域、断裂活动和埋藏作用的影响,水进体系域厚层净砂岩是形成优质储层的物质基础,微裂缝发育提高了渗流能力,快速埋藏减缓了储层孔隙水的排出和储层物性的降低。根据优质储层发育特征及生产动态资料,优化水井分层配注,降低平面及纵向上水驱不均,实现了油田均衡驱替。

关键词: 优质储层, 微裂缝, 控制因素, 沙三上段, 垦利L油田

Abstract: The physical characteristics and genesis of the upper part of the 3rd member of Eocene Shahejie Formation (E2s3u) in Kenli L oilfield of Laizhou Bay sag in Bohai Bay basin were clarified by using a variety of analyses and testing methods, such as casting thin sections, SEM, X diffraction, pore permeability test and drilling test, combined with the related research results of regional tectonic setting and sedimentary system, the physical properties control factors of E2s3u were discussed, and applied in oilfield water injection development. The results show that:the reservoir of E2s3u with the average porosity of 28.9% and the average permeability of 762.7×10-3μm2 belongs to "high porosity-permeability" reservoir,the reservoir space is mainly primary intergranular pores with secondary intergranular pores, mold holes, and micro-fractures; the average width of the micro-fractures is 180 μm, the existence of the micro-fractures provided a highly efficient seepage channels, which makes drilling test pore permeability is obviously better than that through core test. The physical properties of high quality reservoirs are mainly affected by system tract, fault activity and burial, the thick net sandstone under transgressive system tract is the material basis of forming high-quality reservoirs; the developed micro-fractures improved seepage capacity; rapid burial slowed the drainage of reservoir pore water and the decline of reservoir physical properties. Based on high-quality reservoir development characteristics and production dynamic data, optimizing layered allocation of water wells, reducing uneven water flooding in the horizontal and vertical directions, and then Kenli L oilfield achieved balanced displacement.

Key words: high quality reservoir, micro-fracture, control factors, E2s3u, Kenli L oilfield

中图分类号: 

  • TE122.2
[1] 付兆辉, 秦伟军, 李敏. 渤海湾盆地垦东凸起构造演化及对沉积的控制作用[J]. 石油地质与工程, 2011, 25(4):7-10. Fu Zhaohui, Qing Weijun, Li Min. Tectonic Evolution and Its Controlling Effect on Sedimentation of the Kendong Uplift in Bohai Bay Basin[J]. Petroleum Geology and Engineering,2011,25(4):7-10.
[2] 彭文绪,辛仁臣,孙和风,等.渤海海域莱州湾凹陷的形成和演化[J].石油学报,2009,30(5):654-660. Peng Wenxu, Xin Renchen, Sun Hefeng, et al. Formation and Evolution of Laizhouwan Sag in Bohai Bay[J]. Acta Petrolei Sinica,2009,30(5):654-660.
[3] 王亮, 牛成民, 杨波,等. 莱州湾凹陷沙三段含油气系统与有利勘探方向[J].断块油气田, 2011, 18(5):545-548. Wang Liang, Niu Chengmin, Yang Bo, et al. Petroleum System and Favorable Exploration Targets of the Third Member of Shahejie Formation in Laizhouwan Depression[J]. Fault-Block Oil & Gas Field,2011,18(5):545-548.
[4] 吴时国,余朝华,邹东波,等.莱州湾地区郯庐断裂带的构造特征及其新生代演化[J].海洋地质与第四纪地质,2006,26(6):101-110. Wu Shiguo, Yu Zhaohua, Zou Dongbo, et al. Structural Features and Cenozoic Evolution of the Tanlu Fault Zone in the Laizhou Bay, Bohai Sea[J]. Marine Geology & Quaternary Geology,2006,26(6):101-110.
[5] 孙和风,周心怀,彭文绪,等.莱州湾凹陷东部走滑带盐相关构造特征[J]. 地球科学与环境学报,2008,30(4):380-384. Sun Hefeng, Zhou Xinhuai, Peng Wenxu, et al. Characteristics of Salt-Related Structures in the Eastern Strike-Slip Zone of Laizhou Bay Sag[J]. Journal of Earth Sciences and Environment,2008,30(4):380-384.
[6] Ma B B, Kenneth A E, Cao Y C, et al. Fluid Flow and Related Diagenetic Processes in a Rift Basin:Evidence from the Fourth Member of the Eocene Shahejie Formation Interval, Dongying Depression, Bohai Bay Basin, China[J]. AAPG Bulletin, 2016, 100(11):1633-1662.
[7] 辛云路,任建业,李建平.构造-古地貌对沉积的控制作用:以渤海南部莱州湾凹陷沙三段为例[J].石油勘探与开发,2013, 40(3):2-10. Xin Yunlu,Ren Jianye,Li Jianping. Control of Tectonic-Paleogeomorphology on Deposition:A Case from the Shahejie Formation Sha 3 Member, Laizhouwan Sag, Southern Bohai Sea[J]. Petroleum Exploration and Development, 2013, 40(3):2-10.
[8] 赵汉卿,张建民,李栓豹,等. 渤海湾盆地A油田新近系明下段沉积特征及演化模式[J].吉林大学学报(地球科学版), 2017, 47(4):1021-1029. Zhao Hanqing, Zhang Jianmin, Li Shuanbao, et al.Sedimentary Characteristics and Evolution Models of Lower Part of Minghuazhen Formation in Neogene System at an Oil Field, Bohai Bay Basin[J]. Journal of Jilin University (Earth Science Edition),2017,47(4):1021-1029.
[9] 方旭庆, 林会喜, 王智帮. 垦东凸起"陀螺式"演化与油气成藏[J].西安石油大学学报(自然科学版), 2007, 22(4):13-16. Fang Xuqing, Lin Huixi, Wang Zhibang.Gyro-Type Tectonic Evolution and Hydrocarbon Accumulation of Kendong Uplift[J]. Journal of Xi'an Shiyou University (Natural Science Edition), 2007,22(4):13-16.
[10] 赵汉卿, 陈存良, 陈晓明,等.垦利10-4油田沙三上段成岩作用与油气充注耦合关系[J].断块油气田, 2018, 25(4):435-439. Zhao Hanqing, Chen Cunliang, Chen Xiaoming, et al. Coupling Relationship Between Diagenesis and Hydrocarbon Charging in the Upper 3rd Member of Eogene Shahejie Formation of the Kenli 10-4 Oilfield[J]. Fault-Block Oil &Gas Field, 2018, 25(4):435-439.
[11] 吴胜和. 储集层表征与建模[M]. 北京:石油工业出版社, 2010,210-215. Wu Shenghe. Reservoir Characterization & Modeling[M]. Beijing:Petroleum Industry Press, 2010:210-215.
[12] 赵汉卿,张建民,李栓豹,等. 长周期基准面下降半旋回内浅水三角洲沉积演化规律及其在开发中的应用:以渤海A油田明下段为例[J].海洋地质与第四纪地质, 2018, 38(5):71-79. Zhao Hanqing, Zhang Jianmin, Li Shuanbao, et al. Sedimentary Evolution of Shallow-Water Delta in a Long-Term Base-Level Cycle Decreasing Semi-Cycle and the Application in Development:Taking an Oilfield, Baohai as Example[J]. Marine Geology and Quaternary Geology, 2018, 38(5):71-79.
[13] 万桂梅,周东红,汤良杰.渤海海域郯庐断裂带对油气成藏的控制作用[J].石油与天然气地质,2009,30(4):450-454,461. Wang Guimei, Zhou Donghong, Tang Liangjie. Control of the Tan-Lu Fault Zone on Hydrocarbon Accumulation in the Bohai Sea Waters[J]. Oil & Gas Geology,2009,30(4):450-454,461.
[14] Mansurbeg H, Morad S, Salem A, et al. Diagenesis and Reservoir Quality Evolution of Palaeocene Deep-Water, Marine Sandstones, the Shetland-Faroes Basin, British Continental Shelf[J]. Marine and Petroleum Geology, 2008, 25(6):514-543.
[15] 牛成民. 渤海南部海域莱州湾凹陷构造演化与油气成藏[J]. 石油与天然气地质, 2012, 33(3):424-431. Niu Chengmin. Tectonic Evolution and Hydrocarbon Accumulation of Laizhouwan Depression in Southern Bohai Sea[J]. Oil & Gas Geology,2012,33(3):424-431.
[16] 操应长,贾艳聪,王艳忠,等.渤南洼陷北带沙四上亚段储层成岩流体演化[J].现代地质,2014,28(1):197-207. Cao Yingchang, Jia Yancong, Wang Yanzhong, et al. Diagenetic Fluid Evolution of Reservoir in Es4s in the North Zone of the Bonan Sag[J].Geoscience, 2014,28(1):197-207.
[17] 祝海华, 钟大康, 姚泾利, 等. 碱性环境成岩作用及对储集层孔隙的影响:以鄂尔多斯盆地长7段致密砂岩为例[J]. 石油勘探与开发, 2015, 42(1):51-59. Zhu Haihua, Zhong Dakang, Yao Jingli, et al. Alkaline Diagenesis and Its Effects on Reservoir Porosity:A Case Study of Upper Triassic Chang 7 Tight Sandstones in Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2015, 42(1):51-59.
[18] Huabg C G, Zhao F, Yuan J Y, et al. Acid Fluids Reconstruction Clastic Reservoir Experiment in Qaidam Saline Lacustrine Basin, China[J]. Carbonates & Evaporites, 2015, 31(3):319-328.
[19] 隋风贵, 刘庆, 张林晔. 济阳断陷盆地烃源岩成岩演化及其排烃意义[J].石油学报, 2007, 28(6):12-16. Sui Fenggui, Liu Qing, Zhang Linye. Diagenetic Evolution of Source Rocks and Its Significance to Hydrocarbon Expulsion in Shahejie Formation of Jiyang Depression[J]. Acta Petrolei Sinica, 2007, 28(6):12-16.
[20] 高崇龙, 纪友亮, 靳军,等. 准噶尔盆地莫索湾地区清水河组深层优质储层特征及其物性控制因素[J]. 吉林大学学报(地球科学版), 2017, 47(4):990-1006. Gao Chonglong, Ji Youliang, Jin Jun, et al. Characteristics and Controlling Factors on Physical Properties of Deep Buried Favorable Reservoirs of the Qingshuihe Formation in Muosuowan Area, Junggar Basin[J]. Journal of Jilin University (Earth Science Edition), 2017, 47(4):990-1006.
[21] Anjos S M, Deros L F, Desouza R S, et al. Depositional and Diagenetic Controls on the Reservoir Quality of Lower Cretaceous Pendencia Sandstones, Potiguar Rift Basin, Brazil[J]. AAPG Bulletin, 2000, 84(11):1719-1742.
[22] Chilingar G V, Serebryakov V A, Robertson J O. Origin and Prediction of Abnormal Formation Pressure[M]. Amsterdam:Elsevier Scientific Publishing Company,2002:123-150.
[23] 张永贵, 陈明强, 吴莹. 利用动态资料研究巴喀油田裂缝分布[J]. 石油勘探与开发, 1998,25(5):68-71. Zhang Yonggui, Chen Mingqiang, Wu Ying. Integrating Dynamics Data to Characterize Naturally Fractured Reservoir:A Case Study of Baka Oil Field, Turpan-Hami Basin, China[J]. Petroleum Exploration and Development, 1998, 25(5):68-71.
[1] 林孟雄, 刘立, 张一果, 常森, 夏阳. 苏里格气田东二区气水分布及产水控制因素分析[J]. 吉林大学学报(地球科学版), 2020, 50(2): 627-634.
[2] 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.
[3] 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.
[4] 陈爱民. 澳大利亚Bonaparte盆地WA-406-P区块油气成藏条件及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(4): 965-980.
[5] 林敉若, 操应长, 葸克来, 王健, 陈洪, 吴俊军. 阜康凹陷东部斜坡带二叠系储层特征及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(4): 991-1007.
[6] 贾艳聪, 操应长, 林畅松, 王健. 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[J]. 吉林大学学报(地球科学版), 2018, 48(3): 652-664.
[7] 孙海涛, 钟大康, 李勇, 毛亚昆, 杨宪彰. 超深低孔特低渗砂岩储层的孔隙成因及控制因素——以库车坳陷克深地区巴什基奇克组为例[J]. 吉林大学学报(地球科学版), 2018, 48(3): 693-704.
[8] 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.
[9] 高崇龙, 纪友亮, 靳军, 王剑, 任影, 车世琦, 王茹, 桓芝俊. 准噶尔盆地莫索湾地区清水河组深层优质储层特征及其物性控制因素[J]. 吉林大学学报(地球科学版), 2017, 47(4): 990-1006.
[10] 李福来, 王石头, 苗顺德, 杨军侠, 徐志尧, 李文帅. 华庆地区长63段低渗储层特征及优质储层主控因素[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1580-1588.
[11] 操应长, 张会娜, 葸克来, 赵贤正, 周磊, 崔周旗, 金杰华. 饶阳凹陷南部古近系中深层有效储层物性下限及控制因素[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1567-1579.
[12] 徐波, 唐铁柱, 李辰. 鄂尔多斯盆地中东部马五段碳酸盐岩气藏富气主控因素—以陕200井区为例[J]. 吉林大学学报(地球科学版), 2015, 45(5): 1299-1309.
[13] 潘荣, 朱筱敏, 张剑锋, 何敏, 邸宏利. 克拉苏冲断带深层碎屑岩有效储层物性下限及控制因素[J]. 吉林大学学报(地球科学版), 2015, 45(4): 1011-1020.
[14] 刘四兵, 沈忠民, 吕正祥, 宋荣彩, 王鹏. 川西新场气田上三叠统须二、须四段相对优质储层成因差异性分析[J]. 吉林大学学报(地球科学版), 2015, 45(4): 993-1001.
[15] 姚泾利, 赵彦德, 邓秀芹, 郭正权, 罗安湘, 楚美娟. 鄂尔多斯盆地延长组致密油成藏控制因素[J]. 吉林大学学报(地球科学版), 2015, 45(4): 983-992.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!