吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (5): 1342-1352.doi: 10.13278/j.cnki.jjuese.20170155

• 地质与资源 • 上一篇    下一篇

辫状河致密砂岩储层构型单元定量表征方法

瞿雪姣1,2, 李继强1,2, 张吉3, 赵忠军3, 戚志林1,2, 罗超1,2   

  1. 1. 复杂油气田勘探开发重庆市重点实验室, 重庆 401331;
    2. 重庆科技学院石油与天然气工程学院, 重庆 401331;
    3. 中国石油长庆油田公司, 西安 710018
  • 收稿日期:2018-01-07 发布日期:2018-11-20
  • 通讯作者: 李继强(1973-),男,教授级高级工程师,主要从事油气田开发方面的研究,E-mail:lijiqiangcq@163.com E-mail:lijiqiangcq@163.com
  • 作者简介:瞿雪姣(1986-),男,讲师,博士,主要从事石油地质和大陆科学钻探方面的研究,E-mail:quxuejiao2008@aliyun.com
  • 基金资助:
    国家重大科技专项项目(2016ZX05017-001-HZ02);国家自然科学基金项目(51374269)

Quantitative Characterization of Reservoir Architecture Units of Braided River Tight Sandstone Reservoirs

Qu Xuejiao1,2, Li Jiqiang1,2, Zhang Ji3, Zhao Zhongjun3, Qi Zhilin1,2, Luo Chao1,2   

  1. 1. Key Laboratory of Complex Oil and Gas Exploration and Development of Chongqing, Chongqing 401331, China;
    2. School of Petroleum Engineering, Chongqing University of Science and Technology, Chongqing 401331, China;
    3. Changqing Oilfield Company, PetroChina, Xi'an 710018, China
  • Received:2018-01-07 Published:2018-11-20
  • Supported by:
    Supported by National Science and Technology Major Project(2016ZX05017-001-HZ02) and National Natural Science Foundation of China(51374269)

摘要: 针对现有辫状河储层构型单元定量表征方法关键参数获取困难且可靠性存疑的问题,以储层构型理论为指导,基于现代辫状河沉积、钻井岩心、录井和测井等资料,提出了基于单一辫状河道宽度的构型单元定量表征方法。首先,根据单井构型单元解释结果,确定同期辫状河道平面分布;其次,根据连井对比剖面,确定连井剖面内单一辫状河道间的界线位置;再次,根据现代辫状河单一辫状河道宽度与构型单元关系定量模型,限定辫状水道宽度、复合心滩长度及宽度等4级构型单元规模;最后,在单一辫状河道内确定4级构型单元平面分布,进而在密集井网区对复合心滩进行解剖,确定单个心滩位置和几何形态。采用该方法对苏××提高采收率试验区盒81-3单层辫状河致密砂岩气藏进行了分析,结果表明:该单层砂岩气藏发育5条单一辫状河道,其宽度为1 050~1 890 m;辫状水道宽度为234~435 m;复合心滩长度和宽度分别为1 931~3 569 m、685~1 242 m;单个心滩长度和宽度分别为660~1 880 m、310~1 030 m。

关键词: 定量表征方法, 储层构型单元, 单一辫状河道宽度, 辫状河, 致密砂岩气藏, 苏里格气田盒8下亚段

Abstract: Aiming at the difficulty in obtaining the key parameters and the doubtful reliability of the existing quantitative characterization method for braided river reservoir architecture units, based on the theory of reservoir architecture on single braided channel width, a new method is proposed. Firstly, based on the analysis of single well reservoir architecture units, the horizontal distribution of coeval braided river channels is determined. Secondly, the single braided river channels are set up, and their width can be measured through connecting-well profiles perpendicular to the paleo-current direction. Thirdly, according to the new quantitative model, the width of braided water channel and the length and width of a complex channel bar are calculated. Lastly, in a single braided channel, the plane distribution of four-stage configuration units is determined, and then the compound channel bar is dissected in the dense well network area to determine the location and geometry of the single channel bar. The new method is applied to evaluate the scale of the reservoir architecture units of the braided river tight sandstone gas field of the 1-3 layer of the lower part of 8th member of the Xiashihezi Formation in the Su××EOR test area. It is shown that five single braided river channels are developed in the 1-3 layer of the 8th member within the width of 1 050 m-1 890 m, a braided channel width of 234 m to 435 m;the length and width of a compound channel bar are 1 931-3 569 m and 685-1 242 m respectively,while those of a single channel bars are 660-1 880 m and 310-1 030 m respectively.

Key words: quantitatively characterization method, reservoir architecture units, width of single braided river channel, braided river, tight sandstone gas, the lower part of 8th member of Xiashihezi Formation of Sulige gas field

中图分类号: 

  • P618.13
[1] Miall A D. Architectural Elements Analysis:A News Method of Facies Analysis Applied to Fluvial Deposits[J]. Earth Science Reviews,1985,22(2):261-308.
[2] 吴胜和. 储层表征与建模[M]. 北京:石油工业出版社,2009:1-448. Wu Shenghe. Reservoir Characterization and Modeling[M]. Beijing:Petroleum Industry Press,2009:1-448.
[3] 曾祥平. 储集层构型研究在油田精细开发中的应用[J]. 石油勘探与开发,2010,37(4):483-489. Zeng Xiangping. Application of Reservoir Structure Research in the Fine Exploitation of Oilfields[J]. Petroleum Exploration and Development,2010,37(4):483-489.
[4] 周银邦,吴胜和,计秉玉,等. 曲流河储层构型表征研究进展[J]. 地球科学进展,2011,26(7):695-702. Zhou Yinbang,Wu Shenghe,Ji Bingyu,et al. Research Progress on the Characterization of Fluvial Reservoir Architecture[J]. Advances in Earth Science,2011,26(7):695-702.
[5] 于兴河,马兴祥,穆龙新,等. 辫状河储层地质模式及层次界面分析[M]. 北京:石油工业出版社,2004:1-207. Yu Xinghe,Ma Xingxiang,Mu Longxin,et al. Reservoir Geology Model and Analysis of Hierarchy Surface[M]. Beijing:Petroleum Industry Press,2004:1-207.
[6] Miall A D. Architectural Elements Bounding Surfaces in Fluvial Deposits:Anatomy of the Kayenta Formation (Lower Jurassic),Southwest Colorado[J]. Sedimentary Geology,1988,55(3/4):233-262.
[7] Miall A D. The Geology of Fluvial Deposits:Sedi-mentary Facies,Basin Analysis,and Petroleum Geology[M]. Berlin:Springer Verlag,1996:1-582.
[8] Miall A D. Reconstructing the Architecture and Se-quence Stratigraphy of the Preserved Fluvial Record as a Tool for Reservoir Development:A Reality Check[J]. AAPG Bulletin,2006,90(7):989-1002.
[9] Einsele G. Sedimentary Basins Evolution,Facies,and Sediment Budget[M]. 2nd ed. Berlin:Springer Verlag,2000:1-790.
[10] 刘海,林承焰,张宪国,等. 孔店油田馆陶组辫状河储层构型及剩余油分布规律[J]. 吉林大学学报(地球科学版),2018,48(3):665-677. Liu Hai,Lin Chengyan,Zhang Xianguo,et al. Reservoir Architecture and Remaining Oil Distribution in Braided River of Guantao Formation,Kongdian Oilfield[J]. Journal of Jilin University (Earth Sciences Edition),2018,48(3):665-677.
[11] 张昌民,尹太举,赵磊,等. 辫状河储层内部建筑结构分析[J]. 地质科技情报,2013,32(4):7-13. Zhang Changmin,Yin Taiju,Zhao Lei,et al. Reservoir Architecture Analysis of Braided Channel[J]. Geological Science and Technology Information,2013,32(4):7-13.
[12] 孙天建,穆龙新,赵国良. 砂质辫状河储集层隔夹层类型及其表征方法:以苏丹穆格莱特盆地Hegli油田为例[J]. 石油勘探与开发,2014,41(1):112-120. Sun Tianjian, Mu Longxin, Zhao Guoliang. Classification and Characterization of Barrier-Intercalation in Study Braided River Reservoirs:Taking Hegli Oilfield of Muglad Basin in Sudan as an Example[J]. Petroleum Exploration and Development,2014,41(1):112-120.
[13] Bridge J S,Tye R S. Interpreting the Dimensions of Ancient Fluvial Channel Bars,Channels,and Channel Belts from Wireline-Logs and Cores[J]. AAPG Bulletin,2000,84(8):1205-1228.
[14] Bridge J S. Fluvial Facies Models:Recent Develop-ments[J]. Society for Sedimentary Geology,2006,84(1):83-168.
[15] Kelly S. Scaling and Hierarchy in Braided River and Their Deposits:Examples and Implication for Reservoir Modeling[M]//Sambrook S G H,Best J L,Bristow C S,et al. Braided Rivers:Process,Deposits,Ecology and Management. Oxford:Blackwell Publishing,2006:75-106.
[16] Leclair S F,Bridge J S,Wang F. Preservation of Crossstrata due to Migration of Subaqueous Dunes over Aggrading and Non-Aggrading Beds:Comparison of Experimental Data with Theory[J]. Geoscience Canada, 1997,24(1):55-66.
[17] Bridge J S. Thickness of Sets of Cross Strata and Planar Strata as a Function of Formative Bed-Wave Geometry and Migration,and Aggradation Rate[J]. Geology,1997,25(11):971-974.
[18] 李维锋,高振中,彭德堂. 侧积交错层:辫状河道的主要沉积构造类型[J]. 石油实验地质,1996,18(3):298-302. Li Weifeng,Gao Zhenzhong,Peng Detang. Lateral Accretion Cross-Bedding:The Main Type of Sedimentary Structures in the Braided Channel[J]. Experimental Petroleum Geology,1996,18(3):298-302.
[19] 王彦,彭军,赵冉. 准噶尔盆地西北缘辫状河沉积模式探:以七区下侏罗统八道湾组辫状河沉积为例[J]. 沉积学报,2012,30(2):264-273. Wang Yan,Peng Jun,Zhao Ran. Dentative Discussion on Depositioal Facies Model of Braided Stream in the Northwestern Margin,Junggar Basin:A Case of Braided Stream Depositon of Badaowan Formation,Lower Jurrasic in No. 7 Area[J]. Acta Sedimentologica Sinica,2012,30(2):264-273.
[20] 雷卞军,李跃刚,李浮萍,等. 鄂尔多斯盆地苏里格中部水平井开发区盒8段沉积微相和砂体展布[J]. 古地理学报,2015,17(1):91-105. Lei Bianjun,Li Yuegang,Li Fuping,et al. Sedimentary Microfacies and Sandbody Distribution of the Member 8 of Xiashihezi Formation in Horizontal Well Zone,Central Sulige Area,Ordos Basin[J]. Journal of Paleogeography,2015,17(1):91-105.
[21] 周银邦,吴胜和,岳大力,等. 复合分流河道砂体内部单河道划分:以萨北油田北二西区萨Ⅱ1+2b小层为例[J]. 油气地质与采收率,2010,17(2):4-8. Zhou Yinbang,Wu Shenghe,Yue Dali,et al. Identification of Single Channel in Compound Distributary Sand Body:Case of SⅡ1+2b Layer of West Ⅱ Region,3rd Block of Daqing Oilfield[J]. Petroleum Geology and Recovery Efficiency,2010,17(2):4-8.
[22] 赵忠军,李进步,马志欣,等. 苏36-11提高采收率试验区辫状河储集层构型单元定量表征[J]. 新疆石油地质,2017,38(1):55-61. Zhao Zhongjun,Li Jinbu,Ma Zhixin,et al. Quantitative Characterization of Architecture Units for Braided River Reservior in Su36-11 EOR Test Area[J]. Xinjiang Petroleum Geology,2017,38(1):55-61.
[23] 田景春,吴琦,王峰,等. 鄂尔多斯盆地下石盒子组盒8段储集砂体发育控制因素及沉积模式研究[J]. 岩石学报,2011,27(8):2403-2412. Tian Jingchun,Wu Qi,Wang Feng,et al. Research on Development Factors and the Deposition Model of Large Area Reservoir Sandstones of He8 Section of Xiashihezi Formation of Permian in Ordos Basin[J]. Acta Petrologica Sinica,2011,27(8):2403-2412.
[24] 杨华,付金华,李新社,等. 苏里格大型致密砂岩气藏形成条件及勘探技术[J]. 石油学报,2012,33(增刊1):27-36. Yang Hua,Fu Jinhua,Li Xinshe,et al. Formation Condition and Exploration Technology of Large-Scale Tight Sandstone Gas Reservoir in Sulige[J]. Acta Petrolei Sinica,2012,33(Sup. 1):27-36.
[25] 王国亭,何东博,王少飞,等. 苏里格致密砂岩气田储层岩石孔隙结构及储集性能特征[J]. 石油学报,2013,34(4):660-666. Wang Guoting,He Dongbo,Wang Shaofei,et al. Characteristic of the Pore Structure and Storage Capability of Sulige Tight Sandstone Gasfield[J]. Acta Petrolei Sinica,2013,34(4):660-666.
[26] 李进步,付斌,赵忠军,等. 苏里格气田致密砂岩气藏储层表征技术及其发展展望[J]. 天然气工业,2015,35(12):35-41. Li Jinbu,Fu Bin,Zhao Zhongjun,et al. Characterization Technology for Tight Sandstone Gas Reservoir in the Sulige Gas Field,Ordos Basin,and Its Development Prospect[J]. Natural Gas Industry,2015,35(12):35-41.
[27] 刘鹏,王伟锋,孟蕾,等. 鄂尔多斯盆地上古生界煤层气与致密气联合优选区评价[J]. 吉林大学学报(地球科学版),2016,46(3):692-701. Liu Peng,Wang Weifeng,Meng Lei,et al. Joint Optimization of Coal-Bed Methane and Tight Gas in the Upper Paleozoic of the Ordos Basin[J]. Journal of Jilin University (Earth Sciences Edition),2016,46(3):692-701.
[28] 朱筱敏. 沉积岩石学[M]. 第四版:北京:石油工业出版社,2008:1-484. Zhu Xiaomin. Sedimentary Petrology[M]. 4th ed. Beijing:Petroleum Industry Press,2008:1-484.
[1] 张建坤, 杨国涛, 吴吉忠, 吴鑫, 王方鲁. 黄骅坳陷北部马头营凸起馆陶组砂体成因及展布特征[J]. 吉林大学学报(地球科学版), 2017, 47(1): 48-60.
[2] 陈冬霞, 庞雄奇, 杨克明, 祝渭平, 严青霞. 川西坳陷深层叠复连续型致密砂岩气藏成因及形成过程[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1611-1623.
[3] 单敬福, 张吉, 王继平, 赵忠军, 李浮萍, 陈治华, 石林辉, 刘利峰. 苏里格气田西区盒8亚段辫状河沉积论证与分析[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1597-1607.
[4] 李顺明, 宋新民, 刘曰强, 王友启, 李艳明, 唐后军. 温米退积型与进积型浅水辫状河三角洲沉积模式[J]. J4, 2011, 41(3): 665-672.
[5] 唐海发,彭仕宓,赵彦超. 致密砂岩气藏储层流动单元划分方法及随机模拟[J]. J4, 2007, 37(3): 469-0474.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!