鄂尔多斯盆地马岭油田长8_1储层不同成岩相类型可动流体赋存特征分析
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Occurrence Characteristics of Movable Fluids in Different Diagenetic Facies of the Chang 8_1 Reservoir,Maling Oilfield,Ordos Basin
  • 作者:黎盼 ; 孙卫 ; 高永利 ; 折文旭 ; 杜堃
  • 英文作者:LI Pan;SUN Wei;GAO Yongli;SHE Wenxu;DU Kun;State Key Laboratory for Continental Dynamics and Department of Geology,Northwest University;College of Petroleum Engineering,Xi'an Shiyou University;
  • 关键词:马岭油田 ; 长81储层 ; 不同成岩相 ; 微观孔隙结构 ; 可动流体 ; 鄂尔多斯盆地
  • 英文关键词:Maling oilfield;;Chang 81 reservoir;;different diagenetic facies;;microscopic pore structure;;movable fluids;;Ordos basin
  • 中文刊名:DZKT
  • 英文刊名:Geology and Exploration
  • 机构:西北大学地质学系/大陆动力学国家重点实验室;西安石油大学石油工程学院;
  • 出版日期:2019-03-15
  • 出版单位:地质与勘探
  • 年:2019
  • 期:v.55;No.483
  • 基金:国家科技重大专项大型油气田及煤层气开发(编号:2011ZX05044);; 陕西省青年人才基金(编号:No.2016JQ4022)联合资助
  • 语种:中文;
  • 页:DZKT201902020
  • 页数:12
  • CN:02
  • ISSN:11-2043/P
  • 分类号:205-216
摘要
针对鄂尔多斯盆地马岭油田长8_1储层微观非均质性强、微观孔隙结构复杂、流体分布特征差异性明显等问题,利用核磁共振技术对不同成岩相类型储层可动流体进行定量评价,辅助以常规物性、图像孔隙、铸体薄片、扫描电镜、高压压汞和恒速压汞等微观实验,分析不同类型的成岩相可动流体赋存特征差异性及其主控因素。研究结果表明,研究区主要分成四种成岩相,分别为绿泥石+伊利石胶结-粒间孔相、伊利石+高岭石胶结-粒间孔+溶蚀相、绿泥石+伊利石胶结-溶蚀相和碳酸盐胶结致密相。四种不同成岩相类型的微观孔隙结构有着明显的差异,微观孔隙结构差异是造成可动流体饱和度差异的主要因素。不同成岩相类型的储层渗透率与可动流体参数的相关性较强,储层物性越好,可动流体参数变化幅度越大;孔喉半径大小、孔喉半径比、分选系数、孔喉进汞饱和度以及粘土矿物的充填是影响不同成岩相类型可动流体赋存特征差异的主控因素。其中有效喉道半径、孔喉进汞饱和度、孔喉半径比是影响可动流体饱和度的主要因素,分选系数对可动流体饱和度影响较明显,储层物性对可动流体饱和度的影响较小。
        The exploration of the Chang 8_1 reservoir in Maling Oilfield,Ordos Basin,has been challenged by strong heterogeneity,complicated microscopic pore structures,low saturation of movable fluids,and different fluid distribution characteristics. To solve this problem,this study used nuclear magnetic resonance( NMR) technique to quantitatively evaluate the movable fluids in the reservoir with different diagenetic facies types. Moreover,microscopic experiments were conducted to analyze the occurrence characteristics and influential factors of movable fluids in different diagenetic facies types,including conventional physical property analysis,image porosity measurement,casting thin section observation,SEM analysis,high pressure mercury intrusion tests,and rate-controlled mercury intrusion tests. The results show that four types of diagenetic facies could be divided in the area,namely chlorite + illite cementation-intergranular pore facies,illite + kaolinite cementation-intergranular pore + solution facies,chlorite + illite cementation-solution facies and carbonate cementation dense facies. There are obvious differences in the micro-pore structure of these four types of diagenetic facies and micro-pore structure is the main factor that causes the difference of the saturation of movable fluid. Reservoir permeability is well correlated with movable fluid saturation.Generally,better physical properties lead to larger variation of movable fluid saturation. The pore throat radius,pore-throat radius ratio,sorting coefficient,maximum mercury saturation in pores and throats,and interstitial clay minerals are the main factors that influence the occurrence characteristics in different diagenetic facies. Among them,the effective pore throat radius,maximum mercury saturation and pore-throat radius ratio are the dominant factors; the sorting coefficient has a certain influence; and physical properties can pose a little effect on the movable fluid saturation.
引文
Bai R T,Li Z P,Wang H L,Liu X Y,Wei Q,Li H.2016.Fractal nature of microscopic pore throat structure in Chang 7 tight oil reservoir of Longdong area[J].Sci.Technol.Eng,16(5):54-59.
    Cao Lei,Sun Wei,Sheng Jun,Huo Lei,Chen Qiang,Xie Caihua.2016.Amethod to determine movable fluid saturation of low-permeability and tight oil reservoirs-by taking tight oil reservoirs in sixth member of Yanchang Formation in Banqiao area as an example[J].Journal of Yangtze University(Natural Science Edition),13(20):1-8(in Chinese with English abstract).
    Chen Dayou,Zhu Yushuang,Zhang Jiaosheng,Du Shouli,Sang Shizhe,Li Chao.2015.Diagenesis and favorable diagenetic facies of the eight member of Yanchang Formation in Maling area,the Ordos basin[J].Petroleum Geology&Experiment,37(6):721-728(in Chinese with English abstract).
    Cheng Jinghua,Li Rongxi,Tan Xiaoli,Li Delu,Zhao Bangsheng,Li Jiajia,Wu Xiaoli,Wang Ning.2016.Impact of diagenetic facies on mechanical properties of sandstone rock in low-permeability reservoirs:A case study of the Upper Paleozoic gas reservoir in east Ordos basin[J].Acta Petrolei Sinica,37(10):1256-1264(in Chinese with English abstract).
    Dai Q Q,Luo Q,Zhang C,Lu C J,Zhang Y Z,Lu S J,Zhao Y.2016.Pore structure characteristics of tight-oil sandstone reservoir based on a new parameter measured by NMR experiment:A case study of seventh Member in Yanchang Formation,Ordos basin[J].Acta Pet.Sin,37(7):887-897.
    Daigle H.,Johnson A..2016.Combing mercury intrusion and nuclear magnetic resonance measurements using percolation theory[J].Transp.Porous Media,111(3):669-679.
    Gao Hui,Li Huazhou.2015.Determination of movable fluid percentage and movable fluid porosity in ultra-low permeability sandstone using nuclear magnetic resonance(NMR)technique[J].Journal of Petroleum Science and Engineering,133(9):258-267.
    Li Pan,Liu Zhidi,Chen Yuming,Zhao Jiahong.2017.Summarization of application for identifying diagenetic in low porosity and low permeability reservoirs using well-logging information[J].Progress in Geophysics,32(1):183-190(in Chinese with English abstract).
    Li Pan,Sun Wei,Gao Yongli,Zhang Xi,Du Kun,Bai Yunyun.2018.Quantitative calculation of tight sandstone reservoir porosity evolution based on different diagenesis:A case study from Chang 81reservoir of Maling area,Ordos basin[J].Geological Science and Technology Infornation,37(1):135-142(in Chinese with English abstract).
    Li Y,Fan Y R,Deng S G,Liu B K.2008.Experimental study of pore structure with nuclear magnetic resonance[J].Prog.Explor.Geophys,31(2):129-132.
    Liu Jiangbin,Ren Zhanli,Li Wenhou,Hu Cuilin.2017.Diagenesis and porosity evolution in the Chang 81reservoir of the Triassic Yanchang Formation in the Xunyi area,Ordos Basin[J].Geology and Exploration,53(2):0371-0380(in Chinses with English abstract).
    Ma Baoquan,Yang Shaochun,Zhang Hong,Bai Qinglin,Yang Zhaolin.2018.Quantitative evaluation of low-permeability sandstone diagenetic facies based on DEA method:A case study of Chang 81reservoirs in the Yanwu region,Ordos basin[J].Journal of China University of Mining&Technology,47(2):373-382(in Chinese with English abstract).
    Ma Chunlin,Wang Ruijie,Luo Bilin,Duan Wenbiao,Feng Chunyan,Wang Shaoping,Suo Yuxia,Qiang Zhenzhen.2012.Characteristics of Chang 8 oil reservoir and distribution of oil reservoirs in Maling oilfield,Ordos basin[J].Natural Gas Geoscience,23(3):514-519(in Chinese with English abstract).
    Pang Zhenyu,Li Yan,Zhao Xisen,Dang Hailong,Li Jian,Duan Jingjie.2017.Study on movable fluid saturation in ultra low permeability reservoir:taking Chang 6 reservoir in Ganguyi oil field as an example[J].Progress in Geophysics,32(2):0702-0708(in Chinese with English abstract).
    Qu Xuefeng,Sun Wei,Lei Qihong,Huang Hai,Huo Lei,Chen Bin.2016.Study on saturation of movable fluid in the low-permeability sandstone reservoirs of Huaqing oilfield and its influencing factors[J].Journal of Xi'an Shiyou University(Natural Science),31(2):93-98(in Chinese with English abstract).
    Ren Ying,Sun Wei,Ming Hongxia,Zhang Xi,Huo Lei,Cao Lei,Chen Bin.2016.Characteristics of movable fluids in different diagenetic facies and the influencing factors of low-permeability reservoir:Taking Chang 6 Jiyuan oilfield as an example[J].Geoscience,30(5):1124-1133(in Chinese with English abstract).
    Ren Xiaoxia,Li Aifen,Wang Yongzheng,Wu Songtao,Wang Guijuan.2015.Pore structure of tight sand reservoir and its influence on percolation-taking the Chang 8 reservoir in Maling oilfield in Ordos basin as an example[J].Oil&Gas Geology,36(5):774-779(in Chinese with English abstract).
    Ren Yinghui,Wu Ke,He Kangning,Wu Guanzhou,Zhu Yalin,Wu Hanning,Yang Youyun.2017.Application of NMR technique to movable fluid of ultra-low permeability and tight reservoir:A case study on the Yanchang Formation in Longdong area,Ordos basin[J].Journal of Mineralogy and Petrology,37(1):103-110.
    Shen Jun,Sun Wei,Liu Yanni,Li Gang,Zhang Tao,Cao Lei.2016.Effect of the difference of low permeability reservoir microscopic pore structure on movable fluid:A case for the Chang6 reservoir of Jiyuan and Banqiao areas in Ordos basin[J].Geological Science and Technology Information,35(3):167-172(in Chinese with English abstract).
    SY/T 6285-2011.2011.Oil and gas reservoir evaluation methods[S].Beijing:Petroleum Industry Press(in Chinese).
    Timur A.1969.Pulsed nuclear magnetic resonance studies of porosity,movable fluid,and permeability of sandstone[J].Pet.Sci.Eng,21:775-786.
    Wang Meng,Zeng Ming,Chen Hongao,Yang Gang,Xu Jifang,Qiu Haibin,Guo Hongguang,Wang Jiamin.2017.Influencing factors of tight reservoirs and favorable diagenetic facies:A case study of Chang 8reservoir of the Upper Triassic Yanchang Formation in Maling oilfield,Ordos basin[J].Lithologic Reservoirs,29(1):59-70(in Chinese with English abstract).
    Wang Wei,Niu Xiaobing,Liang Xiaowei,Dan Weidong.2017.Study on movable fluid saturation in ultra low permeability reservoir:Taking Chang 6 reservoir in Ganguyi oil field as an example[J].Geological Science and Technology Information,36(1):183-187(in Chinese with English abstract).
    Wu Changhui,Zhao Xisen.2017.Determination of T2cut-off value of nuclear magnetic resonance in tight sandstone reservoir and lower limit of movable fluid:A case study of Chang 9 reservoir of Wucangbao oilfield[J].Unconventional Oil&Gas,4(2):91-94(in Chinese with English abstract).
    Yang P,Guo H K,Yang D Y.2013.Determination of residue oil saturation during water flooding in tight oil formations with NMR relaxometry measurements[J].Energy Fuels,27(10):5750-5756.
    Yao Y,Liu D.2012.Comparison of low-field NMR and mercury intrusion porosimetry in characterizing pore size distributions of coals[J].Fuel,95:152-158.
    Zhang Hao,Chen Gang,Tang Xin,Dang Yongchao,Shao Fei,Li Li,Chen Chen,Jia Ran.2017.Evaluation of tight oil reservoir diagenetic facies by logging response:A case study of the Chang 7 reservoir in Heshui area,Ordos basin[J].Geological Science and Technology Information,36(3):262-270(in Chinese with English abstract).
    Zheng Qinghua,Liu Yiqun.2015.Microscopic pore structure and movable fluid saturation of ultra low permeability reservoir[J].Geological Science and Technology Information,34(4):124-131(in Chinese with English abstract).
    Zhang Xi,Sun Wei,Ren Dazhong.2017.Quantitative calculation of porosity evolution and formation mechanism of tight sandstone in Chang 63reservoirs of the Huaqing area,Ordos basin[J].Geology and Exploration,53(4):0807-0817(in Chinese with English abstract).
    曹雷,孙卫,盛军,霍磊,陈强,谢彩花.2016.低渗透致密油藏可动流体饱和度计算方法-以板桥地区长6油层组致密油储层为例[J].长江大学学报(自然版),13(20):1-8.
    陈大友,朱玉双,张皎生,杜守礼,桑轼辙,李超,刘萍.2015.鄂尔多斯盆地马岭地区长8储层成岩作用与有利成岩相带[J].石油实验地质,37(6):721-728.
    程敬华,李荣西,覃小丽,李得路,赵帮胜,李佳佳,吴小力,王宁.2016.成岩相对低渗透储层砂岩岩石力学性质的控制-以鄂尔多斯盆地东部上古生界天然气储层为例[J].石油学报,37(10):1256-1264.
    李盼,刘之的,陈玉明,赵家宏.2017.测井资料在低孔-低渗储集层成岩相识别中的应用综述[J].地球物理学进展,32(1):183-190.
    黎盼,孙卫,高永利,张茜,杜堃,白云云.2018.致密砂岩储层差异性成岩演化对孔隙度定量演化表征影响:以鄂尔多斯盆地马岭地区长81储层为例[J].地质科技情报,37(1):135-142.
    刘江斌,任战利,李文厚,胡桂林.2017.旬邑地区三叠系延长组长81储层成岩作用与孔隙演化[J].地质与勘探,53(2):0371-0380.
    马宝全,杨少春,张鸿,白青林,杨兆林.2018.基于DEA定量表征低渗透砂岩储层成岩相-以鄂尔多斯盆地演武地区延长组长81段为例[J].中国矿业大学学报,47(2):373-382.
    马春林,王瑞杰,罗必林,段文标,冯春燕,王绍平,锁玉霞,强阵阵.2012.鄂尔多斯盆地马岭油田长8油层组储层特征与油藏分布研究[J].天然气地球科学,23(3):514-519.
    庞振宇,李艳,赵习森,党海龙,李剑,段景杰.2017.特低渗储层可动流体饱和度研究-以甘谷驿油田长6储层为例[J].地球物理学进展,32(2):0702-0708.
    屈雪峰,孙卫,雷启鸿,黄海,霍磊.2016.华庆油田低渗透砂岩储层可动流体饱和度及其影响因素[J].西安石油大学学报(自然科学版),31(2):93-98.
    任颖,孙卫,明红霞,张茜,霍磊,曹雷,陈斌.2016.低渗透储层不同成岩相可动流体赋存特征及其影响因素分析-以鄂尔多斯盆地姬塬地区长6段储层为例[J].现代地质,30(5):1124-1133.
    任晓霞,李爱芬,王永政,吴松涛,王桂娟.2015.致密砂岩储层孔隙结构及其对渗流的影响-以鄂尔多斯盆地马岭油田长8储层为例[J].石油与天然气地质,36(5):774-779.
    任颖惠,吴珂,何康宁,吴广洲,朱亚林,吴汉宁,杨友运.2017.核磁共振技术在研究超低渗-致密油储层可动流体中的应用-以鄂尔多斯盆地陇东地区延长组为例[J].矿物岩石,37(1):103-110.
    盛军,孙卫,刘艳妮,李纲,张弢,曹雷.2016.低渗透油藏储层微观孔隙结构差异对可动流体的影响:以鄂尔多斯盆地姬塬与板桥地区长6储层为例[J].地质科技情报,35(3):167-172.
    SY/T 6285-2011.2011.油气储层评价方法[S].北京:石油工业出版社.
    王猛,曾明,陈鸿傲,杨刚,徐绩芳,邱海滨,郭红光,王家敏.2017.储层致密化影响因素分析与有利成岩相带预测-以马岭油田长8油层组砂岩储层为例[J].岩性油气藏,29(1):59-70.
    王伟,牛小兵,梁晓伟,淡卫东.2017.鄂尔多斯盆地致密砂岩储层可动流体特征:以姬塬地区延长组长7段油层组为例[J].地质科技情报,36(1):183-187.
    吴长辉,赵习森.2017.致密砂岩油藏核磁共振T2截止值的确定及可动流体喉道下限-以吴仓堡下组合长9油藏为例[J].非常规油气,4(2):91-94.
    张浩,陈刚,唐鑫,党永潮,邵飞,李莉,陈晨,贾然.2017.应用测井响应评价致密油储层成岩相:以鄂尔多斯盆地合水地区长7储层为例[J].地质科技情报,36(3):262-270.
    郑庆华,柳益群.2015.特低渗透储层微观孔隙结构和可动流体饱和度特征[J].地质科技情报,34(4):124-131.
    张茜,孙卫,任大忠.2017.鄂尔多斯盆地华庆地区长63储层成藏期孔隙度定量演化及致密成因机理[J].地质与勘探,53(4):0807-0817.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700