岩性油气藏 ›› 2022, Vol. 34 ›› Issue (2): 31–44.doi: 10.12108/yxyqc.20220203

• 地质勘探 • 上一篇    下一篇

鄂尔多斯盆地樊家川地区三叠系长63储层特征及主控因素

魏钦廉1,2, 王翀峘1,2, 刘军峰3, 胡榕1,2, 刘美荣3, 吕玉娟3   

  1. 1. 西安石油大学 地球科学与工程学院, 西安 710065;
    2. 陕西省油气成藏地质学重点实验室, 西安 710065;
    3. 中国石油长庆油田分公司 第二采油厂, 甘肃 庆阳 745100
  • 收稿日期:2021-08-04 修回日期:2021-10-15 出版日期:2022-03-01 发布日期:2022-03-14
  • 作者简介:魏钦廉(1976-),男,博士,教授,主要从事石油地质方面的教学和研究工作。地址:(710065)陕西省西安市雁塔区电子二路东段18号。Email:wql@xsyu.edu.cn。
  • 基金资助:
    国家科技重大专项“CO2捕集、驱油与埋存技术示范工程”（编号：2016ZX05056）和西安石油大学研究生创新与实践能力培养计划“陇东地区不同物源长6储层孔隙结构差异及其控制因素”（编号：YCS21113106）联合资助

Characteristics and main controlling factors of Triassic Chang 63 reservoir in Fanjiachuan area, Ordos Basin

WEI Qinlian1,2, WANG Chonghuan1,2, LIU Junfeng3, HU Rong1,2, LIU Meirong3, LYU Yujuan3   

  1. 1. School of Earth Science and Engineering, Xi'an Shiyou University, Xi'an 710065, China;
    . 2. Shaanxi Key Laboratory of Petroleum Accumulation Geology, Xi'an Shiyou University, Xi'an 710065, China;
    3. No. 2 Oil Production Plant, PetroChina Changqing Oilfield Company, Qingyang 745100, Gansu, China
  • Received:2021-08-04 Revised:2021-10-15 Online:2022-03-01 Published:2022-03-14

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摘要： 鄂尔多斯盆地樊家川长6储层为新的开发区域，其中长63为主力油层。为研究其致密储层特征及主控因素，开展了岩石薄片鉴定、常规物性及高压压汞分析等，对储层的岩石学、物性及孔隙结构特征进行了详细研究，建立了不同孔隙结构与成岩参数的识别函数，分析了不同孔隙结构储层储集性能主控因素。结果表明：①樊家川地区长63主要岩石类型为岩屑长石砂岩，岩性较细，黏土矿物主要发育水云母，其次是绿泥石，碳酸盐胶结物主要发育铁白云石，其次是铁方解石；②樊家川地区长63储层孔隙主要发育粒间孔和长石溶孔，物性较差，平均孔隙度为9.05%，平均渗透率为0.17 mD，以低孔-特低孔、超低渗储层为主；依据孔隙结构分类标准将樊家川长63储层孔隙结构分成3类，并区分各自的喉道类型与分布区域；③沉积微相是控制樊家川长63储层物性和含油性的关键因素，压实作用是造成储层致密化的主要成岩作用，胶结作用和溶蚀作用是造成孔隙结构差异的重要因素，且不同孔隙结构储层其沉积和成岩作用的影响存在较大差异。该研究结果对长庆油田致密油的综合评价具有指导价值。

关键词: 相控, 砂质碎屑流, 成岩作用, 长63, 三叠系, 樊家川, 鄂尔多斯盆地

Abstract: Chang 6 reservoir in Fanjiachuan area of Ordos Basin is a new development area, of which Chang 63 is the main reservoir.In order to study its tight reservoir characteristics and main controlling factors, casting thin sections, conventional physical properties and high-pressure mercury intrusion data were applied to study the petrological characteristics, physical properties and pore structure characteristics of Chang 63 reservoir in Fanjiachuan area of Ordos Basin, recognition functions for different pore structures and diagenetic parameters were established, and the main controlling factors of reservoir performance with different pore structures were analyzed.The results show that:(1) The Chang 63 reservoir in Fanjiachuan area consists of lithic feldspar sandstone with fine lithologies.Clay minerals mainly develop with hydromica, followed by chlorite, and carbonate cements mainly develop with iron dolomite, followed by iron calcite.(2) The Chang 63 reservoir in Fanjiachuan area mainly develops intergranular pores and feldspar dissolved pores, with poor physical properties, and mainly belongs to lowextra low porosity and ultra-low permeability reservoirs, with an average porosity of 9.05% and an average permeability of 0.17 mD.According to the classification standard of pore structure, the pore structures of Chang 6 3 reservoir can be divided into three types, and their throat types and distribution areas distinguished.(3) Sedimentary microfacies is a key factor controlling the physical properties and oil-bearing properties of Chang 63 reservoir in Fanjiachuan area.Compaction is the main diagenesis causing reservoir densification.Cementation and dissolution are important factors resulting in pore structure differences, and the influences of sedimentation and diagenesis are quite different in reservoirs with different pore structures.The research results have guiding significance for the comprehensive evaluation of tight oil of Changqing Oilfield.

Key words: facies control, sandy debris flow, diagenesis, Chang 63 reservoir, Triassic, Fanjiachuan area, Ordos Basin

中图分类号: 

  • TE122.2
[1] FU Qilong, HU Suyun, XU Zhaohai, et al.Depositional and diagenetic controls on deeply buried Cambrian carbonate reservoirs:Long-wangmiao Formation in the Moxi-Gaoshiti area, Sichuan Basin, southwestern China[J].Marine and Petroleum Geology, 2020, 117:104318.
[2] 代勇.鄂尔多斯盆地上里塬地区长6、长8储层非均质性研究[D].西安:西北大学, 2008.DAI Yong.A study on heterogeneities of Chang 6 and Chang 8 reser-voirs of Yanchang Formation at Shangliyuan area in Ordos Basin[D].Xi'an:Northwest University, 2008.
[3] 付金华, 高振中, 牛小兵, 等.鄂尔多斯盆地环县地区上三叠统延长组长63砂层组沉积微相特征及新认识[J].古地理学报, 2012, 14(6):695-706.FU Jinhua, GAO Zhenzhong, NIU Xiaobing, et al.Sedimentary micro-facies characteristics and new understandings of the Upper Triassic Yanchang Formation Chang 63 interval in Huanxian area in Ordos Basin[J].Journal of Palaeogeography, 2012, 14(6):695-706.
[4] 侯明才, 李旭, 邓敏.鄂尔多斯盆地环县地区三叠系长8-长6油层组沉积相特征[J].成都理工大学学报(自然科学版), 2011, 38(3):241-248.HOU Mingcai, LI Xu, DENG Min.Study on the sedimentary environment of Chang 8-6 oil-bearing formations of Yanchang Formation in Huanxian area, Ordos Basin[J].Journal of Chengdu University of Technology (Science&Technology Edition), 2011, 38(3):241-248.
[5] 钱晓春.油田高含水期剩余油分布研究方法及应用:以樊家川油田中区为例[D].西安:西安石油大学, 2012.QIAN Xiaochun.Study methods and application of residual oil distribution in high water-cut reservoir[D].Xi'an:Xi'an Shiyou University, 2012.
[6] 邵远, 文佳涛, 程文, 等.鄂尔多斯盆地环县地区上三叠统长63物源分析及沉积体系[J].科学技术与工程, 2012, 12(33):8807-8814.SHAO Yuan, WEN Jiatao, CHENG Wen, et al.Provenances analysis and depositional systems of Upper Triassic Chang 63 sand set in Huanxian region in Ordos Basin[J].Science Technology and Engineering, 2012, 12(33):8807-8814.
[7] 帅松青.鄂尔多斯盆地环县-庆城地区延长组长6沉积体系研究[D].荆州:长江大学, 2013.SHUAI Songqing.The research on sedimentary system of the Chang 6 interval of Yanchang Formation in Huanxian-Qingcheng area, Ordos Basin[D].Jingzhou:Yangtze University, 2013.
[8] 程文.环县地区长63沉积微相研究[D].荆州:长江大学, 2012.CHENG Wen.Research of sedimentary microfacies of Chang 6 3 Formation in Huanxian area[D].Jingzhou:Yangtze University, 2012.
[9] 刘化清, 廖建波, 房乃珍, 等.鄂尔多斯盆地环县地区长6沉积体系展布特征[J].沉积学报, 2005, 23(4):584-588.LIU Huaqing, LIAO Jianbo, FANG Naizhen, et al.Distribution characteristics of the Chang 6 sedimentary system (Triassic) in Huanxian area, Ordos Basin[J].Acta Sedimentologica Sinica, 2005, 23(4):584-588.
[10] 魏钦廉, 郑荣才, 肖玲, 等.鄂尔多斯盆地吴旗地区长6储层特征及影响因素分析[J].岩性油气藏, 2007, 19(4):45-50.WEI Qinlian, ZHENG Rongcai, XIAO Ling, et al.Influencing factors and characteristics of Chang 6 reservoir in Wuqi area, Ordos Basin[J].Lithologic Reservoirs, 2007, 19(4):45-50.
[11] 魏钦廉, 崔改霞, 刘美荣, 等.鄂尔多斯盆地西南部二叠系盒8下段储层特征及控制因素[J].岩性油气藏, 2021, 33(2):17-25.WEI Qinlian, CUI Gaixia, LIU Meirong, et al.Reservoir characteristics and controlling factors of Permian lower He 8 member in southwestern Ordos Basin[J].Lithologic Reservoirs, 2021, 33(2):17-25.
[12] 宋国初, 李克勤, 凌升阶.陕甘宁盆地大油田形成与分布[M].北京:石油工业出版社, 1998.SONG Guochu, LI Keqin, LING Shengjie.Formation and distribution of major oil and natural gas cumulation in Shanganning Basin[M].Beijing:Petroleum Industry Press, 1998.
[13] YOUSUF A F, ZHAO Y C, LIU H P, et al.Origin and reservoir properties of deep-water gravity flow sediments in the Upper Triassic Ch6-Ch7 members of the Yanchang Formation in the Jinghe Oilfield, the southern Ordos Basin, China[J].Energy Exploration&Exploitation, 2019, 37(4):1227-1252.
[14] BEARD D C, WEYL P K.Influence of texture on porosity and permeability of unconsolidated sand[J].AAPG Bulletin, 1973, 57(2):349-369.
[15] HUOSEKNECHT D W.Assessing the relative importance of compaction processes and cementation to reduction of porosity in sandstone[J].AAPG Bulletin, 1987, 71(6):633-642.
[16] 付晶, 吴胜和, 付金华, 等.鄂尔多斯盆地陇东地区延长组储层定量成岩相研究[J].地学前缘, 2013, 20(2):9086-9097.FU Jing, WU Shenghe, FU Jinhua, et al.Research on quantitative diagenetic facies of the Yanchang Formation in Longdong area, Ordos Basin[J].Earth Science Frontiers, 2013, 20(2):9086-9097.
[17] 王振鹏, 陈民锋, 尹承哲.砾岩油藏水驱开发潜力分级评价[J].岩性油气藏, 2018, 30(5):109-115.WANG Zhenpeng, CHEN Minfeng, YIN Chengzhe.Development potential classi-fication evaluation for water-flooding in conglomerate reservoir[J].Lithologic Reservoirs, 2018, 30(5):109-115.
[18] MENG Dewei, JIA Ailin, JI Guang, et al.Water and gas distribution and its controlling factors of large scale tight sand gas fields:A case study of western Sulige gas field, Ordos Basin, NW China[J].Petroleum Exploration and Development, 2016, 43(4):663-671.
[19] 邹才能, 赵政璋, 杨华, 等.陆相湖盆深水砂质碎屑流成因机制与分布特征:以鄂尔多斯盆地为例[J].沉积学报, 2009, 27(6):1065-1075.ZOU Caineng, ZHAO Zhenzhang, YANG Hua, et al.Genetic mechanism and distribution of sandy debris flows in Terrestrial Lacustrine Basin[J].Acta Sedimentologica Sinica, 2009, 27(6):1065-1075.
[20] 刘为, 杨希冰, 张秀苹, 等.莺歌海盆地东部黄流组重力流沉积特征及其控制因素[J].岩性油气藏, 2019, 31(2):75-82.LIU Wei, YANG Xibing, ZHANG Xiuping, et al.Characteristics and controlling factors of gravity flow deposits of Huangliu Formation in eastern Yinggehai Basin[J].Lithologic Reservoirs, 2019, 31(2):75-82.
[21] 曹思佳, 孙增玖, 党虎强, 等.致密油薄砂体储层预测技术及应用实效:以松辽盆地敖南区块下白垩统泉头组为例[J].岩性油气藏, 2021, 33(1):239-247.CAO Sijia, SUN Zengjiu, DANG Huqiang, et al.Prediction technology of tight oil thin sand reservoir and its application effect:A case study of Lower Cretaceous Quantou Formation in Aonan block, Songliao Basin[J].Lithologic Reservoirs, 2021, 33(1):239-247.
[22] 兰叶芳, 邓秀芹, 程党性, 等.鄂尔多斯盆地华庆地区长6油层组砂岩成岩相及储层质量评价[J].岩石矿物学杂志, 2014, 33(1):51-63.LAN Yefang, DENG Xiuqin, CHENG Dangxing, et al.Diagenetic fades and reservoir quality evaluation of Chang 6 sandstone reservoir in the Upper Triassic Yanchang Formation of Huaqing area, Ordos Basin[J].Acta Petrologica et Mineralogica, 2014, 33(1):51-63.
[23] 张满郎, 孔凡志, 谷江锐, 等.九龙山气田珍珠冲组砂砾岩储层评价及有利区优选[J].岩性油气藏, 2020, 32(3):1-13.ZHANG Manlang, KONG Fanzhi, GU Jiangrui, et al.Assessment of glutenite reservoirs and optimization of prospects of Zhenzhuchong Formation in Jiulongshan gas field, Sichuan Basin[J].Lithologic Reservoirs, 2020, 32(3):1-13.
[24] 傅强, 李璟, 邓秀琴, 等.沉积事件对深水沉积过程的影响:以鄂尔多斯盆地华庆地区长6油层组为例[J].岩性油气藏, 2019, 31(1):20-29.FU Qiang, LI Jing, DENG Xiuqin, et al.Influence of sedimentary events on deep water sedimentation process:A case of Chang 6 reservoir in Huaqing area, Ordos Basin[J].Lithologic Reservoirs, 2019, 31(1):20-29.
[25] 刘翰林, 杨友运, 王凤琴, 等.致密砂岩储集层微观结构特征及成因分析:以鄂尔多斯盆地陇东地区长6段和长8段为例[J].石油勘探与开发, 2018, 45(2):223-234.LIU Hanlin, YANG Youyun, WANG Fengqin, et al.Micro pore and throat characteristics and origin of tight sandstone reservoirs:A case study of the Triassic Chang 6 and Chang 8 members in Longdong area, Ordos Basin[J].Petroleum Exploration and Development, 2018, 45(2):223-234.
[26] 魏钦廉, 卢帆雨, 淡卫东, 等.致密砂岩储层成岩相类型划分:以鄂尔多斯盆地环县西部地区长33储层为例[J].断块油气田, 2020, 27(5):591-596.WEI Qinlian, LU Fanyu, DAN Weidong, et al.Classification of diagenetic fades in tight sandstone reservoirs:A case study of Chang 33 reservoir in the west of Huanxian, Ordos Basin[J].Fault-Block Oil&Gas Field, 2020, 27(5):591-596.
[27] 吴浩, 刘锐娥, 纪友亮, 等.典型致密砂岩气储层孔隙结构分类及其意义:以鄂尔多斯盆地盒8段为例[J].天然气地球科学, 2016, 27(5):835-843.WU Hao, LIU Ruie, JI Youliang, et al.Classification of pore structures in typical tight sandstone gas reservoir and its significance:A case study of the He 8 member of Upper Palaeozoic Shihezi Formation in Ordos Basin, China[J].Natural Gas Geoscience, 2016, 27(5):835-843.
[28] WANG Junjie, WU Shenghe, LI Qing, et al.Characterization of the pore-throat size of tight oil reservoirs and its control on reservoir phy-sical properties:A case study of the Triassic tight sandstone of the sediment gravity flow in the Ordos Basin, China[J].Journal of Petroleum Science and Engineering, 2020, 186:106701.
[29] 王继伟, 朱玉双, 饶欣久, 等.鄂尔多斯盆地胡尖山地区长61致密砂岩储层成岩特征与孔隙度定量恢复[J].岩性油气藏, 2020, 32(3):34-43.WANG Jiwei, ZHU Yushuang, RAO Xinjiu, et al.Diagenetic characteristics and quantitative porosity restoration of Chang 6 1 tight sandstone reservoir in Hujianshan area, Ordos Basin[J].Lithologic Reservoirs, 2020, 32(3):34-43.
[30] 周晓峰, 唐海忠, 魏军, 等.砂岩高岭石赋存状态、成因机制及其对物性的影响:以酒泉盆地营尔凹陷下沟组为例[J].东北石油大学学报, 2019, 43(1):40-49.ZHOU Xiaofeng, TANG Haizhong, WEI Jun, et al.Occurrences and formation mechanisms of kaolinite cements in sandstones and their effects on sandstone property:Taking Xiagou Formation in Yinger Depression, Jiuquan Basin as an example[J].Natural Gas Geoscience, 2019, 43(1):40-49.
[31] 沈健.鄂尔多斯盆地陇东地区致密砂岩储层碳酸盐胶结物特征及成因机理[J].岩性油气藏, 2020, 32(2):24-32.SHEN Jian.Carbonate cementation characteristics and genetic mechanism of tight sandstone reservoirs in Longdong area, Ordos Basin[J].Lithologic Reservoirs, 2020, 32(2):24-32.
[32] LIAN P Q, CHENG L S, LIU L F.Characteristics of productivity curves in abnormal high-pressure reservoirs[J].Petroleum Science and Technology, 2011, 29(2):109-120.
[33] KHAN Z, SACHAN H K, AHMAD A H M, et al.Microfacies, diagenesis, and stable isotope analysis of the Jurassic Jumara Dome carbonates, Kachchh, western India:Implications for depositional environments and reservoir quality[J].Geological Journal, 2020, 55(1):1041-1061.
[34] 楚美娟, 郭正权, 齐亚林, 等.鄂尔多斯盆地延长组长8储层定量化成岩作用及成岩相分析.天然气地球科学, 2013, 24(3):477-484.CHU Meijuan, GUO Zhengquan, QI Yalin, et al.Quantitative diagenesis and diagenetic facies analysis on Chang 8 reservoir of Yanchang Formation in Ordos Basin[J].Natural Gas Geoscience, 2013, 24(3):477-484.
[35] 王志康, 林良彪, 余瑜, 等.川西新场地区须家河组第二段优质储层主控因素[J].成都理工大学学报(自然科学版), 2020, 47(6):661-672.WANG Zhikang, LIN Liangbiao, YU Yu, et al.The main controlling factors of high quality reservoir in the second member of Xujiahe Formation in Xinchang area, western Sichuan, China[J].Journal of Chengdu University of Technology (Science&Technology Edition), 2020, 47(6):661-672.
[36] 呼延钰莹, 姜福杰, 庞雄奇, 等.鄂尔多斯盆地东缘康宁地区二叠系致密储层成岩作用与孔隙度演化[J].岩性油气藏, 2019, 31(2):56-65.HUYAN Yuying, JIANG Fujie, PANG Xiongqi, et al.Diagenesis and porosity evolution of Permian tight reservoirs in Kangning area, eastern margin of Ordos Basin[J].Lithologic Reservoirs, 2019, 31(2):56-65.
[37] 曹英权, 王清斌, 曲希玉, 等.岩屑的有机酸溶蚀实验及验证:以渤中凹陷CFD6-4油田东营组为例[J].石油学报, 2020, 41(7):841-852.CAO Yingquan, WANG Qingbin, QU Xiyu, et al.A dissolution experiment of organic acid of cuttings and its verification:A case study of the Dongying Formation of the CFD6-4 oilfield, Bozhong Sag[J].Acta Petrolei Sinica, 2020, 41(7):841-852.
[38] 远光辉.成岩过程中长石和碳酸盐矿物溶蚀机理及其物性响应[J].青岛:中国石油大学(华东), 2015.YUAN Guanghui.Genetic mechanism of dissolution of feldspars and carbonate minerals during diagenesis and its impact on reservoir property[J].Qingdao:China University of Petroleum (East China), 2015.
[39] 李书恒, 方国庆, 杨金龙, 等.鄂尔多斯盆地超低渗透储层成因研究及意义[J].岩性油气藏, 2012, 24(6):32-37.LI Shuheng, FANG Guoqing, YANG Jinlong, et al.Origin of ultra-low permeability reservoirs in Ordos Basin and its significance[J].Lithologic Reservoirs, 2012, 24(6):32-37.
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