岩性油气藏 ›› 2017, Vol. 29 ›› Issue (1): 51–58.doi: 10.3969/j.issn.1673-8926.2017.01.007

• 油气地质 • 上一篇    下一篇

鄂尔多斯盆地周家湾地区长8致密砂岩储层特征及影响因素

王维斌1,2, 朱静1,2, 马文忠1,2, 冯顺彦1,2, 刘艳妮1,2, 赵静3   

  1. 1. 中国石油长庆油田分公司 勘探开发研究院, 西安 710018;
    2. 低渗透油气田勘探开发国家工程实验室, 西安 710018;
    3. 中国石油长庆油田分公司 西安长庆化工集团有限公司, 西安 710018
  • 收稿日期:2016-08-12 修回日期:2016-09-29 出版日期:2017-01-21 发布日期:2017-01-21
  • 第一作者:王维斌(1986-),男,硕士,工程师,主要从事油藏评价及油田开发方面的研究工作。地址:(710018)陕西省西安市未央区凤城四路中国石油长庆油田分公司勘探开发研究院。电话:(029)86594214。Email:wbwang_cq@petrochina.com.cn。
  • 基金资助:
    国家重大科技专项“鄂尔多斯盆地致密油资源潜力、甜点预测与关键技术应用”(编号:2016ZX05046-005)资助

Characteristics and influencing factors of Chang 8 tight sandstone reservoir of Triassic Yanchang Formation in Zhoujiawan area, Ordos Basin

WANG Weibin1,2, ZHU Jing1,2, MA Wenzhong1,2, FENG Shunyan1,2, LIU Yanni1,2, ZHAO Jing3   

  1. 1. Research Institute of Exploration and Development, PetroChina Changqing Oilfield Company, Xi'an 710018, China;
    2. National Engineering Laboratory for Exploration and Development of Low Permeability Oil and Gas Fields, Xi'an 710018, China;
    3. Xi'an Changqing Chemical Group Co., Ltd, PetroChina Changqing Oilfield Company, Xi'an 710018, China
  • Received:2016-08-12 Revised:2016-09-29 Online:2017-01-21 Published:2017-01-21

摘要: 鄂尔多斯盆地周家湾地区三叠系延长组长8 致密砂岩储层特征和优质储层控制因素研究薄弱,制约了该区油气的勘探与开发进程。在岩心观察的基础上,结合大量铸体薄片、扫描电镜、压汞及常规物性等分析化验资料,对周家湾地区长8 致密砂岩储层的宏观和微观特征及其影响因素进行了研究。结果表明,长8 储层岩石类型以岩屑长石砂岩和长石岩屑砂岩为主,填隙物含量较高;长81 和长82小层的孔隙度分别为8.03% 和8.17%,渗透率分别为0.17 mD 和0.25 mD,均属致密砂岩储层,储层物性较差;储集空间以剩余原生粒间孔和次生长石溶孔为主,微细喉道,形成了长8 储层高排驱压力、高中值压力及低退汞效率的特征。受沉积和成岩作用的共同控制,研究区长8 油层组有利储层主要发育于分流河道和水下分流河道沉积微相中,压实作用、碳酸盐胶结作用和硅质胶结作用致使储层物性变差,溶蚀作用则有效改善了储层孔渗条件。

Abstract: The characteristics and controlling factors of Chang 8 tight sandstone reservoir of Triassic Yanchang Formation in Ordos Basin is unclear,which restricts the hydrocarbon exploration and development in this area. Based on core observation and data of cast thin sections,scanning electronic microscope,mercury intrusion and conventional physical properties,the characteristics and influencing factors of the Chang 8 tight sandstone reservoir were analyzed. The results show that the Chang 8 reservoir rocks are mainly composed of lithic arkose and feldspathic lithic sandstones,with high content of matrix. The porosity of Chang 81 and Chang 82 sublayers are 8.03% and 8.17%,respectively,and the permeability are 0.17 mD and 0.25 mD,respectively, showing the poor properties and tight sandstone reservoirs. The pores are dominated by the remaining primary intergranular pores and secondary feldspar dissolved pores,together with small throat,which characterizes the Chang 8 reservoir with high expulsion pressure,high median pressure and low ejection efficiency. Under the control of deposition and diagenesis,the favorable reservoirs are mainly developed in distributary channel and subaqueous distributary channel. Compaction,carbonate and siliceous cementation make the reservoir properties poor,and dissolution improve the reservoir porosity and permeability.

中图分类号: 

  • TE121.2
[1] 杨华,窦伟坦,喻建,等. 鄂尔多斯盆地低渗透油藏勘探新技 术.中国石油勘探,2003,8(1):32-33. YANG H,DOU W T,YU J,et al. New technology for exploration of low permeability reservoirs in Ordos Basin. China Petroleum Exploration,2003,8(1):32-33.
[2] 李士祥,楚美娟,黄锦秀,等. 鄂尔多斯盆地延长组长8 油层 组砂体结构特征及成因机理. 石油学报,2013,34(3):435- 444. LI S X,CHU M J,HUANG J X,et al. Characteristics and genetic mechanism of sandbody architecture in Chang- 8 oil layer of Yanchang Formation,Ordos Basin. Acta Petrolei Sinica,2013,34(3):435-444.
[3] 韩永林,王成玉,王海红,等. 姬塬地区长8 油层组浅水三角 洲沉积特征.沉积学报,2009,27(6):1057-1064. HAN Y L,WANG C Y,WANG H H,et al. Sedimentary characteristics of shallow water deltas in Chang 8 subsection of Yanchang Formation,Jiyuan Area. Acta Sedimentologica Sinica, 2009,27(6):1057-1064.
[4] 李元昊,刘池洋,独育国,等. 鄂尔多斯盆地西北部上三叠统 延长组长8 油层组浅水三角洲沉积特征及湖岸线控砂. 古地 理学报,2009,11(3):265-274. LI Y H,LIU C Y,DU Y G,et al. Sedimentary characteristics of shallow water delta and lake shoreline control on sandbodies of Chang 8 oil- bearing interval of the Upper Triassic Yanchang Formation in Northwestern Ordos Basin. Journal of Palaeogeography, 2009,11(3):265-274.
[5] 赵小强,万友利,易超,等. 鄂尔多斯盆地姬塬油田长8 段沉积 相研究. 岩性油气藏,2011,23(4):94-99. ZHAO X Q,WAN Y L,YI C,et al. Study on sedimentary facies of Chang 8 member in Jiyuan Oilfield,Ordos Basin. Lithologic Reservoirs,2011,23(4):94-99.
[6] 刘化清,李相博,完颜容,等. 鄂尔多斯盆地长8 油层组古地理 环境与沉积特征. 沉积学报,2011,29(6):1086-1095. LIU H Q,LI X B,WANYAN R,et al. Palaeogeographic and sedimentological characteristics of the Triassic Chang 8,Ordos Basin,China. Acta Petrolei Sinica,2011,29(6):1086-1095.
[7] 姚光庆,马正,赵彦超,等. 浅水三角洲分流河道砂体储层特 征.石油学报,1995,16(1):24-31. YAO G Q,MA Z,ZHAO Y C,et al. Reservoir characteristics of distributary channel sand bodies of shallow water delta. Acta Petrolei Sinica,1995,16(1):24-31.
[8] 罗顺社,银晓. 鄂尔多斯盆地姬塬地区延长组长8 沉积相的 研究. 石油天然气学报,2008,30(4):5-9. LUO S S,YIN X. Study on the sedimentary facies of Chang 8 oil group ofYanchang Formation in Jiyuan area of Ordos Basin. Journal of Oil and Gas Technology,2008,30(4):5-9.
[9] 谢正温,谢渊,王剑,等. 鄂尔多斯盆地富县地区延长组主要 油层组储层特征. 石油实验地质,2005,27(12):575-582. XIE Z W,XIE Y,WANG J,et al. The reservoir characteristics of Yanchang Formation in Fuxian Region,Ordos Basin. Petroleum Geology & Experiment,2005,27(12):575-582.
[10] 李凤杰,王多云,徐旭辉. 鄂尔多斯盆地陇东地区三叠系延长 组储层特征及影响因素分析. 石油实验地质,2005,27(4): 365-370. LI F J,WANG D Y,XU X H. The influential factors and characteristics of TriassicYanchang Formation reservoir in Longdong Area,Ordos Basin. Petroleum Geology & Experiment,2005,27 (4):365-370.
[11] 郑荣才,耿威,周刚,等. 鄂尔多斯盆地白豹地区长6 砂岩成岩 作用与成岩相研究.岩性油气藏,2007,19(2):1-8. ZHENG R C,GENG W,ZHOU G,et al. Diagenesis and diagenetic facies of Chang 6 sandstone of Yanchang Formation in Baibao area,Ordos Basin. Lithologic Reservoirs,2007,19(2): 1-8.
[12] 朱平,黄思静,李德敏,等. 黏土矿物绿泥石对碎屑储集岩孔 隙的保护. 成都理工大学学报(自然科学版),2004,31(2): 153-156. ZHU P,HUANG S J,LI DM,et al. Effect and protection of chlorite on clastic reservoir rocks. Journal of Chengdu University of Technology(Science & Technology Edition),2004,31(2):153- 156.
[13] 李斌,孟自芳,李相博,等. 靖安油田上三叠统长6 储层成岩 作用研究.沉积学报,2005,23(4):574-583. LI B,MENG Z F,LI X B,et al. Diagenetic characteristics of the Chang 6 oil- bearing interval of the Upper Triassic in the Jing'an Oilfield,Ordos Basin.Acta Sedimentologica Sinica,2005, 23(4):574-583.
[14] 王琪,禚喜准,陈国俊,等. 鄂尔多斯西部长6 砂岩成岩演化 与优质储层.石油学报,2005,26(5):17-23. WANG Q,ZHUO X Z,CHEN G J,et al. Diagenetic evolution and high quality reservoir in Chang 6 sandstone in the Western Ordos Basin. Acta Petrolei Sinica,2005,26(5):17-23.
[15] 李春玉,谢渊,刘绍光,等. 陕北富县延长组特低孔渗砂岩储 层控制因素分析. 成都理工大学学报(自然科学版),2002,29 (3):285-289. LI C Y,XIE Y,LIU S G,et al. Factors controlling the very low porosity and permeability sandstone reservoir of the Yanchang Formation in Fuxian Area,North Shaanxi. Journal of Chengdu University of Technology(Science &Technology Edition),2002, 29(3):285-289.
[16] 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.岩性油气藏,2007,19(4):45-50. WEI Q L,ZHENG R C,XIAO L,et al. Influencing factors and characteristics of Chang 6 reservoir in Wuqi Area,Ordos Basin. Lithologic Reservoirs,2007,19(4):45-50.
[17] 陈朝兵,朱玉双,陈新晶,等. 鄂尔多斯盆地姬塬地区延长组 长82储层沉积成岩作用. 石油与天然气地质,2013,34(5): 685-693. CHEN Z B,ZHU Y S,CHEN X J,et al. Sedimentation and diagenesis of Chang 82 reservoir in the Yanchang Formation in Jiyuan Region,Ordos Basin. Oil &Gas Geology,2013,34(5):685-693.
[18] 纪友亮,赵澄林,刘孟慧,等. 东濮凹陷沙河街组碎屑岩成岩 作用. 石油与天然气地质,1995,16(2):148-154. JI Y L,ZHAO C L,LIU M H,et al. Diagenesis of clastic rocks in Shahejie Formation,Dongpu Depression.Oil&Gas Geology, 1995,16(2):148-154.
[19] 杨仁超,樊爱萍,韩作振,等. 马家山-小涧子油田砂岩成岩作 用及其对储层的影响.中国地质,2007,34(2):283-288. YANG R C,FAN A P,HAN Z Z,et al. Diagenesis of sandstone in the Majiashan-Xiaojianzi oilfield,Ordos Basin and its effecton reservoirs. Geology in China,2007,34(2):283-288.
[1] 张培军, 谢明贤, 罗敏, 张良杰, 陈仁金, 张文起, 乐幸福, 雷明. 巨厚膏盐岩形变机制解析及其对油气成藏的影响——以阿姆河右岸东部阿盖雷地区侏罗系为例[J]. 岩性油气藏, 2024, 36(6): 36-44.
[2] 西智博, 廖建平, 高荣锦, 周晓龙, 雷文文. 辽河坳陷陈家断裂带北部构造演化解析及油气成藏[J]. 岩性油气藏, 2024, 36(3): 127-136.
[3] 贺勇, 邱欣卫, 雷永昌, 谢世文, 肖张波, 李敏. 珠江口盆地陆丰13东洼新生代构造演化与油气成藏特征[J]. 岩性油气藏, 2023, 35(1): 74-82.
[4] 余海波. 东濮凹陷构造特征及古生界有利勘探区带评价[J]. 岩性油气藏, 2022, 34(6): 72-79.
[5] 阴钰毅, 姚志纯, 郭小波, 王乐立, 陈思谦, 余小雷, 岑向阳. 鄂尔多斯盆地西缘二叠系隐伏构造特征及勘探意义[J]. 岩性油气藏, 2022, 34(4): 79-88.
[6] 易志凤, 张尚锋, 王雅宁, 徐恩泽, 赵韶华, 王玉瑶. 差异曲率下的曲流河点坝砂体定量表征——以黄河源区白河现代沉积为例[J]. 岩性油气藏, 2022, 34(1): 34-42.
[7] 马文辛, 欧阳诚, 廖波勇, 徐邱康, 陈仁金, 王欣, 夏慧萍, 张婷. 阿姆河盆地东部牛津阶微生物灰岩储层特征及成因[J]. 岩性油气藏, 2021, 33(5): 59-69.
[8] 覃阳亮, 何幼斌, 蔡俊, 李华, 张灿, 刘建宁. 东非海岸Davie构造带的构造演化特征及其成因机制[J]. 岩性油气藏, 2021, 33(2): 104-115.
[9] 胡贺伟, 李慧勇, 许鹏, 陶莉, 华晓莉. 断裂密集带油气差异富集主控因素探讨——以歧口凹陷歧南断阶带为例[J]. 岩性油气藏, 2020, 32(5): 34-45.
[10] 朱珍君, 黄光明, 邱津, 刘康宁, 李琦, 胡俊杰. 哈萨克斯坦斋桑盆地构造特征及其对油气成藏的影响[J]. 岩性油气藏, 2020, 32(4): 23-35.
[11] 尹帅, 赵威, 范子宜. 沁水盆地南部地区古构造恢复及其油气意义[J]. 岩性油气藏, 2017, 29(6): 43-50.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 黄思静,黄培培,王庆东,刘昊年,吴 萌,邹明亮. 胶结作用在深埋藏砂岩孔隙保存中的意义[J]. 岩性油气藏, 2007, 19(3): 7 -13 .
[2] 刘震, 陈艳鹏, 赵阳,, 郝奇, 许晓明, 常迈. 陆相断陷盆地油气藏形成控制因素及分布规律概述[J]. 岩性油气藏, 2007, 19(2): 121 -127 .
[3] 丁超,郭兰,闫继福. 子长油田安定地区延长组长6 油层成藏条件分析[J]. 岩性油气藏, 2009, 21(1): 46 -50 .
[4] 李彦山,张占松,张超谟,陈鹏. 应用压汞资料对长庆地区长6 段储层进行分类研究[J]. 岩性油气藏, 2009, 21(2): 91 -93 .
[5] 罗 鹏,李国蓉,施泽进,周大志,汤鸿伟,张德明. 川东南地区茅口组层序地层及沉积相浅析[J]. 岩性油气藏, 2010, 22(2): 74 -78 .
[6] 左国平,屠小龙,夏九峰. 苏北探区火山岩油气藏类型研究[J]. 岩性油气藏, 2012, 24(2): 37 -41 .
[7] 王飞宇. 提高热采水平井动用程度的方法与应用[J]. 岩性油气藏, 2010, 22(Z1): 100 -103 .
[8] 袁云峰,才业,樊佐春,姜懿洋,秦启荣,蒋庆平. 准噶尔盆地红车断裂带石炭系火山岩储层裂缝特征[J]. 岩性油气藏, 2011, 23(1): 47 -51 .
[9] 袁剑英,付锁堂,曹正林,阎存凤,张水昌,马达德. 柴达木盆地高原复合油气系统多源生烃和复式成藏[J]. 岩性油气藏, 2011, 23(3): 7 -14 .
[10] 石战战,贺振华,文晓涛,唐湘蓉. 一种基于EMD 和GHT 的储层识别方法[J]. 岩性油气藏, 2011, 23(3): 102 -105 .