岩性油气藏 ›› 2019, Vol. 31 ›› Issue (6): 26–35.doi: 10.12108/yxyqc.20190603

• 油气地质 • 上一篇    下一篇

鄂尔多斯盆地陇东地区长4+5油层组沉积相展布特征

郑庆华1, 刘乔2, 梁秀玲2, 张建魁2, 张建娜2, 刘涛2   

  1. 1. 榆林学院 化学与化工学院, 陕西 榆林 719000;
    2. 中国石油长庆油田分公司 第五采油厂, 西安 710200
  • 收稿日期:2019-07-14 修回日期:2019-08-21 出版日期:2019-11-21 发布日期:2019-09-28
  • 作者简介:郑庆华(1980-),男,博士,讲师,主要从事油气储层地质学方面的研究与教学工作。地址:(719000)陕西省榆林市榆阳区崇文路51号榆林学院。Email:272594012@qq.com。
  • 基金资助:
    榆林学院博士科研启动基金"鄂尔多斯盆地长7高伽马砂岩研究"（编号：18GK28）、榆林学院横向项目"靖边东部地区长2储层综合评价及有利目标优选"（编号：2018HX52）和中国石油天然气股份有限公司长庆油田分公司油藏评价处横向项目"陇东地区长4+5油藏富集规律及勘探潜力分析"（编号：2015-2-1）联合资助

Sedimentary facies distribution characteristics of Chang 4+5 reservoir in Longdong area,Ordos Basin

ZHENG Qinghua1, LIU Qiao2, LIANG Xiuling2, ZHANG Jiankui2, ZHANG Jianna2, LIU Tao2   

  1. 1. School of Chemistry & Chemical Engineering, Yulin University, Yulin 719000, Shaanxi, China;
    2. No.5 Oil Production Plant, PetroChina Changqing Oilfield Company, Xi'an 710201, China
  • Received:2019-07-14 Revised:2019-08-21 Online:2019-11-21 Published:2019-09-28

PDF (PC)

287

摘要： 为研究鄂尔多斯盆地陇东地区长4+5油层组的沉积相展布特征，开展了野外露头剖面和钻井取心的岩心观察、铸体薄片鉴定、重矿物测试、测井岩电关系分析等工作。结果表明：①陇东地区长4+5油层组的沉积主要受东北、西南和南部共三大物源区控制；②研究区主要发育3类沉积相，东北部为曲流河三角洲相，西南部和南部均为辫状河三角洲相，中部为湖泊相，可进一步将其划分为5类亚相和10类微相；③研究区长4+5油层组主要表现为"湖退-砂进"的沉积特征，长4+51小层沉积时相对于长4+52小层沉积时的湖盆面积较小，砂体规模更大；④相对于西南部和南部，东北部的物源供给更充分，多支水下分流河道汇聚于此，叠置连片分布的厚层砂体更为发育。该研究成果展示了陇东地区长4+5油层组的勘探潜力，可为下一步精细勘探提供借鉴。

关键词: 沉积相, 砂体展布, 物源, 长4+5, 陇东地区, 鄂尔多斯盆地

Abstract: In order to study the distribution characteristics of sedimentary facies of Chang 4+5 reservoir in Longdong area of Ordos Basin,core observation,casting thin section identification,heavy mineral testing and log rockelectricity relationship analysis were carried out in outcrop profile and drilling coring. The results show that:(1)The deposits of Chang 4+5 reservoir in Longdong area are mainly controlled by three provenance areas in northeast, southwest and south;(2)Three types of sedimentary facies are mainly developed in the study area,inclu-ding meandering river delta facies in the northeast,braided river delta facies in the southwest and south,and lacu-strine facies in the central region,which can be further divided into five types of subfacies and 10 types of microfacies; (3)The Chang 4+5 reservoir in the study area is mainly characterized by "lake retreat-sand progradation". The lake basin area of Chang 4+51 sublayer is smaller than that of Chang 4+52 sublayer,but the scale of sand body is larger;(4)Compared with the southwest and south,the northeast has a more abundant supply of provenances and many underwater distributary channels converge. As a result,thick sand bodies with overlapping and continuous distribution are more developed. The research results show the exploration potential of Chang 4+5 reser-voir in Longdong area,which can provide reference for further fine exploration.

Key words: sedimentary facies, sand body distribution, provenance, Chang 4+5, Longdong area, Ordos Basin

中图分类号: 

  • TE121.3
[1] 李道品. 低渗透油田高效开发决策论. 北京:石油工业出版, 2003. LI D P. Effective development technique of low permeability oilfield. Beijing:Petroleum Industry Press,2003.
[2] 杨伟伟,柳广弟,刘显阳,等. 鄂尔多斯盆地陇东地区延长组低渗透砂岩油藏成藏机理与成藏模式. 地学前缘,2013,20(2):132-139. YANG W W,LIU G D,LIU X Y,et al. The accumulation mechanism and accumulation models of oil in low permeability reservoir of Yanchang Formation in Longdong area,Ordos Basin. Earth Science Frontiers,2013,20(2):132-139.
[3] 杨俊杰. 鄂尔多斯盆地构造演化与油气分布规律. 北京:石油工业出版社,2002. YANG J J. Tectonic evolution and oil-gas reservoirs distribution in Ordos Basin. Beijing:Petroleum Industry Press,2002.
[4] 杨华,刘显阳,张才利,等. 鄂尔多斯盆地三叠系延长组低渗透岩性油藏主控因素及其分布规律. 岩性油气藏,2007,19(3):1-6. YANG H,LIU X Y,ZHANG C L,et al. The main controlling factors and distribution of low permeability lithologic reservoirs of Triassic Yanchang Formation in Ordos Basin. Lithologic Reservoirs,2007,19(3):1-6.
[5] 杨华. 鄂尔多斯盆地三叠系延长组沉积体系及含油性研究. 成都:成都理工大学,2004. YANG H. Deposition system and oil accumulation research of Yanchang Formation in Triassic,Ordos Basin. Chengdu:Chengdu University of Technology,2004.
[6] 杨华,张文正,刘显阳,等. 优质烃源岩在鄂尔多斯低渗透富油盆地形成中的关键作用. 地球科学与环境学报,2013,35(4):1-9. YANG H,ZHANG W Z,LIU X Y,et al. Key role of high-quality source rocks on the formation of low-permeability oil-rich reservoirs in Ordos Basin. Journal of Earth Sciences and Environment,2013,35(4):1-9.
[7] 闫海龙. 南梁-华池地区三叠系(长3-长4+5油层组)沉积微相及有利区带预测. 西安:西北大学,2005. YAN H L. Study on sedimentary facies and advantageous distribution of oil in the Chang 34+5 oil pools of Triassic Yanhang Formation in Nanliang-Huachi area. Xi'an:Northwest University, 2005.
[8] 于峰丹. 南梁油田华64区延9及长4+5沉积微相研究. 西安:长安大学,2008. YU D F. Study on the deposit micro-facies of Yang 9 and Chang 4+5 in Hua 64 borefield of Nanliang Oilfield. Xi'an:Chang'an University,2008.
[9] 关成尧,赵国春,李晓锋,等.白豹油田三叠系长3,长4+5沉沉积微相研究. 新疆地质,2009,27(1):62-65. GUAN C Y,ZHAO G C,LI X F,et al. Sedimentary microfacies study of Chang 3,Chang 4+5 of Triassic Formation in Baibao Oilfield. Xinjiang Geology,2009,27(1):62-65.
[10] 张慧元. 华池地区三叠系延长组长3-长4+5油层组沉积相研究. 西安:西北大学,2010. ZHANG H Y. Study on the sedimentary facies of the Chang 4+5 and 3 of Triassic Yanchang Formation in Huachi area. Xi'an:Northwest University,2010.
[11] 张慧元,李文厚,张慧军,等. 鄂尔多斯盆地华池地区三叠系延长组长4+5油层组沉积相研究. 特种油气藏,2010,17(2):27-30. ZHANG H Y,LI W H,ZHANG H J,et al. Study on sedimentary facies of Chang 4+5 oil unit in Triassic Yanchang Formation in Huachi area of Ordos Basin. Special Oil and Gas Reservoirs, 2010,17(2):27-30.
[12] 刘正伟. 南梁西区三叠系长4+5油层组沉积体系研究. 西安:西北大学,2011. LIU Z W. Depositional system of Chang 4+5 oil formation of Triassic Yanchang Formation of the western Nanliang area. Xi'an:Northwest University,2011.
[13] 何右安,郭路,高文冰. 吴堡地区南梁油田长4+5油层组沉积微相研究. 石油天然气学报,2014,36(5):15-19. HE Y A,GUO L,GAO W B. Sedimentary microfacies of Chang 4+5 reservoir of Nanliang oilfield in Wubu area. Journal of Oil and Gas Technology,2014,36(5):15-19.
[14] 周瑶. 镇北-环江地区长4+5段沉积相特征及有利区带预测.成都:成都理工大学,2015. ZHOU Y. The sedimentary facies characteristics and favorable block prediction in Chang 4+5 member of Yanchang Formation,Zhenbei-Huanjiang area. Chengdu:Chengdu University of Technology,2015.
[15] 朱童. 镇北-环江地区长4+5油层组砂体分布、成因及有利区预测. 成都:成都理工大学,2015. ZHU T. The distribution,origin,and favorable area prediction of Chang 4+5 formation in the region of Zhenbei-Huanjiang. Chengdu:Chengdu University of Technology,2015.
[16] 李金超. 鄂尔多斯盆地长4+5油层组沉积相特征及层序演化. 西安:长安大学,2005. LI J C. The characteristics of sedimentary facies and evolution of sequence stratigraphy of Chang 4+5 oil-bearing bed in Triassic Yanchang Formation in Ordos Basin. Xi'an:Chang'an University, 2005.
[17] 李文厚,庞军刚,曹红霞,等. 鄂尔多斯盆地晚三叠世延长期沉积体系及岩相古地理演化. 西北大学学报(自然科学版), 2009,39(3):501-506. LI W H,PANG J G,CAO H X,et al. Depositional system and paleogeographic evolution of the Late Triassic Yanchang stage in Ordos Basin. Journal of Northwest University(Natural Science Edition),2009,39(3):501-506.
[18] 朱筱敏,邓秀芹,刘自亮,等. 大型坳陷湖盆浅水辫状河三角洲沉积特征及模式:以鄂尔多斯盆地陇东地区延长组为例. 地学前缘,2013,20(2):19-28. ZHU X M,DENG X Q,LIU Z L,et al. Sedimentary characteristics and model of shallow braided delta in large-scale lacustrine:an example from Triassic Yanchang Formation in Ordos Basin. Earth Science Frontiers,2013,20(2):19-28.
[19] 赵红格,刘池洋.物源分析方法及研究进展.沉积学报,2003, 21(3):409-415. ZHAO H G,LIU C Y. Approaches and prospects of provenance analysis. Acta Sedimentologica Sinica,2003,21(3):409-415.
[20] 魏斌,魏红红,陈全红,等. 鄂尔多斯盆地上三叠统延长组物源分析. 西北大学学报(自然科学版),2003,33(4):447-450. WEI B,WEI H H,CHEN Q H,et al. Sediment provenance analysis of Yanchang Formation in Ordos Basin. Journal of Northwest University(Natural Science Edition),2003,33(4):447-450.
[21] 王若谷. 鄂尔多斯盆地三叠系延长组长6-长7油层组沉积体系研究. 西安:西北大学,2010. WANG R G. Depositional system of Chang 6& 7 oil formation of the Triassic Yanchang Formation in Ordos Basin. Xi'an:Northwest University,2010.
[22] 张春宇,赵越,刘金,等. 柴达木盆地北缘牦牛山组物源分析及其构造意义. 地质学报,2019,93(3):712-723. ZHANG C Y,ZHAO Y,LIU J,et al. Provenance analysis of the Maoniushan Formation in the north Qaidam Basin and its tectonic significance. Acta Geologica Sinica,2019,93(3):712723.
[23] 付金华,邓秀芹,张晓磊,等. 鄂尔多斯盆地三叠系延长组深水砂岩与致密油的关系. 古地理学报,2013,15(5):624-634. FU J H,DENG X Q,ZHANG X L,et al. Relationship between deepwater sandstone and tight oil of the Triassic Yanchang Formation in Ordos Basin. Journal of Palaeogeography,2013,15(5):624-634.
[24] SHANMUGAM G. Basin-floor fans in the North Sea:Sequence stratigraphic models vs. sedimentary facies. AAPC Bulletin, 1995,79(4):477-512.
[25] SHANMUGAM G. 50 years of the turbidite paradigm(1950-1990 s):Deep-water processes and facies models:a critical perspective. Marine and Petroleum Geology,2000,17(2):285342.
[26] TALLING P J,MASSON D G,SUMMER E J,et al. Subaqueous sediment density flows:Depositional processes and deposit types. Sedimentology,2012,59(7):1937-2003.
[27] 付金华,罗顺社,牛小兵,等. 鄂尔多斯盆地陇东地区长7段沟道型重力流沉积特征研究. 矿物岩石地球化学通报, 2015,34(1):29-37. FU J H,LUO S S,NIU X B,et al. Sedimentary characteristics of channel type gravity flow of the member 7 of Yanchang Formation in the Longdong area,Ordos Basin. Bulletin of Mineralogy,Petrology and Geochemistry,2015,34(1):29-37.
[28] SHANMUGAM G. High-density turbidity currents:are they sandy debris flows. Journal of Sedimentary Research,1996,66(1):210.
[29] SHANMUGAM G. The Bouma sequence and the turbidite mind set. Earth Science Reviews,1997,42(4):201-229.
[30] 杨华,窦伟坦,刘显阳,等. 鄂尔多斯盆地三叠系延长组长7沉积相分析. 沉积学报,2010,28(2):254-263. YANG H,DOU W T,LIU X Y,et al. Analysis on sedimentary facies of Chang 7 member in Yanchang Formation of Triassic in Ordos Basin. Acta Sedimentologica Sinica,2010,28(2):254263.
[31] 张廷山,何映颉,伍坤宇,等. 筠连地区上二叠统宣威组沉积相及聚煤控制因素. 岩性油气藏,2017,29(1):1-10. ZHANG T S,HE Y J,WU K Y,et al. Sedimentary facies and controlling factors of coal accumulation of the Upper Permian Xuanwei Formation in Junlian area. Lithologic Reservoirs, 2017,29(1):1-10.
[32] 林森虎,汪梦诗,袁选俊. 大型坳陷湖盆定量化沉积相编图新方法:以鄂尔多斯盆地中部长7油层组为例. 岩性油气藏, 2017,29(3):10-17. LIN S H,WANG M S,YUAN X J. A new quantitative method of sedimentary facies mapping of large lacustrine depression:a case from Chang 7 reservoir in central Ordos Basin. Lithologic Reservoirs,2017,29(3):10-17.
[1] 徐宁宁, 王永诗, 张守鹏, 邱隆伟, 张向津, 林茹. 鄂尔多斯盆地大牛地气田二叠系盒1段储层特征及成岩圈闭[J]. 岩性油气藏, 2021, 33(4): 52-62.
[2] 李志远, 杨仁超, 张吉, 王一, 杨特波, 董亮. 天然气扩散散失率定量评价——以苏里格气田苏X区块为例[J]. 岩性油气藏, 2021, 33(4): 76-84.
[3] 郑荣臣, 李宏涛, 史云清, 肖开华. 川东北元坝地区三叠系须三段沉积特征及成岩作用[J]. 岩性油气藏, 2021, 33(3): 13-26.
[4] 张汶, 吕世聪, 赵大林, 贾海松, 蔡越钎. 渤海湾盆地西南部古近系滩坝沉积特征及主控因素[J]. 岩性油气藏, 2021, 33(3): 85-94.
[5] 许飞. 考虑化学渗透压作用下页岩气储层压裂液的自发渗吸特征[J]. 岩性油气藏, 2021, 33(3): 145-152.
[6] 姚海鹏, 于东方, 李玲, 林海涛. 内蒙古地区典型煤储层吸附特征[J]. 岩性油气藏, 2021, 33(2): 1-8.
[7] 魏钦廉, 崔改霞, 刘美荣, 吕玉娟, 郭文杰. 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.
[8] 张晓辉, 张娟, 袁京素, 崔小丽, 毛振华. 鄂尔多斯盆地南梁-华池地区长81致密储层微观孔喉结构及其对渗流的影响[J]. 岩性油气藏, 2021, 33(2): 36-48.
[9] 严敏, 赵靖舟, 曹青, 吴和源, 黄延昭. 鄂尔多斯盆地临兴地区二叠系石盒子组储层特征[J]. 岩性油气藏, 2021, 33(2): 49-58.
[10] 周新平, 邓秀芹, 李士祥, 左静, 张文选, 李涛涛, 廖永乐. 鄂尔多斯盆地延长组下组合地层水特征及其油气地质意义[J]. 岩性油气藏, 2021, 33(1): 109-120.
[11] 高计县, 孙文举, 吴鹏, 段长江. 鄂尔多斯盆地东北缘神府区块上古生界致密砂岩成藏特征[J]. 岩性油气藏, 2021, 33(1): 121-130.
[12] 张闻亭, 龙礼文, 肖文华, 魏浩元, 李铁锋, 董震宇. 酒泉盆地青西凹陷窟窿山构造带下沟组沉积特征及储层预测[J]. 岩性油气藏, 2021, 33(1): 186-197.
[13] 曹江骏, 陈朝兵, 罗静兰, 王茜. 自生黏土矿物对深水致密砂岩储层微观非均质性的影响——以鄂尔多斯盆地西南部合水地区长6油层组为例[J]. 岩性油气藏, 2020, 32(6): 36-49.
[14] 何维领, 罗顺社, 李昱东, 吴悠, 吕奇奇, 席明利. 斜坡背景下沉积物变形构造时空展布规律——以鄂尔多斯盆地镇原地区长7油层组为例[J]. 岩性油气藏, 2020, 32(6): 62-72.
[15] 王朋, 孙灵辉, 王核, 李自安. 鄂尔多斯盆地吴起地区延长组长6储层特征及其控制因素[J]. 岩性油气藏, 2020, 32(5): 63-72.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 杨秋莲, 李爱琴, 孙燕妮, 崔攀峰. 超低渗储层分类方法探讨[J]. 岩性油气藏, 2007, 19(4): 51 -56 .
[2] 张杰, 赵玉华. 鄂尔多斯盆地三叠系延长组地震层序地层研究[J]. 岩性油气藏, 2007, 19(4): 71 -74 .
[3] 杨占龙, 张正刚, 陈启林, 郭精义,沙雪梅, 刘文粟. 利用地震信息评价陆相盆地岩性圈闭的关键点分析[J]. 岩性油气藏, 2007, 19(4): 57 -63 .
[4] 朱小燕, 李爱琴, 段晓晨, 田随良, 刘美荣. 镇北油田延长组长3 油层组精细地层划分与对比[J]. 岩性油气藏, 2007, 19(4): 82 -86 .
[5] 方朝合, 王义凤, 郑德温, 葛稚新. 苏北盆地溱潼凹陷古近系烃源岩显微组分分析[J]. 岩性油气藏, 2007, 19(4): 87 -90 .
[6] 韩春元，赵贤正，金凤鸣，王权，李先平，王素卿. 二连盆地地层岩性油藏“多元控砂—四元成藏—主元富集”与勘探实践（IV）——勘探实践[J]. 岩性油气藏, 2008, 20(1): 15 -20 .
[7] 戴朝成，郑荣才，文华国，张小兵. 辽东湾盆地旅大地区古近系层序—岩相古地理编图[J]. 岩性油气藏, 2008, 20(1): 39 -46 .
[8] 尹艳树，张尚峰，尹太举. 钟市油田潜江组含盐层系高分辨率层序地层格架及砂体分布规律[J]. 岩性油气藏, 2008, 20(1): 53 -58 .
[9] 石雪峰，杜海峰. 姬塬地区长3—长4+5油层组沉积相研究[J]. 岩性油气藏, 2008, 20(1): 59 -63 .
[10] 严世邦，胡望水，李瑞升，关键，李涛，聂晓红. 准噶尔盆地红车断裂带同生逆冲断裂特征[J]. 岩性油气藏, 2008, 20(1): 64 -68 .

陇ICP备17006252号
版权所有© 2018 中国石油集团西北地质研究所有限公司《岩性油气藏》编辑部

地址：甘肃省兰州市城关区雁儿湾路535号(陇ICP备17006252号)    电话：0931-8686158;8686058;8686288    邮箱：yxyqc@petrochina.com.cn

甘公网安备 62010202002827号

本系统由北京玛格泰克科技发展有限公司设计开发