岩性油气藏 ›› 2019, Vol. 31 ›› Issue (6): 54–66.doi: 10.12108/yxyqc.20190606

• 油气地质 • 上一篇    下一篇

准噶尔盆地乌夏地区中上二叠统碎屑岩成岩作用及次生孔隙演化

李佳思1,2,3, 付磊4, 张金龙4, 陈静4, 牛斌3,5, 张顺存1,   

  1. 1. 中国科学院西北生态环境资源研究院, 兰州 730000;
    2. 甘肃省油气资源研究重点实验室, 兰州 730000;
    3. 中国科学院大学, 北京 100049;
    4. 中国石油新疆油田分公司石西油田作业区, 新疆 克拉玛依 834000;
    5. 中国科学院青藏高原研究所/高寒生态学与生物多样性实验室, 北京 100101
  • 收稿日期:2019-01-11 修回日期:2019-05-13 出版日期:2019-11-21 发布日期:2019-09-28
  • 作者简介:李佳思(1993-),男,中国科学院在读硕士研究生,研究方向为储层沉积学。地址:(730000)甘肃省兰州市城关区东岗西路382号。Email:lijiasi1993@163.com。
  • 基金资助:
    国家自然科学基金"富火山岩岩屑砂砾岩储层中沸石类自生矿物的形成条件和溶蚀机理及其对储层物性的影响"（编号：41872145）和甘肃省重点实验室专项（编号：1309RTSA041）联合资助

Diagenesis and secondary pore evolution of Middle and Upper Permian clastic rocks in Wu-Xia area,Junggar Basin

LI Jiasi1,2,3, FU Lei4, ZHANG Jinlong4, CHEN Jing4, NIU Bin3,5, ZHANG Shuncun1,   

  1. 1. Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
    2. Key Laboratory of Petroleum Resources, Gansu Province, Lanzhou 730000, China;
    3. University of Chinese Academy of Sciences, Beijing 100049, China;
    4. Shixi Oilfield Operation District, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    5. Institute of Tibetan Plateau Research/Laboratory of Alpine Ecology and Biodiversity, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2019-01-11 Revised:2019-05-13 Online:2019-11-21 Published:2019-09-28

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摘要： 准噶尔盆地乌夏地区中上二叠统碎屑岩储层埋藏深，物性差，以次生孔隙为主，成岩作用是影响中深部储层次生孔隙发育的最主要因素。铸体薄片、扫描电镜、X射线衍射等微观研究表明乌夏地区中上二叠统储层碎屑岩成分及结构成熟度均较低，次生孔隙发育，下乌尔禾组和夏子街组的平均孔隙度分别为8.15%和7.85%，其中次生孔隙分别占下乌尔禾组和夏子街组总孔隙的77.18%和80.90%，孔隙增生量平均值分别为6.49%和4.74%。研究区碎屑岩储层主要处于中成岩阶段A-B期，成岩作用以压实作用、胶结作用及溶蚀作用为主，压实作用造成的孔隙度损失平均约为24.5%，胶结作用造成的孔隙度损失平均约为6.14%，溶蚀作用以长石和岩屑颗粒的溶蚀为主，其产生的孔隙增生量对下乌尔禾组和夏子街组的贡献率分别为47.62%和55.86%。研究区受大气水溶蚀、断裂带及有机酸溶蚀作用的影响，在纵向上形成3个次生孔隙发育带。次生孔隙发育带是研究区在低孔低渗条件下寻找相对有利储层的重要区带。

关键词: 碎屑岩, 成岩作用, 次生孔隙演化, 中上二叠统, 准噶尔盆地

Abstract: The Middle and Upper Permian clastic reservoirs in Wu-Xia area of Junggar Basin are deeply buried and poor in reservoir properties,mainly with secondary pores. Diagenesis is the most important factor affecting the development of secondary pores in middle-deep reservoirs. Based on casting thin section identification,scanning electron microscopy(SEM),X-ray diffraction analysis method with logging and mud logging data,the diagenesis and secondary pore evolution of the Middle and Upper Permian clastic rocks in Wu-Xia area were studied. The results show that the reservoir compositional maturity and textural maturity were low and the most pores were secondary pores. The average porosity of lower Urho Formation and Xiazijie Formation was 8.15% and 7.85% respectively,secondary pores account for 77.18% and 80.90% respectively,and the amount of hyperplasia of pores was 6.49% and 4.74% respectively. The clastic reservoir in the study area was mainly at the A-B stage of the middle diagenetic stage,and the diagenesis was dominated by compaction,cementation and dissolution. The degree of porosity loss caused by compaction and cementation was 24.5% and 6.14% respectively. Dissolution was the main cause of secondary pores and the dissolution of feldspar and debris particles contributed the most to secondary pore growth. Lower Urho Formation and Xiazijie Formation have the rate of 47.62% and 55.86% respectively. Affected by atmospheric water dissolution,fault zone and dissolution of organic acids,there are three secondary pore development zones vertically developed in the reservoir of the study area. The secondary pore development zones are important zones for finding relatively favorable reservoirs under low porosity and low permeability conditions.

Key words: clastic rocks, diagenesis, secondary pore evolution, Middle and Upper Permian, Junggar Basin

中图分类号: 

  • TE122.2
[1] 雷德文,陈刚强,刘海磊,等.准噶尔盆地玛湖凹陷大油(气)区形成条件与勘探方向研究.地质学报,2017,91(7):1604-1619. LEI D W,CHEN G Q,LIU H L,et al. Study on the forming conditions ang exploration fields of the Mahu giant oil(gas) province,Junggar Basin.Acta Geologica Sinica,2017,91(7):1604-1619.
[2] WORDEN R H,BURLEY S D. Sandstone diagenesis:The evolution of sand to stone//BURLEY S D,WORDEN R H. Sandstone diagenesis:Recent and ancient. Malden:Blackwell Publishing Inc.,2009:1-44.
[3] MORAD S,AL-RAMADAN K,KETZER J M,et al. The impact of diagenesis on the heterogeneity of sandstone reservoirs:a review of the role of depositional facies and sequence stratigraphy. AAPG Bulletin,2010,94(8):1267-1309.
[4] TAYLOR T R,GILES M R,HATHON L A,et al. Sandstone diagenesis and reservoir quality prediction:Models,myths,and reality.AAPG Bulletin,2010,94(8):1093-1132.
[5] 王艳忠,操应长,葸克来.次生孔隙发育带的概念及石油地质意义新认识.吉林大学学报(地球科学版),2013,43(3):659-668. WANG Y Z,CAO Y C,XI K L. New view on the concept of secondary pore developing zones and its significance of petroleum geology. Journal of Jilin University(Earth Science Edition),2013,43(3):659-668.
[6] 罗挺.准噶尔盆地西北缘乌尔禾-夏子街地区侏罗系沉积相演化.乌鲁木齐:新疆大学,2015. LUO T. Jurassic sedimentary facies evolution in the WuerheXiazijie area on the northwestern margin of the Junggar Basin. Urumqi:Xinjiang University,2015.
[7] 姜文超.准噶尔盆地乌夏地区三叠系中下统沉积特征研究. 长春:吉林大学,2015. JIANG W C. Sedimentary characteristics of the Middle and Lower Triassic in the Wu-Xia area,Junggar Basin. Changchun:Jilin University,2015.
[8] 鄢继华,崔永北,陈世悦,等.准噶尔盆地乌夏地区二叠系沉积特征及有利储集层.新疆石油地质,2009,30(3):304-306. YAN J H,CUI Y B,CHEN S Y,et al. Sedimentary features and favorable reservoirs of Permian in Wu-Xia area of Junggar Basin. Xinjiang Petroleum Geology,2009,30(3):304-306.
[9] 余杰.准噶尔盆地西北缘乌夏地区测井沉积微相及层序地层分析.青岛:中国石油大学(华东),2007. YU J. Analysis of logging sedimentary microfacies and sequence stratigraphy in Wu-Xia area,northwestern margin of Junggar Basin. Qingdao:China University of Petroleum(East China), 2007.
[10] 张鹏,陈世悦.准噶尔盆地乌夏地区侏罗系八道湾组储层特征.西部探矿工程,2007(3):76-79. ZHANG P,CHEN S Y. Reservoir characteristics of Jurassic Badaowan Formation at Wuxia area in Junggar Basin. West-China Exploration Engineering,2007(3):76-79.
[11] 徐怀宝,蔡正旗,丁超,等.乌夏地区油气成藏主控因素分析. 西部探矿工程,2011(2):108-111. XU H B,CAI Z Q,DING C,et al. Analysis of main controlling factors of oil and gas accumulation in Wu-Xia area. West-China Exploration Engineering,2011(2):108-111.
[12] 牛海青,陈世悦,张鹏,等.准噶尔盆地乌夏地区二叠系碎屑岩储层成岩作用与孔隙演化.中南大学学报(自然科学版), 2010,41(2):749-758. NIU H Q,CHEN S Y,ZHANG P,et al. Diagenesis and porosity evolution of Permian reservoir in Wu-Xia area,Junggar Basin. Journal of Central South University(Science and Technology), 2010,41(2):749-758.
[13] 张顺存,刘振宇,刘巍,等.准噶尔盆地西北缘克-百断裂下盘二叠系砂砾岩储层成岩相研究.岩性油气藏,2010,22(4):43-51. ZHANG S C,LIU Z Y,LIU W,et al. Diagenesis facies of Permian sandy conglomerate reservoir in footwall of Kebai Fault in northwestern margin of Junggar Basin. Lithologic Reservoirs,2010,22(4):43-51.
[14] 崔殿.准噶尔盆地西北缘克夏断裂带胶结封闭作用研究.岩性油气藏,2015,27(6):48-54. CUI D. Cemented sealing in Kexia fault zone in northwestern margin of Junggar Basin.Lithologic Reservoirs,2015,27(6):48-54.
[15] 牛海青,陈世悦,张鹏,等.准噶尔盆地乌夏地区二叠系储集层特征及影响因素分析.古地理学报,2009,11(4):425-434. NIU H Q,CHEN S Y,ZHANG P,et al. Analysis of the Permian reservoir characteristics and controlling factors in Wuxia area, Junggar Basin. Journal of Palaeogeography,2009,11(4):425434.
[16] 张鹏.准噶尔盆地西北缘乌夏地区成岩作用与储层评价.青岛:中国石油大学(华东),2007. ZHANG P. Diagenesis and reservoir evaluation of Wu-Xia area in the northwestern margin of Junggar Basin. Qingdao:China University of Petroleum,2007.
[17] 曲江秀,邱贻博,时振峰,等.准噶尔盆地西北缘乌夏断裂带断裂活动与油气运聚.新疆石油地质,2007,28(4):403-405. QU J X,QIU Y B,SHI Z F,et al. Fault activities and hydrocarbon accumulation in Wu-Xia fault belt in northwestern margin of Junggar Basin. Xinjiang Petroleum Geology,2007,28(4):403-405.
[18] 冯建伟,戴俊生,葛盛权.准噶尔盆地乌夏断裂带构造演化及油气聚集.中国石油大学学报(自然科学版),2008,32(3):23-29. FENG J W,DAI J S,GE S Q. Structural evolution and poolforming in Wuxia fault belt of Junggar Basin. Journal of China University of Petroleum(Edition of Natural Science),2008,32(3):23-29.
[19] 朱世发,朱筱敏,陶文芳,等.准噶尔盆地乌夏地区二叠系风城组云质岩类成因研究.高校地质学报,2013,19(1):38-45. ZHU S F,ZHU X M,TAO W F,et al. Origin of dolomitic reservoir rock in the Permian Fengcheng Formation in Wu-Xia area of the Junggar Basin. Geological Journal of China Universities, 2013,19(1):38-45.
[20] 夏雨,陈世悦,杨俊生.准噶尔盆地乌夏地区二叠系层序地层特征研究.断块油气田,2008,15(1):18-21. XIA Y,CHEN S Y,YANG J S. Sequence stratigraphy characteristics of Permian in Wuxia area,Junggar Basin. Fault-Block Oil & Gas Field,2008,15(1):18-21.
[21] 冯有良,胡素云,李建忠,等.准噶尔盆地西北缘同沉积构造坡折对层序建造和岩性油气藏富集带的控制.岩性油气藏, 2018,30(4):14-25. FENG Y L,HU S Y,LI J Z,et al. Controls of syndepositional structural slope-break zones on sequence architecture and enrichment zones of lithologic reservoirs in northwestern margin of Junggar Basin. Lithologic Reservoirs,2018,30(4):14-25.
[22] 李振华,邱隆伟,师政,等.准噶尔盆地中拐地区佳二段沸石类矿物成岩作用及其对油气成藏的意义.中国石油大学学报(自然科学版),2014,38(1):1-7. LI Z H,QIU L W,SHI Z,et al. Diagenesis of zeolite minerals and its significance for hydrocarbon accumulation in the second member of Jiamuhe Formation of Zhongguai area,Junggar Basin. Journal of China University of Petroleum(Edition of Natural Science),2014,38(1):1-7.
[23] 许多年,潘建国,陈永波,等.地震储层学在准噶尔盆地火山岩油气勘探中的应用:以乌夏地区为例.岩性油气藏,2010, 22(3):5-8. XU D N,PAN J G,CHEN Y B,et al. Application of seismic reservoir to volcanic reservoir exploration in Wuxia area of Junggar Basin. Lithologic Reservoirs,2010,22(3):5-8.
[24] 朱世发,朱筱敏,王一博,等.准噶尔盆地西北缘克百地区三叠系储层溶蚀作用特征及孔隙演化.沉积学报,2010,28(3):547-555. ZHU S F,ZHU X M,WANG Y B,et al. Dissolution characteristics and pore evolution of Triassic reservoir in Ke-Bai area, Northwestern Margin of Junggar Basin. Acta Sedimentologica Sinica,2010,28(3):547-555.
[25] 郭沫贞,徐洋,寿建峰,等.准噶尔盆地西北缘二叠系碎屑岩次生孔隙发育控制因素.沉积学报,2017,35(2):330-342. GUO M Z,XU Y,SHOU J F,et al. Controlling factors of secondary pore development and petroleum exploration significance of Permian clastic rocks in northwest margin of Junggar Basin. Acta Sedimentologica Sinica,2017,35(2):330-342.
[26] 李汶国,张晓鹏,钟玉梅.长石砂岩次生溶孔的形成机理.石油与天然气地质,2005,26(2):220-223. LI W G,ZHANG X P,ZHONG Y M. Formation mechanism of secondary dissolved pores in arcose. Oil & Gas Geology,2005, 26(2):220-223.
[27] 邱楠生,王绪龙,杨海波,等.准噶尔盆地地温分布特征.地质科学,2001,36(3):350-358. QIU N S,WANG X L,YANG H B,et al. The characteristics of temperature distribution in the Junggar Basin. Chinese Journal of Geology,2001,36(3):350-358.
[28] 刘再振,刘玉明,李洋冰,等.鄂尔多斯盆地神府地区太原组致密砂岩储层特征及成岩演化.岩性油气藏,2017,29(6):51-59. LIU Z Z,LIU Y M,LI Y B,et al. Tight sandstone reservoir characteristics and diagenesis evolution of Taiyuan Formation in Shenmu-Fugu area,Ordos Basin. Lithologic Reservoirs,2017, 29(6):51-59.
[29] 吴陈冰洁,朱筱敏,魏巍,等.查干凹陷下白垩统巴二段储层特征及孔隙演化.岩性油气藏,2017,29(1):71-80. WU-CHEN B J,ZHU X M,WEI W,et al. Reservoir characteristics and pore evolution of the second member of the Lower Cretaceous Bayingebi Formation in Chagan Depression. Lithologic Reservoirs,2017,29(1):71-80.
[30] 谭开俊,许多年,尹路,等.准噶尔盆地乌夏地区三叠系成岩相定量研究.岩性油气藏,2011,23(6):24-29. TAN K J,XU D N,YIN L,et al. Quantitative study on Triassic diagenetic facies in Wuxia area,Junggar Basin. Lithologic Reservoirs,2011,23(6):24-29.
[31] 王琪,马东旭,余芳,等.鄂尔多斯盆地临兴地区下石盒子组不同粒级砂岩成岩演化及孔隙定量研究.沉积学报,2017,35(1):163-172. WANG Q,MA D X,YU F,et al. The diagenetic evolution and quantitative research of porosity in different grain size sandstones of the Lower Shihezi Formation in Linxing area,Ordos Basin. Acta Sedimentologica Sinica,2017,35(1):163-172.
[32] 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.岩性油气藏,2019, 31(2):56-65. HUYAN Y Y,JIANG F J,PANG X Q,et al. Diagenesis and porosity evolution of Permian tight reservoirs in Kangning area, eastern margin of Ordos Basin. Lithologic Reservoirs,2019,31(2):56-65.
[33] 李亚哲,王力宝,郭华军,等. 基于地震波形指示反演的砂砾岩储层预测:以中拐-玛南地区上乌尔禾组为例. 岩性油气藏,2019,31(2):134-142. LI Y Z,WANG L B,GUO H J,et al. Prediction of glutenite reservoir based on seismic waveform indicative inversion:a casestudy of the upper Wuerhe Formation in Zhongguai-Manan area. Lithologic Reservoirs,2019,31(2):134-142.
[34] 何周,史基安,唐勇,等.准噶尔盆地西北缘二叠系碎屑岩储层成岩相与成岩演化研究.沉积学报,2011,29(6):1069-1078. HE Z,SHI J A,TANG Y,et al. Characteristics of diagenesis and diageneticFacies of Permian clastic reservoir in Northwest Margin of Junggar Basin. Acta Sedimentologica Sinica,2011, 29(6):1069-1078.
[35] 梅华平,陈玉良,龚福华,等.准噶尔盆地西北缘二叠系下乌尔禾组储层控制因素分析.西安科技大学学报,2014,34(4):420-425. MEI H P,CHEN Y L,GONG F H,et al. Analysis of reservoir control factors for Xiawuerhe formation of Permian in northwestern margin of Junggar Basin. Journal of Xi'an University of Science and Technology,2014,34(4):420-425.
[36] 靳军,康逊,胡文瑄,等.准噶尔盆地玛湖凹陷西斜坡百口泉组砂砾岩储层成岩作用及对储集性能的影响.石油与天然气地质,2017,38(2):323-333. JIN J,KANG X,HU W X,et al. Diagenesis and its influence on coarse clastic reservoirs in the Baikouquan Formation of western slope of the Mahu Depression,Junngar Basin. Oil & Gas Geology,2017,38(2):323-333.
[37] 王艳忠.东营凹陷北带古近系次生孔隙发育带成因机制及演化模式.青岛:中国石油大学(华东),2010. WANG Y Z. The genetic mechanism and evolution model of the secondary pore development belt of the Paleogene in the northern belt of Dongying Sag. Qingdao:China University of Petroleum(East China),2010.
[38] 王清斌.松辽盆地齐家北地区扶余油层次生孔隙发育规律及次生孔隙发育带预测.长春:吉林大学,2007. WANG Q B. The developing regularities and the developing zones forecasting of secondary pore of Fuyu reservoir in qijiabei area,Songliao Basin. Changchun:Jilin University,2007.
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