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天然气地球科学

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东营凹陷盐家地区沙四上亚段近岸水下扇砂砾岩颗粒结构特征

操应长,马奔奔，王艳忠，刘惠民，高永进，刘海宁,陈林   

  1. 1.中国石油大学地球科学与技术学院，山东 青岛 266580； 2.中国石化胜利油田地质科学研究院，山东 东营 257015；3.中国石化胜利油田物探研究院，山东 东营 257015； 4.中国石化胜利油田西部新区研究中心，山东 东营 257015
  • 收稿日期:2013-08-11 修回日期:2014-01-16 出版日期:2014-06-10 发布日期:2014-06-10
  • 通讯作者: 操应长cyc8391680@163.com E-mail:cyc8391680@163.com
  • 作者简介:操应长(1969-)，男，安徽潜山人，教授，主要从事沉积学、层序地层学等教学和科研工作. E-mail：cyc8391680@163.com.
  • 基金资助:

    国家科技重大专项课题(编号：2011ZX05006-003)；国家自然科学基金项目(编号：41102058)；国家自然基金石油化工石油化工联合基金重点项目(编号：U1262203);中国石油大学(华东)优秀博士学位论文培育计划项目(编号:LW140101A)联合资助.

The Particle Texture Characteristics of Sandy Conglomerate in theNearshore Subaqueous Fan of Upper Es4 in the Yanjia Area,Dongying Depression

CAO Ying-chang，MA Ben-ben，WANG Yan-zhong，LIU Hui-Min，GAO Yong-jin，LIU Hai-ning，CHEN Lin   

  1. 1.School of Geosciences in China University of Petroleum,Qingdao 266580,China;
    2.Geological Scientific Research Institute of Shengli Oilfield Company,SINOPEC,Dongying 257015,China;
    3.Geophysical Research Institute of Shengli Oilfield Company,SINOPEC,Dongying 257015,China;
    4.Western New Prospect Research Center of Shengli Oilfield Company,SINOPEC,Dongying 257015,China
  • Received:2013-08-11 Revised:2014-01-16 Online:2014-06-10 Published:2014-06-10

PDF (PC)

1238

摘要：

针对现有的粒度分析方法难以实现对砾岩、砾质砂岩等粗碎屑岩颗粒结构特征分析的问题，采用宏观岩心精描与微观薄片相结合的粒度分析方法，建立由砾级颗粒到砂级颗粒的粒度概率累积曲线，求取颗粒结构参数，并对近岸水下扇不同岩相组合类型颗粒结构特征展开定量研究。依据岩石结构、沉积构造和颜色等特征，将东营凹陷盐家地区沙四上亚段近岸水下扇砂砾岩体划分为11种岩相类型和14种岩相组合类型。依据φ5、Mz、So和砾石含量等颗粒结构参数绝对值及其垂向递降度特征，将近岸水下扇岩相组合划分为3大类6小类。总体上距物源方向断层边界距离由近及远砂砾岩颗粒结构参数具有粒度变细、分选变好、砾石含量降低和垂向递降度先增大后减小的特点。

关键词: 近岸水下扇, 砂砾岩, 颗粒结构, 沙四上亚段, 东营凹陷

Abstract:

It′s difficult to analyze the particle texture characteristics of coarse clastic rocks (conglomerate,conglomerate-sandstone,etc.) by using existing methods of particle size analysis.A method of combining macroscopic core delineation with microscopic thin-section identification was used.Probability cumulative grain size curves from gravel to sand were established.The parameters of particle texture were calculated,and the characteristics of particle texture among different lithofacies assemblages in near-shore subaqueous fan were studied quantitatively.According to the characteristics of rock structure,sedimentary structure and rock color,the sandy conglomerate bodies are separated into 11 types of lithofacies as well as 14 types of lithofacies assemblages of upper Es4 in the Yanjia area,Dongying Depression.On the basis of parameters of particle texture such as φ5,Mz,So,gravel contents and the characteristics of their vertical degradation degree,the types of lithofacies assemblages are divided into three categories and six subcategories.Generally,with the distance from near to distant from the fault boundary  in source direction,particle size turns fine,sorting becomes better,gravel contents decrease and vertical degradation degree increases at first then decreases.

Key words: Nearshore subaqueous fan, Sandy conglomerate, Particle texture, Upper Es4, Dongying Depression

中图分类号: 

  • TE122.2+2

［1］Jiang Zaixing.Sedimentology[M].Beijing:Petroleum Industry Press,2010.［姜在兴.沉积学[M].北京:石油工业出版社,2010.］
［2] Wu Zhixiong,Shi Ji′an,Zhang Yongshu,et al.Sedimentary features and facies of Paleogene braided river in Mabei area[J].Natural Gas Geoscience,2012,23(5):849-855.［吴志雄,史基安,张永庶,等.柴达木盆地北缘马北地区古近系辫状河微相特征及沉积模式[J].天然气地球科学,2012,23(5):849-855.］
［3］Yang Fei,Zou Niuniu,Shi Ji′an,et al.Probability cumulative grain size curves in the Paleogene clastic sediments and environmental significance in Maxian region of northern Qaidam Basin[J].Natural Gas Geoscience,2013,24(4):690-700.［杨飞,邹妞妞,史基安,等.柴达木盆地北缘马仙地区古近系碎屑岩沉积环境粒度概率累积曲线特征[J].天然气地球科学,2013,24(4):690-700.］
［4］Visher G S.Grain size distributions and depositional processes[J].Journal of Sedimentary Petrology,1969,39:1074-1106.
［5］Yuan Jing,Du Yumin,Li Yunnan.Probability cumulative grain size curves in terrigenous depositional environments of the Paleogene in Huimin Sag[J].Petroleum Exploration and Development,2003,30(3):103-107.［袁静,杜玉民,李云南.惠民凹陷古近系碎屑岩主要沉积环境粒度概率累积曲线特征[J].石油勘探与开发,2003,30(3):103-107.］
［6］Zhu Xiaomin,Kang An,Wang Guiwen,et al.Sedimentary characteristics of Jurassic braid delta in Santanghu Basin[J].Journal of the University of Petroleum,China:Natural Science Edition,1998,22(1):14-17.［朱筱敏,康安,王贵文,等.三塘湖盆地侏罗系辫状河三角洲沉积特征[J].石油大学学报:自然科学版,1998,22(1):14-17.］
［7］Yuan Jing,Yang Xuejun,Lu Zhiyong,et al.Probability cumulative grain size curves in sandy conglomerate of the upper Es4 in Yan 22 Block,Dongying Depression[J].Acta Sedimentologica Sinica,2011,29(5):815-823.［袁静,杨学君,路智勇,等.东营凹陷盐22块沙四上亚段砂砾岩粒度概率累积曲线特征[J].沉积学报,2011,29(5):815-823.］
［8］Sui Fenggui.Characteristics of reservoiring dynamic on the sand-conglomerate fanbodies in the steep-slope belt of continental fault basin:A case study on Dongying Depression[J].Oil & Gas Geology,2003,24(4):335-340.［隋风贵.断陷湖盆陡坡带砂砾岩扇体成藏动力学特征——以东营凹陷为例[J].石油与天然气地质,2003,24(4):335-340.］
［9］Kong Fanxian.Exploration technique and practice of sandy-conglomeratic fans in the northern part of Dongying Depression[J].Acta Petrolei Sinica,2000,21(5):27-31．［孔凡仙.东营凹陷北带砂砾岩扇体勘探技术与实践[J].石油学报,2000,21(5):27-31.］
［10］Sui Fenggui,Cao Yingchang,Liu Huimin,et al.Physical properties evolution and hydrocarbon accumula-tion of Paleogene nearshore subaqueous fan in the eastern north margin of the Dongying Depression[J].Acta Geologica Sinica,2010,84(2):246-256.［隋风贵,操应长,刘惠民,等.东营凹陷北带东部古近系近岸水下扇储集物性演化及其油气成藏模式[J].地质学报,2010,84(2):246-256.］
［11］Xu Xiaohui,Xu Jianhua,Xie Yuanjun,et al.The reservoir rocks of the subaqueous fans in the western segment of the steep slope zone of northern Dongying Depression,Shandong[J].Sedimentary Geology and Tethyan Geology,2003,23(1):84-85.［徐晓晖,许建华,谢远军,等.东营凹陷北部陡坡带西段水下扇体储集层特征[J].沉积与特提斯地质,2003,23(1):84-85.］
［12］An Jie,Cao Yingchang,Wang Yanzhong.Evolutional characteristics of physical property of sand-conglomerate reservoirs in nearshore subaqueous fans in Es4 in the northern zone of the Dongying Depression[J].Journal of Oil and Gas Technology,2008,30(6):221-222.［安洁,操应长,王艳忠.东营凹陷北带沙四段近岸水下扇砂砾岩储层物性演化特征[J].石油天然气学报,2008,30(6):221-222.］
［13］Zhang Qing.Reservoir characteristics and effective reservoir identification in upper Sha4 member of Yan222 block,Dongying Depression[J].Petroleum Geology and Recovery Efficiency,2008,15(4):33-34.［张清.东营凹陷盐222块沙四段上亚段有效储层识别[J].油气地质与采收率,2008,15(4):33-34.］
［14］Xia Jingsheng,Zhong Jianhua,Gao Xiangcheng.Characteristics and influencing factors of sand-conglomerate bodies in Es4 in the Fengshen1 area[J].Journal of Oil and Gas Technology,2007,29(3):199-200.［夏景生,钟建华,高祥成.丰深1地区沙四段砂砾岩体的储层特征及影响因素[J].石油天然气学报,2007,29(3):199-200.］
［15］Feng Zengzhao.Sedimentology[M].Beijing:Petroleum Industry Press,1993.［冯增昭.沉积岩石学[M].北京:石油工业出版社,1993.］
［16］Yang Guang.Analytical technique of gravels in core image and its application in research of conglomerate fan:Taking the conglomerate fan,northern steep slope,Dongying Sag as an example[J].Petroleum Geology and Recovery Efficiency,2010,17(5):20-23.［杨光.岩心图像砾石分析技术在砂砾岩扇体中的应用——以东营凹陷北部陡坡带扇体为例[J].油气地质与采收率,2010,17(5):20-23.］
［17］Sun Yu,Ma Shizhong,Shu Ping,et al.Analysis on grain-size characteristics and sedimentary environment of Es4 conglomerate reservoirs of Xingcheng gas field in Songliao Basin[J].Journal of Oil and Gas Technology,2010,32(4):171-176.［孙雨,马世忠,舒萍,等.松辽盆地兴城气田营四段砾岩储层粒度特征与沉积环境分析[J].石油天然气学报,2010,32(4):171-176.］
［18］Liu Hui,Cao Yingchang,Yuan Jing,et al.The types and reservoir characteristics of glutenite in the upper Es4 member of Shengtuo area[J].Journal of Southwest Petroleum University :Science ＆ Technology Edition,2010,32(5):10-11.［刘晖,操应长,袁静,等.胜坨地区沙四上亚段砂砾岩类型及储层特征[J].西南石油大学学报:自然科学版,2010,32(5):10-11.］
［19］Liu Fang,Wang Fenghua,Tan Bintian.Sedimentary characteristics and model of sandy conglomerate bodies in upper submember of Es4 of Tuo 76 block,Shengtuo area[J].Petroleum Geology and Recovery Efficiency,2010,17(5):48-50.［刘芳,王风华,谭滨田.胜坨地区坨76块沙四段上亚段砂砾岩体沉积特征及沉积模式[J].油气地质与采收率,2010,17(5):48-50.］
［20］Ran Jing,Du Gu,Pan Zhongxi.Study on methods for particle size analysis of sediment samples [J].Rock and Mineral Analysis,2011,30(6):669-676.［冉敬,杜谷,潘忠习.沉积物粒度分析方法的比较[J].岩矿测试,2011,30(6):669-676.］
［21］Li Wenkai,Wu Yuxin,Huang Zhimin,et al.Measurement results comparison between laser particle analyzer and sieving method in particle size distribution[J].China Powder Science and Technology,2007,4(5):10-13.［李文凯,吴玉新,黄志民,等.激光粒度分析和筛分法测粒径分布的比较[J].中国粉体技术,2007,4(5):10-13.］
［22］Zhang Fuyuan,Feng Xiuli,Zhang Weiyan,et al.Comparison and calibration of laser grain size analysis with pipette-sieve method:A solution for the underestimation of the clay fraction of surface sediments from the eastern South China Sea[J].Acta Sedimentologica Sinica,2011,29(4):767-773.［张富元,冯秀丽,章伟艳,等.南海表层沉积物的沉降法和激光法粒度分析结果对比和校正[J].沉积学报,2011,29(4):767-773.］
［23］Cheng Peng,Gao Shu,Li Xusheng.Evaluation of a wide range laser particle size analyses and comparison with pipette and sieving methods[J].Acta Sedimentologica Sinica,2001,19(3):449-454.［程鹏,高抒,李徐生.激光粒度仪测试结果及其与沉降法、筛析法的比较[J].沉积学报,2001,19(3):449-454.］
［24］Jiang Mingli.Geological applications of grain size analysis[J].Journal of Oil and Gas Technology,2009,31(1):161-163.［蒋明丽.粒度分析及其地质应用[J].石油天然气学报,2009,31(1):161-163.］
［25］Xiao Chenxi,Li Zhizhong.The research summary of grain size analysis and its application in the sedimentation[J].Journal of Xinjiang Normal University:Natural Sciences Edition,2006,25(3):118-122.［肖晨曦,李志忠.粒度分析及其在沉积学中应用研究[J].新疆师范大学学报:自然科学版,2006,25(3):118-122.］
［26］Ding Xigui,Ye Siyuan,Gao Zongjun.Development and applications of grain size analysis technique[J].Global Geology,2005,24(2):203-207.［丁喜桂,叶思源,高宗军.粒度分析理论技术进展及其应用[J].世界地质,2005,24(2):203-207.］
［27］Yu Xinghe,Wang Defa,Sun Zhihua.Lithofacies types,vertical profile features and reservoir geological models of braided deltaic sandbodies in faultde lake basin:The observation on deposition of modern deltas in Daihai Lake,Inner Mongolla[J].Acta Sedimentologica Sinica,2005,24(2):203-207.［于兴河,王德发,孙志华.湖泊辫状河三角洲岩相、层序特征及储层地质模型—内蒙古岱海湖现代三角洲沉积考察[J].沉积学报,1995,13(1):50-52.］
［28］Zhang Zhijie,Li Wei,Yang Jiajing,et al.Lithofacies association and depositional characteristics of the Upper Triassic Xujiahe Formation in Guang′an area,central Sichuan Basin[J].Earth Science Frontiers,2009,16(1):296-305.［张志杰,李伟,杨家静,等.川中广安地区上三叠统须家河组岩相组合与沉积特征[J].地学前缘,2009,16(1):296-305.］
［29］Gao Yongjin.Sedimentary cycle division and correlation of sand-conglomerate body:A case of upper Sha Ⅳ Formation of Yanjia area,Jiyang Depression[J].Petroleum Geology and Recovery Efficiency,2010,17(6):6-7.［高永进.砂砾岩体沉积旋回划分及对比方法——以济阳坳陷盐家地区沙四段上亚段为例[J].油气地质与采收率,2010,17(6):6-7.］
［30］Chen Huanqing,Hu Yongle,Ran Qiquan,et al.Lithofacies characteristics of volcanic gas reservoirs and their influence on reservoir physical properties:A case study of Member 1 of Cretaceous Yingcheng Formation in Xudong area of the Xushen Gasfield[J].Acta Petrologica et Mineralogica,2011,30(1):61-68.［陈欢庆,胡永乐,冉启全,等.火山岩气藏储层岩相特征及其对储层物性的影响——以徐深气田徐东地区白垩系营城组一段火山岩为例[J].岩石矿物学杂志,2011,30(1):61-68.］
［31］Wu Yanxiong,Wang Pujun,Qu Licai,et al.Detailed description of lithology,lithofacies and porosity and permeability of the first and the lower member of Yingcheng Formation:Based on the latest data of Ying-1D1 well cores in standard section[J].Journal of Jilin University:Earth Science Edition,2007,37(6):1193-1197.［吴颜雄,王璞珺,曲立才,等.营城组一段及下段岩性岩相和储层物性的精细刻画——基于标准剖面营一D1井全取心钻孔资料[J].吉林大学学报:地球科学版,2007,37(6):1193-1197.］
［32］Wang Pujun,Wu Heyong,Pang Yanming,et al.Volcanic facies of the Songliao Basin:sequence,model and the quantitative relationship with porosity & permeability of the volcanic reservoir[J].Journal of Jilin University:Earth Science Edition,2006,36(5):806-810.［王璞珺,吴河勇,庞颜明,等.松辽盆地火山岩相:相序、相模式与储层物性的定量关系[J].吉林大学学报:地球科学版,2006,36(5):806-810.］
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