天然气地球科学
高级检索
作者投稿 专家审稿 编辑办公

天然气地球科学 doi: 10.11764/j.issn.1672-1926.2017.06.002

• 天然气地质学 • 上一篇    下一篇

鄂尔多斯盆地西南部长6—长8段致密砂岩储层微观孔隙特征

杨智峰1,2，曾溅辉1,2，韩菲3，冯枭1,2，冯森1,2，张译丹1,2，乔俊程1,2   

  1. 1.中国石油大学油气资源与探测国家重点实验室,北京 102249;
    2.中国石油大学地球科学学院，北京 102249;3.联想(北京)有限公司,北京 100085
  • 收稿日期:2017-02-13 修回日期:2017-05-09 出版日期:2017-06-10 发布日期:2017-06-10
  • 作者简介:杨智峰(1987-)，男，新疆克拉玛依人，博士研究生，主要从事盆地流体与油气运聚成藏研究. E-mail：yangzhifeng_2005@126.com.
  • 基金资助:

    国家自然科学基金重点项目“致密砂岩微米_纳米级孔喉网络系统石油充注、运移和聚集机理”(编号：1330139)资助.

Characterization of microscopic pore texture of Chang 6-Chang 8 members tight sandstone reservoirs in the southwestern part of Ordos Basin,China

Yang Zhi-feng1,2，Zeng Jian-hui1,2，Han Fei3，Feng Xiao1,2，Feng Sen1,2，Zhang Yi-dan1,2，Qiao Jun-cheng1,2   

  1. 1. State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Beijing 102249,China;
    2. College of Geosciences,China University of Petroleum,Beijing 102249,China;
    3.Lenovo(Beijing) Co.,Ltd.,Beijing 100085,China
  • Received:2017-02-13 Revised:2017-05-09 Online:2017-06-10 Published:2017-06-10

PDF (PC)

783

摘要：

为了精确、直观地表征鄂尔多斯盆地西南部长6—长8段致密砂岩储层的微观孔隙结构，应用铸体薄片、扫描电镜与高压压汞等方法分析了储集空间的类型与物性特征，通过微米—纳米CT三维成像技术定量表征了微观孔隙的结构并对其三维孔隙的空间形态、大小、连通情况及分布特征进行了深入的研究，在此基础上进一步探讨了微观孔隙结构对孔隙度的影响。结果表明：长6—长8段致密砂岩储层发育多种类型的微观孔隙，常见有粒间孔、粒内孔、晶间孔与微裂缝4类孔隙类型。依据长宽比值(l/d)划分三维微观孔隙的空间形态类型，其中粒间孔为不规则状，粒内孔与晶间孔为球状，微裂缝多为管束状。微米尺度下不规则状与管束状孔隙发育，孔隙连通性较好，孔隙体积多为20～100μm3，平均孔隙半径多小于5μm；纳米尺度下球状孔隙发育，孔隙连通性较差，孔隙体积多为104～107nm3，平均孔隙半径多小于0.1μm。致密砂岩孔隙度与平均孔隙半径的相关性较差，其中管束状孔隙的数量、管束状与不规则状孔隙的平均半径对样品孔隙度的影响较大。由此可知微米尺度下管束状与不规则状孔隙是长6—长8段致密砂岩储层储集空间的主要贡献者。

关键词: 致密砂岩储层, 微米&mdash, 纳米CT, 孔隙类型, 长6&mdash, 长8段, 鄂尔多斯盆地

Abstract:

In order to characterize the pore structure of Chang 6-Chang 8 members tight sandstone reservoirs in the southwestern part of Ordos Basin accurately and visually,thin-section,Scanning Electron Microscope (SEM) and high pressure mercury injection techniques were used to analyze pore types and reservoir characteristics. Micro-nano CT imaging technology is adopted to give three-dimensional (3D) representation of pore spatial morphology,size and connection,and effect of pore type on porosity is further analyzed in this paper. The results indicate that Chang 6-Chang 8 members sandstones have four major types of pore textures,including inter-granular pores,intra-granular pores,inter-crystalline pores,and micro-fractures. Pore spatial morphology of 3D is divided into three types by the ratio of length to width（l/d）. Inter-granular pores are irregularly shaped with 3D imaging,whereas intra-granular and inter-crystalline pores,and microfractures have spherical and pipe shape,respectively. Irregular-shaped and pipe-shaped pores are predominated at micro-scale,the pore connectivity is better. The pore volume ranges mostly from 20 to 100μm3,and the average pore radius is commonly less than 5μm. The spherical pores are predominated at nano-scale,the pore volume ranges mainly from 104 to 107nm3,with the average pore radius of less than 0.1μm. The correlation between porosity and pore abundance is poor. Pipe-shaped pore quantity,average radius of pipe-shaped and irregular-shaped pores have significant effect on sample porosity. Pipe-shaped and irregular-shaped pores at micro-scale have significant effect on porosity of Chang 6-Chang 8 members tight sandstone reservoirs.

Key words: Tight sandstone reservoir, Micro-nano CT, Pore types, Chang 6-Chang 8 members, Ordos Basin

中图分类号: 

  • TE122.1

[1]Zou Caineng,Zhu Rukai,Wu Songtao,et al.Types,characteristics,genesis and prospects of conventional and unconventional hydrocarbon accumulations:Taking tight oil and tight gas in China as an instance[J].Acta Petrolei Sinica,2012,33(2):173-187.[邹才能,朱如凯,吴松涛,等.常规与非常规油气聚集类型、特征、机理及展望——以中国致密油和致密气为例[J].石油学报,2012,33(2):173-187.]
[2]Zeng Jianhui,Yang Zhifeng,Feng Xiao,et al.Study status and key scientific issue of tight reservoir oil and gas accumulation mechanism[J].Advances in Earth Science,2014,29(6):651-661.[曾溅辉,杨智峰,冯枭,等.致密储层油气成藏机理研究现状及其关键科学问题[J].地球科学进展,2014,29(6):651-661.]
[3]You Yuan,Niu Xiaobing,Xin Honggang,et al.Research on micro pore structure of overseas tight oil reservoir and its influence on Ordos Basin[J].Oil Forum,2013,32(1):12-18.[尤源,牛小兵,辛红刚,等.国外致密油储层微观孔隙结构研究及其对鄂尔多斯盆地的启示[J].石油科技论坛,2013,32(1):12-18.]
[4]Jiang Yuqiang,Chen Lin,Jiang Chan,et al.Characterization techniques and trends of the pore structure of tight reservoirs[J].Geological Science and Technology Inforamtion,2014,33(3):63-70.[蒋裕强,陈林,蒋婵,等.致密储层孔隙结构表征技术及发展趋势[J].地质科技情报,2014,33(3):63-70.]
[5]Wang Weiming,Lu Shuangfang,Li Jie,et al.Analyses of micro-pore structural characteristics of tight sandstone  reservoirs:A case study in Turpan-Hami Basin,northwestern China[J].Natural Gas Geoscience,2016,27(10):1828-1836.[王伟明,卢双舫,李杰,等.致密砂岩储层微观孔隙特征评价——以中国吐哈盆地为例[J].天然气地球科学,2016,27(10):1828-1836.]
[6]Loucks R G,Reed R M,Ruppel S C et al.Morphology,genesis,and distribution of nanometer-scale pores in siliceous mudstones of the mississippian barnett shale[J].Journal of Sedimentary Research,2009,79(12):848-861.
[7]Yang Feng,Ning Zhengfu,Kong Detao,et al.Pore structure of shales from high pressure mercury injection and nitrogen adsorp-tion method[J].Natural Gas Geoscience,2013,24(3):450-455.[杨峰,宁正福,孔德涛,等.高压压汞法和氮气吸附法分析页岩孔隙结构[J].天然气地球科学,2013,24(3):450-455.]
[8]Shi Tiaotiao,Sun Wei,Zhang Chuang,et al.Diagenetic facies and micro-pore structure of Chang 6 reservoir in Yanchang Formation,Huaqing area,Ordos Basin[J].Geoscience,2012,26(4):769-777.[师调调,孙卫,张创,等.鄂尔多斯盆地华庆地区延长组长6储层成岩相及微观孔隙结构[J].现代地质,2012,26(4):769-777.]
[9]Wang Wei,Zhu Yushuang,Niu Xiaobing,et al.Characteristics of reservoir microscopic pore structure and its controlling factors of Chang6 in Jiyuan area of Ordos Basin[J].Geological Science and Techology Information,2013,32(2):118-124.[王伟,朱玉双,牛小兵,等.鄂尔多斯盆地姬塬地区长6储层微观孔隙结构及控制因素[J].地质科技情报,2013,32(2):118-124.]
[10]Wu Hao,Guo Yinghai,Zhang Chunlin,et al.Characteristics and classifications of micro-pore structure in tight oil reservoir:A case study of the triassic Yanchang Formation Chang7 in Longdong area,Ordos Basin[J].Journal of Northeast Petroleum University,2013,37(6):12-17.[吴浩,郭英海,张春林,等.致密油储层微观孔吼结构特征及分类——以鄂尔多斯盆地陇东地区三叠统延长组长7段为例[J].东北石油大学学报,2013,37(6):12-17.]
[11]Wu Songtao,Zhu Rukai,Cui Jinggang,et al.Characteristics of lacustrine shale porosity evolution,Triassic Chang 7 member,Ordos Basin,NW China[J].Petroleum Exploration and Development,2015,42(2):167-176.[吴松涛,朱如凯,崔京钢,等.鄂尔多斯盆地长7湖相泥页岩孔隙演化特征[J].石油勘探与开发,2015,42(2):167-176.]
[12]Yang Wei,Chen Guojun,Lv Chengfu,et al.Micro characteristics of the organic-rich in the 7th member of the Yanchang Formation in the southeast of Ordos Basin[J].Natural Gas Geoscience,2015,26(3):418-426.[杨巍,陈国俊,吕成福,等.鄂尔多斯盆地东南部延长组长7段富有机质页岩孔隙特征[J].天然气地球科学,2015,26(3):418-426.]
[13]Bera Bijoyendra,Mitra Sushanta K,Vick Douglas.Understanding the micro structure of Berea Sandstone by the simultaneous use of micro-computed tomography (micro-CT)and focused ion beam-scanning electron microscopy (FIB-SEM)[J].Micron,2011,42(5):412-418.
[14]Peng S,Hu Q,Dultz S,et al.Using X-ray computed tomography in pore structure characterization for a Berea sandstone:resolution effect[J].Journal of Hydrology,2012,(472/473):254-261.
[15]Qu Le,Sun Wei,Du Huanhong,et al.Characterization technique of pore structure by 3D digital core based on CT scanning and its application:An example from Sangonghe Formation of 116 well field in Mobei Oilfield[J].Geoscience,2014,28(1):190-196.[屈乐,孙卫,杜环虹,等.基于CT扫描的三维数字岩心孔隙结构表征方法及应用——以莫北油田116井区三工河组为例[J].现代地质,2014,28(1):190-196.]
[16]Zheng Jianfeng,Chen Yongquan,Ni Xinfeng,et al.Microstructure characterization based on CT imaging technology of Cambrain dolomite reservoir in Tarim Basin[J].Natural Gas Geoscience,2016,27(5):780-789.[郑剑锋,陈永权,倪新锋,等.基于CT成像技术的塔里木盆地寒武系白云岩储层微观表征[J].天然气地球科学,2016,27(5):780-789.]
[17]Jia Chengzao,Zou Caineng,Li Jianzhong,et al.Assessment criteriam,main types,basicthe tight oilfeatures and resource prospects oil in China [J].Acta Petrolei Sinica,2012,33(3):343-350.[贾承造,邹才能,李建忠,等.中国致密油评价标准、主要类型、基本特征及资源前景[J].石油学报,2012,33(3):343-350.]
[18]Yao Jingli,Zhao Yande,Deng Xiuqin,et al.Controlling Factors of Tight Oil Reservior in Triassic Yanchang Formation in Ordos Basin [J].Journal of Jilin University:Earth Science Edition,2015,45(4):983-992.[姚泾利,赵彦德,邓秀芹,等.鄂尔多斯盆地延长组致密油成藏控制因素[J].吉林大学学报:地球科学版,2015,45(4):983-992.]
[19]Yang Hua,Li Shixiang,Liu Xianyang.Characteristics and resource prospects of tight oil and shale oil in Ordos Basin [J].Acta Petrolei Sinica,2013,34(1):1-11.[杨华,李士祥,刘显阳.鄂尔多斯盆地致密油、页岩油特征及资源潜力[J].石油学报,2013,34(1):1-11.]
[20]Zhao Jingzhou,Bai Yubin,Cao Qing,et al.Quasi-continuous hydrocarbon accumulation:A new pattern for large tight sand oilfields in the Ordos Basin[J].Oil & Gas Geology,2012,33(6):811-827.[赵靖舟,白玉彬,曹青,等.鄂尔多斯盆地准连续型低渗透—致密砂岩大油田成藏模式[J].石油与天然气地质,2012,33(6):811-827.]
[21]Zhang Shaonan,Ding Xiaoqi.Characters and causes of tight sandstones of Yanchang Formation in southern Ordos Basin,China[J].Journal of Chengdu University of Technology：Science & Technology Edition,2010,37(4):388-394.[张哨南,丁晓琪.鄂尔多斯盆地南部延长组致密砂岩储层特征及其成因[J].成都理工大学学报：自然科学版,2010,37(4):388-394.]
[22]Ding Xiaoqi,Zhang Shaonan,Ge Pengli,et al.Research on Diagensis System of Yanchang Formation Reservoirs,southeast Ordos Basin[J].Acta Sedimentologica Sinica,2011,29(1):97-104.[丁晓琪,张哨南,葛鹏莉,等.鄂尔多斯盆地南部延长组储层成岩体系研究[J].沉积学报,2011,29(1):97-104.]
[23]Zhou Xiang,He Sheng,Chen Zhaoyou,et al.Diagenesis and diagenetic facies of low porosity and permeability sandstone in member 8 of the Yanchang Formation in Daijiaping area,Ordos Basin[J].Oil & Gas Geology,2016,37(2):155-164.[周翔,何生,陈召佑,等.鄂尔多斯盆地代家坪地区延长组8段低孔渗砂岩成岩作用及成岩相[J].石油与天然气地质,2016,37(2):155-164.]
[24]Cui Jingwei,Zhu Rukai,Wu Songtao,et al.Heterogeneity Chang-7 and lower oily limits for tight sandstones:A case study on oil layers of the Yanchang Formation，Ordos Basin[J].Acta Petrolei Sinica,2013,34(5):887-882.[崔景伟,朱如凯,吴松涛,等.致密砂岩层内非均质性及含油下限——以鄂尔多斯盆地三叠系延长组长7段为例[J].石油学报,2013,34(5):887-882.]
[25]Luo Xiaorong,Wang Zhongnan,Lei Yuhong,et al.Heterogeneity characteristic and accumulation model of the ultra-low permeability sandstone reservoirs:A case study of the part of Yanchang Formation in the western Ordos Basin,China[J].Acta Petrolei Sinica,2016,37(1):87-98.[罗晓容,王忠楠,雷裕红,等.特超低渗砂岩油藏储层非均质性特征与成藏模式——以鄂尔多斯盆地西部延长组下组合为例[J].石油学报,2016,37(1):87-98.]
[26]Ren Xiaoxia,Li Aifen,Wang Yongzheng,et al.Pore structure of tight sand reservoir and its influence on percolation-Taking the Chang 8 reservoir in Maling oilfield in Ordos Basin as an example[J].Oil & Gas Geology,2015,36(5):774-779.[任晓霞,李爱芬,王永政,等.致密砂岩储层孔隙结构及其对渗流的影响——以鄂尔多斯盆地马岭油田长8储层为例[J].石油与天然气地质,2015,36(5):774-779.]
[27]Bi Mingwei,Chen Shiyue,Zhou Zhaohua,et al.Characteristics and significance of microscopic pore structure in tight sandstone reservoir of the 8th member of lower Shihezi Formation in the Sub area of Sulige Gasfield[J].Natural Gas Geoscience,2015,26(10):1851-1861.[毕明威,陈世悦,周兆华,等.鄂尔多斯盆地苏里格气田苏6区块盒8段致密砂岩储层微观孔隙结构特征及其意义[J].天然气地球科学,2015,26(10):1851-1861.]
[28]Bai Bin,Zhu Rukai,Wu Songtao,et al.Multi-scale method of Nano(Micro)-CT study on microscopic pore structure of tight sandstone of Yanchang Formation Ordos Basin[J].Petroleum Exploration and development,2013,40(3):329-333.[白斌,朱如凯,吴松涛,等.利用多尺度CT成像表征致密砂岩微观孔喉结构[J].石油勘探与开发,2013,40(3):329-333.]
[29]Zhou Yong,Xu Liming,Ji Youliang,et al.Charateristic and distributing controlling fators of relatively high permeability reservior:A case study from Chang 82 sandstone of Yanchang formation in Longdong area,Ordos Basin[J].Journal of China University of Mining & Technology,2017,46(1):106-117.[周勇,徐黎明,纪友亮,等.致密砂岩相对高渗透储层特征及分布控制因素研究——以鄂尔多斯盆地陇东地区延长组长82为例[J].中国矿业大学学报,2017,46(1):106-117.]
[30]Zhao Jingzhou,Wu Fuli,Yan Shike,et al.Regularity of Triassic petroleum accumulation and distribution in the east part of north Shanbei Slope[J].Acta Petrolei Sinica,2006,27(5):24-34.[赵靖舟,武富礼,闫世可,等.陕北斜坡东部三叠系油气富集规律研究[J].石油学报,2006,27(5):24-34.]
[31]Zou Caineng,Yang Zhi,Tao Shizhen,et al.Nano-hydrocarbon and the accumulation in coexisting source and reservoir[J].Petroleum Exploration and Development,2012,39(1):13-26.[邹才能,杨智,陶士振,等.纳米油气与源储共生型油气聚集[J].石油勘探与开发,2012,39(1):13-26.]
[32]Zhen Ximin,Song Guangshou,Wang Duoyun,et al.Sedimentary anatomy of thick anisotropic sandstone for Chang8 oil formation in Longdong area,Shaan-Gan-Ning Basin[J].Acta sedimentologica sinica,2003,21(2):272-277.[郑希民,宋广涛,王多云,等.陕甘宁盆地陇东地区长8油组厚层非均质砂体的沉积学解剖[J].沉积学报,2003,21(2):272-277.]
[33]Wu Fuli,Li Wenhou,Li Yuhong,et al.Delta sediments and evolution of the Yangchang Formation of Upper Triassic in Ordos Basin[J].Paleogeography,2004,6(3):307-315.[武富礼,李文厚,李玉宏,等.鄂尔多斯盆地上三叠统延长组三角洲沉积及演化[J].古地理学报,2004,6(3):307-315.]
[34]Ketcham R A,Carlson W D.Acquisition,optimization and interpretation of X-ray computed tomographic imagery:applications to the geosciences[J].Computers & Geosciences,2001,27(4):381-400.
[35]Agbogun H M D,Al T A,Hussein E M A.Three dimensional imaging of porosity and tracer concentration distributions in a dolostone sample during diffusion experiments using X-ray micro-CT[J].Journal of Contaminant Hydrology,2013,145:44-53.
[36]Wang Jialu,Gao Jian,Liu Li,et al.Porosity characteristics of sandstone by X-ray CT scanning system[J].Acta Petrolei Sinica,2009,30(6):887-897.[王家禄,高建,刘莉,等.应用CT技术研究岩石孔隙变化特征[J].石油学报,2009,30(6):887-897.]
[37]Yang Shaochun,Wang Huijuan,Luo Haining,et al.Nanoscale pore structure characteristics of clastic rock in Shengli Oilfield[J].Journal of the Univerisity of Petroleum,China:Edition of Natural Science,2012,36(1):8-19.[杨少春,王惠娟,罗海宁,等.胜利油区碎屑岩纳米尺度孔隙结构特征[J].中国石油大学学报:自然科学版,2012,36(1):8-19.]
[1] 景辅泰, 罗霞, 杨智, 张丽君, 李士祥, 陈勇, 曾云锋. 页岩层系致密储层物性下限——以鄂尔多斯盆地三叠系延长组长7段为例[J]. 天然气地球科学, 2020, 31(6): 835-845.
[2] 郭明强, 周龙刚, 张兵, 潘新志, 王应斌. 致密砂岩气水分布特征——以鄂尔多斯盆地东部临兴地区为例[J]. 天然气地球科学, 2020, 31(6): 855-864.
[3] 于洲, 周进高, 丁振纯, 魏柳斌, 魏源, 吴兴宁, 吴东旭, 王少依, 李维岭. 鄂尔多斯盆地中东部奥陶系马五41a储层特征及成因[J]. 天然气地球科学, 2020, 31(5): 686-697.
[4] 梁晓伟,关梓轩,牛小兵,关平,淡卫东,冯胜斌,尤源,周树勋. 鄂尔多斯盆地延长组7段页岩油储层储集性特征[J]. 天然气地球科学, 2020, 31(10): 1489-1500.
[5] 吕文雅, 曾联波, 周思宾, 吉园园, 梁丰, 惠晨, 尉加盛. 鄂尔多斯盆地西南部致密砂岩储层微观裂缝特征及控制因素[J]. 天然气地球科学, 2020, 31(1): 37-46.
[6] 张春林, 李剑, 陈鑫, 吴庆超. 鄂尔多斯盆地东部奥陶系盐下古地貌恢复及其对滩体的控制作用[J]. 天然气地球科学, 2019, 30(9): 1263-1271.
[7] 吴松涛, 林士尧, 晁代君, 翟秀芬, 王晓瑞, 黄秀, 徐加乐. 基于孔隙结构控制的致密砂岩可动流体评价——以鄂尔多斯盆地华庆地区上三叠统长6致密砂岩为例[J]. 天然气地球科学, 2019, 30(8): 1222-1232.
[8] 尤源, 梁晓伟, 冯胜斌, 牛小兵, 淡卫东, 李卫成, 王芳, . 鄂尔多斯盆地长7段致密储层主要黏土矿物特征及其地质意义[J]. 天然气地球科学, 2019, 30(8): 1233-1241.
[9] 崔景伟, 朱如凯, 李森, 齐亚林, 时晓章, 毛治国, . 坳陷湖盆烃源岩发育样式及其对石油聚集的控制——以鄂尔多斯盆地三叠系延长组长7油层组为例[J]. 天然气地球科学, 2019, 30(7): 982-996.
[10] 李阳, 倪小明, 王延斌, 陶传奇. 鄂尔多斯盆地临兴地区上古生界压力特征及其成因机制[J]. 天然气地球科学, 2019, 30(7): 997-1005.
[11] 吴小奇, 倪春华, 陈迎宾, 朱建辉, 李贶, 曾华盛. 鄂尔多斯盆地定北地区上古生界天然气来源[J]. 天然气地球科学, 2019, 30(6): 819-827.
[12] 吴伟涛, 王一, 赵靖舟, 杨特波, 李军, 黄正良. 鄂尔多斯盆地中部奥陶系马家沟组中组合天然气成藏规律[J]. 天然气地球科学, 2019, 30(6): 828-839.
[13] 张成龙, 陶士振, 白斌, 王倩茹. 基于支持向量机模型的烃源岩有机碳含量预测——以鄂尔多斯盆地为例[J]. 天然气地球科学, 2019, 30(5): 761-768.
[14] 刘晓鹏, 赵会涛, 闫小雄, 贾亚妮, . 克拉通盆地致密气成藏地质特征与勘探目标优选——以鄂尔多斯盆地上古生界为例[J]. 天然气地球科学, 2019, 30(3): 331-343.
[15] 高阳, 王志章, 易士威, 佘源琦, 林世国, 李明鹏, 张春林, . 鄂尔多斯盆地天环地区盒8段致密砂岩岩石矿物特征及其对储层质量的影响[J]. 天然气地球科学, 2019, 30(3): 344-352.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] Al-Arouri K;Mckirdy D;Boreham C（澳大利亚）;孙庆峰（译）. 用油源对比方法识别澳大利亚南塔鲁姆凹陷的石油系统[J]. 天然气地球科学, 2000, 11(4-5): 57 -67 .
[2] 马立祥;. 断层封闭性研究在烃类聚集系统分析中的意义[J]. 天然气地球科学, 2000, 11(3): 1 -8 .
[3] 马立祥. 岩石物理流动单元的概念及其研究现状[J]. 天然气地球科学, 2000, 11(2): 30 -36 .
[4] 李在光;杨占龙;李琳;郭精义;黄云峰;吴青鹏;李红哲;. 胜北地区油气分布规律[J]. 天然气地球科学, 2006, 17(1): 94 -96 .
[5] 王杰，刘文汇，秦建中，张隽. 中国东部幔源气藏存在的现实性与聚集成藏的规律性[J]. 天然气地球科学, 2007, 18(1): 19 -26 .
[6] 李亮,万晓龙,李志伟,张永强,张振红. 油气成藏模拟实验在白于山油藏开发中的应用[J]. 天然气地球科学, 2006, 17(2): 219 -222 .
[7] 李广之;袁子艳;胡斌;邓天龙;. 利用顶空气技术判别凝析气(油)储层[J]. 天然气地球科学, 2006, 17(3): 309 -312 .
[8] 李凤杰;王多云;. 鄂尔多斯盆地西峰油田延长组高分辨率层序地层学研究[J]. 天然气地球科学, 2006, 17(3): 339 -344 .
[9] 赵孟军;宋岩;柳少波;秦胜飞;洪峰;傅国友;达江;. 中国中西部前陆盆地成藏特征的初步分析[J]. 天然气地球科学, 2006, 17(4): 445 -451 .
[10] 姚亚明;周继军;何明喜;付代国;陈建军;. 对焉耆盆地油气地质条件的认识[J]. 天然气地球科学, 2006, 17(4): 463 -467 .