岩性油气藏 ›› 2020, Vol. 32 ›› Issue (1): 66–75.doi: 10.12108/yxyqc.20200107

• 油气地质 • 上一篇    下一篇

鄂尔多斯盆地富县地区延长组长7烃源岩特征及评价

黄彦杰1, 白玉彬1,2, 孙兵华3, 黄礼1, 黄昌武4   

  1. 1. 西安石油大学 地球科学与工程学院, 西安 710065;
    2. 陕西省油气成藏地质学重点实验室, 西安 710065;
    3. 延长油田股份有限公司 富县采油厂, 陕西 延安 716000;
    4. 中国石油勘探开发研究院, 北京 100083
  • 收稿日期:2019-04-08 修回日期:2019-07-13 出版日期:2020-01-21 发布日期:2019-11-22
  • 第一作者:黄彦杰(1995-),男,西安石油大学在读硕士研究生,研究方向为油气成藏地质学。地址:(710065)陕西省西安市雁塔区电子二路东段18号。Email:346324589@qq.com
  • 通信作者: 白玉彬(1981-),男,博士,副教授,主要从事油气成藏机理方面的研究。Email:baiyubin@xsyu.edu.cn。
  • 基金资助:
    西安石油大学研究生创新与实践能力培养项目“鄂尔多斯盆地富县地区长7致密油成藏机理与成藏模式”(编号:YCS18212033)、陕西省教育厅科研计划项目“鄂尔多斯盆地志丹地区长9、长10致密油形成机理研究”(编号:18JS090)和陕西省自然科学基础研究计划项目“湖相富有机质页岩储集空间定量表征及含油性研究”(编号:2017JM4014)联合资助

Characteristics and evaluation of Chang 7 source rock of Yanchang Formation in Fuxian area, Ordos Basin

HUANG Yanjie1, BAI Yubin1,2, SUN Binghua3, HUANG Li1, HUANG Changwu4   

  1. 1. School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, China;
    2. Shaanxi Key Laboratory of Petroleum Accumulation Geology, Xi'an 710065, China;
    3. Fuxian Oil Production Plant, Yanchang Oilfield Co., Ltd., Yan'an 716000, Shaanxi, China;
    4. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China
  • Received:2019-04-08 Revised:2019-07-13 Online:2020-01-21 Published:2019-11-22

摘要: 为研究鄂尔多斯盆地富县地区延长组长7烃源岩特征及生烃潜力,开展了岩心分析、测井研究、干酪根镜检、镜质体反射率(Ro)测试、岩石热解分析、气相色谱及色谱-质谱分析。结果表明:(1)富县地区长7烃源岩平均厚度为45 m;总有机碳(TOC)质量分数平均为5.94%;生烃潜量(S1+S2)平均为13.1mg/g。(2)有机质类型以Ⅰ和Ⅱ1型为主,烃源岩母质类型以低等水生生物为主,并含部分高等植物,沉积时水体为还原环境。(3)镜质体反射率平均为0.76%,生物标志化合物中C31藿烷22S(/22R+22S)、20RC29αββ(/αββ+ααα)和αααC2920S(/20S+20R)平均值分别为0.52、0.62和0.49,反映有机质演化进入生油高峰阶段。(4)平面上,富县地区中部和西北部长7烃源岩厚度大、生烃能力更强,为下一步勘探的有利区带。该研究成果对鄂尔多斯盆地富县地区的精细勘探具有重要指导作用。

关键词: 烃源岩, 地球化学特征, 长7, 富县地区, 鄂尔多斯盆地

Abstract: In order to study the characteristics and hydrocarbon generation potential of Chang 7 source rock of Yanchang Formation in Fuxian area of Ordos Basin,core analysis,well logging research, kerogen microscopy, vitrinite reflectance(Ro) test,rock pyrolysis analysis, gas phase chromatography and chromatography-mass spectrometry were carried out. The results show that:(1) The average thickness of Chang 7 source rock in Fuxian area was 45 m,the TOC mass fraction averaged 5.94%,and the average hydrocarbon generation potential(S1+S2) was 13.1 mg/g.(2)The types of organic matter were mainly type I and Ⅱ1,and the source of the source rock was mainly composed of lower aquatic organisms and contained some higher plants. The water body was a reducing environment during sedimentation.(3)The vitrinite reflectance averaged 0.76%. Among the biomarker compounds, C31 hopane 22S(/22R+22S),20RC29αββ(/αββ+ααα)and αααC2920S(/20S+20R), the average values were 0.52,0.62,0.49,respectively,reflecting the evolution of organic matter into the peak stage of oil production.(4)On the plane, Chang 7 source rocks in the central and northwestern Fuxian area have large thicknesses and stronger hydrocarbon generation capacity, which is a favorable zone for further exploration. The research results play an important guiding role for fine exploration in Fuxian area of the Ordos Basin.

Key words: source rock, geochemical characteristics, Chang 7, Fuxian area, Ordos Basin

中图分类号: 

  • TE132.2
[1] 邱振, 李建忠, 吴晓智, 等.国内外致密油勘探现状、主要地质特征及差异.岩性油气藏, 2015, 27(4):119-126. QIU Z, LI J Z, WU X Z, et al.Exploration status, main geologic characteristics and their differences of tight oil between America and China. Lithologic Reservoirs, 2015, 27(4):119-126.
[2] 郭凯.鄂尔多斯盆地陇东地区长7段有效烃源岩及生排烃研究.石油实验地质, 2017, 39(1):15-23. GUO K.Active source rocks of Chang 7 member and hydrocarbon generation and expulsion characteristics in Longdong area, Ordos Basin. Petroleum Geology & Experiment, 2017, 39(1):15-23.
[3] 肖承钰, 尹伟, 张颖, 等.鄂尔多斯镇泾地区延长组成藏体系与油气富集模式.石油实验地质, 2015, 37(3):347-353. XIAO C Y, YIN W, ZHANG Y, et al. Petroleum accumulation systems and oil enrichment patterns of Yanchang Formation in Zhenjing area, southern Ordos Basin. Petroleum Geology & Experiment, 2015, 37(3):347-353.
[4] 白玉彬, 赵靖舟, 方朝强, 等.优质烃源岩对鄂尔多斯盆地延长组石油聚集的控制作用. 西安石油大学学报(自然科学版), 2012, 27(3):1-5. BAI Y B, ZHAO J Z, FANG Z Q, et al. Control effect of highquality source rocks on petroleum accumulation in Yanchang Formation, Ordos Basin. Journal of Xi'an Shiyou University (Natural Science Edition), 2012, 27(3):1-5.
[5] 李威, 文志刚.鄂尔多斯盆地马岭地区上三叠统长7油层组油气富集规律.岩性油气藏, 2012, 24(6):101-105. LI W, WEN Z G. Hydrocarbon enrichment of Upper Triassic Chang 7 oil reservoir set in Maling area, Ordos Basin. Lithologic Reservoirs, 2012, 24(6):101-105.
[6] 唐建云, 王志维, 也尔哈那提·黑扎提, 等.鄂尔多斯盆地旬邑探区延长组烃源岩及原油地球化学特征.岩性油气藏, 2016, 28(6):78-79. TANG J Y, WANG Z W, YE'ERHANATI H Z T, et al. Hydrocarbon source evaluation and oil source contrast of the Yan Chang group in Xunyi Exploration area, Ordos Basin. Lithologic Reservoirs, 2016, 28(6):78-79.
[7] 张文正, 杨华, 李剑锋, 等.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用:强生排烃特征及机理分析.石油勘探与开发, 2006, 33(3):289-293. ZHANG W Z, YANG H, LI J F, et al. Leading effect of high class source rock of Chang 7 in Ordos Basin on enrichment of low permeability oil-gas accumulation:Hydrocarbon generation and expulsion mechanism. Petroleum Exploration and Development, 2006, 33(3):289-293.
[8] 葛云锦, 任来义, 贺永红, 等.鄂尔多斯盆地富县-甘泉地区三叠系延长组7油层组致密油富集主控因素. 石油与天然气地质, 2018, 39(6):1190-1200. GE Y J, REN L Y, HE Y H, et al. Main factors controlling the tight oil enrichment in the 7th oil layer group of the Triassic Yanchang Formation in Fuxian-Ganquan area, Ordos Basin. Oil & Gas Geology, 2018, 39(6):1190-1200.
[9] 邓亚仁, 任战利, 马文强, 等.鄂尔多斯盆地富县地区长8层段致密砂岩储层特征及充注下限.石油实验地质, 2018, 40(2):288-294. DENG Y R, REN Z L, MA W Q, et al. Reservoir properties and hydrocarbon charging threshold of Chang 8 tight sandstones in Fuxian area, Ordos Basin. Petroleum Geology & Experimental, 2018, 40(2):288-294.
[10] 郭德运, 郭艳琴, 李文厚, 等.富县探区上三叠统延长组成岩作用及孔隙结构特征.沉积学报, 2010, 15(2):264-273. GUO D Y, GUO Y Q, LI W H, et al. Diagenesis and pore structure characteristic of Yanchang Formation of Upper Triassic in Fuxian exploration area. Acta Sedimentologica Sinica, 2010, 15(2):264-273.
[11] 李士春, 冯朝荣, 殷世江.鄂尔多斯盆地南部中生界延长组沉积体系与油气富集.岩性油气藏, 2010, 22(2):79-83. LI S C, FENG Z R, YIN S J.Sedimentary systems and hydrocarbon enrichment of Yanchang Formation in southern Ordos Basin. Lithologic Reservoirs, 2010, 22(2):79-83.
[12] 杨华, 张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用:地质地球化学特征. 地球化学, 2005, 34(2):147-154. YANG H, ZHANG W Z. Leading effect of the Seventh Member high-qulity source rock of Yanchang Formation in Ordos Basin during the enrichment of low-penetrating oil-gas accumulation:Geology and Geochemistry. Geochimica, 2005, 34(2):147-154.
[13] 王晖, 高栋臣, 尹锦涛, 等.鄂尔多斯盆地富县地区长7油组页岩气地球化学特征及成因.新疆石油地质, 2017, 38(3):289-295. WANG H, GAO D C, YIN J T, et al. Geochemical characteristics and genesis of shale gas in Chang 7 oil member of Fuxian area, Ordos Basin. Xinjiang Petroleum Geology, 2017, 38(3):289-295.
[14] 袁媛, 杜克锋, 葛云锦, 等.鄂尔多斯盆地甘泉-富县地区长7烃源岩地球化学特征.岩性油气藏, 2018, 30(1):39-45. YUAN Y, DU K F, GE Y J, et al. Geochemistry of hydrocarbon source rocks of Chang 7 in Ganquan-Fuxian area, Ordos Basin. Lithologic Reservoirs, 2018, 30(1):39-45.
[15] 贺永红, 任战利, 陈占军, 等.富县探区长8段致密油藏特征及主控因素.西安科技大学学报, 2016, 36(3):393-399. HE Y H, REN Z L, CHEN Z J, et al. Chang 8 section tight oil reservoir characteristics and distributional controlling factors in Fuxian exploration area. Journal of Xi'an University of Science and Technology, 2016, 36(3):393-399.
[16] 贾承造, 邹才能, 杨智, 等.陆相油气地质理论在中国中西部盆地的重大进展.石油勘探与开发, 2018, 45(4):546-560. JIA C Z, ZOU C N, YANG Z, et al. Significant progress of continental petroleum geology theory in basins of Central and Western China. Petroleum Exploration and Development, 2018, 45(4):546-560.
[17] 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 member 7 in Yanchang Formation of Triassic in Ordos Basin. Acta Sedimentologica Sinica, 2010, 28(2):254-263.
[18] 白玉彬, 罗静兰, 张天杰, 等.鄂尔多斯盆地吴堡地区延长组烃源岩评价及特征. 兰州大学学报(自然科学版), 2012, 48(5):22-28. BAI Y B, LUO J L, ZHANG T J, et al. Characteristics and evaluation of source rocks of Yanchang Fomation in Wubao area, Ordos Basin. Journal of Lanzhou University(Natural Sciences), 2012, 48(5):22-28.
[19] SHU J, LEI C B, YUE W, et al.Hybrid plays of Upper Triassic Chang 7 lacustrine source rock interval of Yanchang Formation, Ordos Basin, China. Journal of Petroleum Science and Engineering, 2017, 33(9):182-196.
[20] 周庆凡, 杨国丰.致密油与页岩油的概念与应用.石油与天然气地质, 2012, 33(4):541-544. ZHOU Q F, YANG G F. Definition and application of tight oil and shale oil terms. Oil & Gas Geology, 2012, 33(4):541-544.
[21] PASSEY Q R, CREANEY S, KULLA J B, et al. Apractical model for organic richness from porosity and resistivity lods. AAPG Bulletin, 1990, 74(12):1777-1794.
[22] 黄晨, 潘保芝.利用测井资料识别与评价大庆外围盆地烃源岩.吉林大学学报(地球科学版), 2006, 36(4):163-165. HUANG C, PAN B Z.Using general log information to evaluate hydrcarbon source rocks of Basins in Daqing Periphery. Journal of Jilin University(Earth Science), 2006, 36(4):163-165.
[23] 朱振宇, 刘洪, 李幼铭, 等.ΔlogR技术在烃源岩识别中的应用与分析.地球物理学进展, 2003, 18(4):647-649. ZHU Z Y, LIU H, LI Y M, et al. The analysis and application of ΔlogR method in the source rock's identification. Progress in Geophysics, 2003, 18(4):647-649.
[24] 李相博, 刘显阳, 周世新, 等.鄂尔多斯盆地延长组下组合油气来源及成藏模式.石油勘探与开发, 2012, 39(2):172-180. LI X B, LIU X Y, ZHOU S X, et al. Hydrocarbon origin and reservoir forming model of the Lower Yanchang Formation, Ordos Basin. Petroleum Exploration and Development, 2012, 39(2):172-180.
[25] 中国石油天然气总公司.SY/T 5735-1995:陆相烃源岩地球化学评价方法.北京:石油工业出版社, 1995. China National Petroleum Corporation. SY/T 5735-1995:Geochemical evaluation of terrestrial source rock. Beijing:Petroleum Industry Press, 1995.
[26] 刘岩, 周文, 邓虎成.鄂尔多斯盆地上三叠统延长组含气页岩地质特征及资源评价.天然气工业, 2013, 33(3):19-23. LIU Y, ZHOU W, DENG H C. Geological characteristics of gas-bearing shales in the Yanchang Formation and its resource assessment in the Ordos Basin. Nature Gas Industry, 2013, 33(3):19-23.
[27] 陈建渝, 郝芳.有机岩石学研究有机质类型和成熟度的改进. 石油实验地质, 1990, 12(4):426-431. CHEN J Y, HAO F. Improvement on study of organic type and maturation with organic petrology. Petroleum Geology & Experiment, 1990, 12(4):426-431.
[28] 唐建云, 宋红霞, 陈玉宝, 等.鄂尔多斯盆地富黄探区延长组烃源岩评价.煤炭技术, 2016, 35(6):110-112. TANG J Y, SONG H X, CHEN Y B, et al. Hydrocarbon source evaluation of Yanchang group in Fu-Huang exploration area, Ordos Basin. Coal Technology, 2016, 35(6):110-112.
[29] 杨燕, 雷天柱, 关宝文, 等.滨浅湖相泥质烃源岩中不同赋存状态可溶有机质差异性研究.岩性油气藏, 2015, 27(2):77-82. YANG Y, LEI T Z, GUAN B W, et al. Differences of solvable organic matters with different occurrence states in argillaceous source rocks of coastal shallow-lake facie. Lithologic Reservoirs, 2015, 27(2):77-82.
[30] 邬立言, 顾信章.热解技术在我国生油岩研究中的应用. 石油学报, 1986, 7(2):13-19. WU L Y, GU X Z. The application of pyrolysis technique in source rocks research. Acta Petrolei Sinica, 1986, 7(2):13-19.
[31] 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.
[32] 刚文哲, 仵岳, 高岗, 等.渤海湾盆地南堡凹陷烃源岩地球化学特征与地质意义.石油实验地质, 2012, 34(2):57-61. GANG W Z, WU Y, GAO G, et al.Geochemical features and geologic significances of source rocks in Nanpu Sag, Bohai Bay Basin. Petroleum Geology & Experiment, 2012, 34(2):57-61.
[33] 任拥军, 周瑶琪, 查明, 等.东营凹陷古近系烃源岩成熟度特征.中国石油大学学报(自然科学版), 2006, 30(2):6-10. REN Y J, ZHOU Y Q, ZHA M, et al. Maturity of Lower Tertiary source rocks in Dongying Depression. Journal of China University of Petroleum(Edition of Natural Science), 2006, 30(2):6-10.
[34] PETERS K E, WALTERS C C, MOLDOWAN J M. The biomarker guide.Volume 2:Biomarkers and isotopes in petroleum exploration and earth history. Cambridge:Cambridge University Press, 2005.
[35] 高福红, 樊馥, 高红梅, 等.孙吴-嘉荫盆地太平林场组烃源岩生物标志化合物地球化学特征.中国石油大学学报(自然科学版), 2010, 37(4):38-45. GAO F H, FAN F, GAO H M, et al.Geochemical characteristics of biomarkers of source rocks from Taipinglinchang Formation in Sunwu-Jiayin Basin. Journal of China University of Petroleum(Edition of Natural Science), 2010, 37(4):38-45.
[36] 梅博文, 刘希江.我国原油中异戊间二烯烷烃的分布及其与地质环境的关系.石油与天然气地质, 1980, 1(2):99-115. MEI B W, LIU X J. The distribution of isoprene alkanes in China's crude oil and its relation with geologic environment. Oil & Gas Geology, 1980, 1(2):99-115.
[37] ANDREW D H, BRADLEY D R, MOLDOWAN J M.Organic geochemistry of oil and source rock strata of the Ordos Basin, north-central China. AAPG Bulletin, 2007, 91(9):1273-1293.
[38] 白玉彬, 赵靖舟, 高振东, 等.鄂尔多斯盆地杏子川油田长9烃源岩特征及油气勘探意义. 中国石油大学学报(自然科学版), 2013, 34(5):631-639. BAI Y B, ZHAO J Z, GAO Z D, et al. Characteristics of Chang 9 member source rocks and its significance of hydrocarbon exploration in Xingzichuan Oilfield, Ordos Basin. Journal of China University of Petroleum(Edition of Natural Science), 2013, 34(5):631-639.
[39] 白玉彬, 赵靖舟, 方朝强, 等.鄂尔多斯盆地长6油层组准连续型致密砂岩油藏形成机理. 石油实验地质, 2013, 35(1):65-71. BAI Y B, ZHAO J Z, FANG Z Q, et al. Forming mechanism of quasi-continuous tight sandstone reservoir of Chang 6 oil-bearing formation, Ordos Basin. Petroleum Geology & Experiment, 2013, 35(1):65-71.
[40] 陈建渝. 生物标志物地球化学的新进展. 地质科技情报, 1995, 14(1):35-44. CHEN J Y. New advances in geochemistry of biomarker. Geological Science and Technology Information, 1995, 14(1):35-44.
[41] 白玉彬, 赵靖舟, 赵子龙, 等.鄂尔多斯盆地志丹地区延长组长7致密油成藏条件与成藏特征.石油与天然气地质, 2013, 34(5):631-639. BAI Y B, ZHAO J Z, ZHAO Z L, et al. Accumulation conditions and characteristics of the Chang 7 tight oil reservoir of the the Yanchang Formation in Zhidan area, Ordos Basin. Oil & Gas Geology, 2013, 34(5):631-639.
[42] 白玉彬, 罗静兰, 王少飞, 等.鄂尔多斯盆地吴堡地区延长组长8致密砂岩油藏成藏主控因素. 中国地质, 2013, 40(4):1159-1167. BAI Y B, LUO J L, WANG S F, et al. The distribution of Chang-8 tight sandstone oil reservoir of Yanchang Formation in Wubao area, Central-south of Ordos Basin. Geology in China, 2013, 40(4):1159-1167.
[1] 赵军, 李勇, 文晓峰, 徐文远, 焦世祥. 基于斑马算法优化支持向量回归机模型预测页岩地层压力[J]. 岩性油气藏, 2024, 36(6): 12-22.
[2] 冉逸轩, 王健, 张熠. 松辽盆地北部中央古隆起基岩气藏形成条件与有利勘探区[J]. 岩性油气藏, 2024, 36(6): 66-76.
[3] 关蕴文, 苏思羽, 蒲仁海, 王启超, 闫肃杰, 张仲培, 陈硕, 梁东歌. 鄂尔多斯盆地南部旬宜地区古生界天然气成藏条件及主控因素[J]. 岩性油气藏, 2024, 36(6): 77-88.
[4] 白玉彬, 李梦瑶, 朱涛, 赵靖舟, 任海姣, 吴伟涛, 吴和源. 玛湖凹陷二叠系风城组烃源岩地球化学特征及页岩油“甜点”评价[J]. 岩性油气藏, 2024, 36(6): 110-121.
[5] 屈卫华, 田野, 董常春, 郭小波, 李立立, 林斯雅, 薛松, 杨世和. 松辽盆地德惠断陷白垩系烃源岩特征及其控藏作用[J]. 岩性油气藏, 2024, 36(6): 122-134.
[6] 王义凤, 田继先, 李剑, 乔桐, 刘成林, 张景坤, 沙威, 沈晓双. 玛湖凹陷西南地区二叠系油气藏相态类型及凝析油气地球化学特征[J]. 岩性油气藏, 2024, 36(6): 149-159.
[7] 乔桐, 刘成林, 杨海波, 王义凤, 李剑, 田继先, 韩杨, 张景坤. 准噶尔盆地盆1井西凹陷侏罗系三工河组凝析气藏特征及成因机制[J]. 岩性油气藏, 2024, 36(6): 169-180.
[8] 程焱, 王波, 张铜耀, 齐玉民, 杨纪磊, 郝鹏, 李阔, 王晓东. 渤中凹陷渤中A-2区新近系明化镇组岩性油气藏油气运移特征[J]. 岩性油气藏, 2024, 36(5): 46-55.
[9] 王子昕, 柳广弟, 袁光杰, 杨恒林, 付利, 王元, 陈刚, 张恒. 鄂尔多斯盆地庆城地区三叠系长7段烃源岩特征及控藏作用[J]. 岩性油气藏, 2024, 36(5): 133-144.
[10] 尹虎, 屈红军, 孙晓晗, 杨博, 张磊岗, 朱荣幸. 鄂尔多斯盆地东南部三叠系长7油层组深水沉积特征及演化规律[J]. 岩性油气藏, 2024, 36(5): 145-155.
[11] 杨海波, 冯德浩, 杨小艺, 郭文建, 韩杨, 苏加佳, 杨皩, 刘成林. 准噶尔盆地东道海子凹陷二叠系平地泉组烃源岩特征及热演化史模拟[J]. 岩性油气藏, 2024, 36(5): 156-166.
[12] 牟蜚声, 尹相东, 胡琮, 张海峰, 陈世加, 代林锋, 陆奕帆. 鄂尔多斯盆地陕北地区三叠系长7段致密油分布特征及控制因素[J]. 岩性油气藏, 2024, 36(4): 71-84.
[13] 段逸飞, 赵卫卫, 杨天祥, 李富康, 李慧, 王嘉楠, 刘钰晨. 鄂尔多斯盆地延安地区二叠系山西组页岩气源储特征及聚集规律[J]. 岩性油气藏, 2024, 36(3): 72-83.
[14] 卞保力, 刘海磊, 蒋文龙, 王学勇, 丁修建. 准噶尔盆地盆1井西凹陷石炭系火山岩凝析气藏的发现与勘探启示[J]. 岩性油气藏, 2024, 36(3): 96-105.
[15] 王宏波, 张雷, 曹茜, 张建伍, 潘星. 鄂尔多斯盆地二叠系盒8段河流扇沉积模式及勘探意义[J]. 岩性油气藏, 2024, 36(3): 117-126.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 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 .
[2] 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 .
[3] 林承焰, 谭丽娟, 于翠玲. 论油气分布的不均一性(Ⅰ)———非均质控油理论的由来[J]. 岩性油气藏, 2007, 19(2): 16 -21 .
[4] 王天琦, 王建功, 梁苏娟, 沙雪梅. 松辽盆地徐家围子地区葡萄花油层精细勘探[J]. 岩性油气藏, 2007, 19(2): 22 -27 .
[5] 王西文,石兰亭,雍学善,杨午阳. 地震波阻抗反演方法研究[J]. 岩性油气藏, 2007, 19(3): 80 -88 .
[6] 何宗斌,倪 静,伍 东,李 勇,刘丽琼,台怀忠. 根据双TE 测井确定含烃饱和度[J]. 岩性油气藏, 2007, 19(3): 89 -92 .
[7] 袁胜学,王 江. 吐哈盆地鄯勒地区浅层气层识别方法研究[J]. 岩性油气藏, 2007, 19(3): 111 -113 .
[8] 陈斐,魏登峰,余小雷,吴少波. 鄂尔多斯盆地盐定地区三叠系延长组长2 油层组沉积相研究[J]. 岩性油气藏, 2010, 22(1): 43 -47 .
[9] 徐云霞,王山山,杨帅. 利用沃尔什变换提高地震资料信噪比[J]. 岩性油气藏, 2009, 21(3): 98 -100 .
[10] 李建明,史玲玲,汪立群,吴光大. 柴西南地区昆北断阶带基岩油藏储层特征分析[J]. 岩性油气藏, 2011, 23(2): 20 -23 .