岩性油气藏 ›› 2023, Vol. 35 ›› Issue (1): 49–62.doi: 10.12108/yxyqc.20230105

• 地质勘探 • 上一篇    下一篇

渤海莱州湾凹陷中部古近系沙三段烃源岩地球化学特征及沉积环境

邓美玲1,2, 王宁1,2, 李新琦3, 陈容涛3, 刘岩1,2, 徐耀辉1,2   

  1. 1. 油气地球化学与环境湖北省重点实验室(长江大学 资源与环境学院)， 武汉 430100;
    2. 油气资源与勘探技术教育部重点实验室(长江大学)， 武汉 430100;
    3. 中海石油(中国)有限公司天津分公司 渤海石油研究院, 天津 300452
  • 收稿日期:2022-05-16 修回日期:2022-06-18 出版日期:2023-01-01 发布日期:2023-01-06
  • 第一作者:邓美玲(1997-),女,长江大学在读硕士研究生,研究方向为油气地球化学。地址:(430100)湖北省武汉市蔡甸区蔡甸街大学路111号。Email:873962517@qq.com
  • 通信作者: 王宁(1990-),女,博士,讲师,主要从事油气地球化学方面的教学与研究工作。Email:cupwangning@outlook.com。
  • 基金资助:
    中海油天津分公司项目“渤海海域中南部优质烃源岩特征及形成机理研究”(编号: CCL2020TJT0NST1956)资助

Geochemical characteristics and sedimentary environment of source rocks of the third member of Paleogene Shahejie Formation in central Laizhouwan Sag,Bohai Sea

DENG Meiling1,2, WANG Ning1,2, LI Xinqi3, CHEN Rongtao3, LIU Yan1,2, XU Yaohui1,2   

  1. 1. Hubei Key Laboratory of Petroleum Geochemistry and Environment (College of Resources and Environment, Yangtze University)， Wuhan 430100, China;
    2. Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education (Yangtze University)， Wuhan 430100, China;
    3. Research Institute of Bohai Petroleum, Tianjin Branch of CNOOC Ltd., Tianjin 300452, China
  • Received:2022-05-16 Revised:2022-06-18 Online:2023-01-01 Published:2023-01-06

PDF (PC)

265

摘要： 通过对渤海海域莱州湾凹陷中部古近系沙三段烃源岩样品的热解、TOC、饱和烃GC/MS分析以及主、微量元素分析，研究了其烃源岩的地球化学特征及沉积环境。研究结果表明: ①莱州湾凹陷中部古近系沙三段烃源岩有机质丰度差异较大，总体为好-优质烃源岩，有机质类型以Ⅰ-Ⅱ型为主，整体处于低熟-成熟阶段；②通过Pr/nC17-Ph/nC18图版、C24四环萜烷/C26三环萜烷 (C24TeT/C26TT) 、C27/C29规则甾烷、奥利烷指数等参数判断沙三段烃源岩有机质来源为低等水生生物和高等植物的混源输入；③综合CIA，Sr/Ba，Pr/Ph，V (/V+Ni)，U/Th值和伽马蜡烷指数等分析了烃源岩形成时期的古环境，认为沙三段沉积时期气候温暖湿润，降水丰富，水体为淡水-微咸水，陆源输入较多，具有较高的初始生产力，沉积时期整体表现为贫氧的弱氧化弱还原环境，沙三下段-沙三上段沉积环境整体变化不大，古气候和古水体盐度基本保持不变，但陆源输入及水体氧化条件随沉积进程呈逐渐增加的趋势。

关键词: 低熟-成熟烃源岩, 地球化学特征, 弱氧化弱还原环境, 陆源, 沙三段, 古近系, 莱州湾凹陷, 渤海

Abstract: The geochemical characteristics and sedimentary environment of the third member of Paleogene Shahejie Formation (E2s3) in central Laizhouwan Sag of Bohai Sea were studied by means of pyrolysis，TOC，GC/MS analysis of saturated hydrocarbons，and major and trace elements analysis of source rock samples. The results show that: (1) The source rocks of E2s3 have different organic matter abundances，they are generally good to high-quality source rocks. The organic matters are mainly type Ⅰ-Ⅱ and in the low mature to mature stage as a whole. (2) According to Pr/nC17-Ph/nC18 plates，C24 tetracyclic terpanes/C26 tricyclic terpanes (C24 TeT/C26 TT)， C27/C29 regular sterane and olliane index，it can be concluded that the organic matters of E2s3 source rocks are derived from mixed inputs of lower aquatic organisms and terrigenous higher plants. (3) CIA，Sr/Ba，Pr/Ph，V (/V+Ni)， U/Th and gammacerane index were used to analyze the paleoenvironment of the source rocks. During the sedimentary period of E2s3，the climate was warm and humid with abundant precipitation. The water environment was fresh-brackish water，accompanied by strong terrigenous input，with high initial productivity，and the sedimentary environment is weak oxidation and weak reduction environment with poor oxygen. The sedimentary environment of E2s3 has little change，and the paleoclimate and water salinity are basically the same. However，terrigenous input and water oxidation conditions gradually increase with the deposition.

Key words: low mature to mature source rocks, geochemical characteristics, weak oxidation and reduction environment, terrigenous, the third member of Shahejie Formation, Paleogene, Laizhouwan Sag, Bohai Sea

中图分类号: 

  • TE122.114
[1] HAO Fang,ZHOU Xinhai,ZHU Yangming,et al. Lacustrine source rock deposition in response to co-evolution of environments and organisms controlled by tectonic subsidence and climate, Bohai Bay Basin,China[J]. Organic Geochemistry,2011,42 (4): 323-339.
[2] 潘文静,杜晓峰,田德瑞,等.渤海莱州湾凹陷烃源岩特征及形成机理分析[J].中国海上油气,2019,31 (6): 60-68. PAN Wenjing,DU Xiaofeng,TIAN Derui,et al. Characteristics and formation mechanism of source rocks in the Laizhou Bay Sag of Bohai Sea[J]. China Offshore Oil and Gas,2019,31 (6): 60-68.
[3] ZHAO Zibin,HOU Dujie,CHENG Xiong,et al. Geochemical and palynological characteristics of the Paleogene source rocks in the northeastern Laizhouwan Sag,Bohai Bay Basin,China: Hydrocarbon potential,depositional environment,and factors controlling organic matter enrichment[J]. Marine and Petroleum Geology,2020,124: 104792.
[4] WANG Feilong,TANG Guomin,WANG Deying,et al. Paleoenvironmental characteristics and evidence of subsag migration within the Laizhouwan Sag in the Bohai Sea[J]. Journal of Petroleum Science and Engineering,2021,210 (6): 109961.
[5] 陈亚军,荆文波,宋小勇,等. 三塘湖盆地马朗凹陷上石炭统沉积岩层地球化学特征及古环境意义[J]. 岩性油气藏, 2021,33 (4): 63-75. CHEN Yajun,JING Wenbo,SONG Xiaoyong,et al. Geochemical characteristics and paleoenvironmental significance of Upper Carboniferous sedimentary strata in Malang Sag,Santanghu Basin[J]. Lithologic Reservoirs,2021,33 (4): 63-75.
[6] 黄彦杰,白玉彬,孙兵华,等. 鄂尔多斯盆地富县地区延长组长 7烃源岩特征及评价[J]. 岩性油气藏,2020,32 (1): 66-75. HUANG Yanjie,BAI Yubin,SUN Binghua,et al. Characteristics and evaluation of Chang 7 source rock of Yanchang Formation in Fuxian area,Ordos Basin[J]. Lithologic Reservoirs,2020,32 (1): 66-75.
[7] 杨海风,涂翔,赵弟江,等.渤海湾盆地莱州湾凹陷沙河街组第三、第四段烃源岩有机相特征[J].成都理工大学学报 (自然科学版)，2021,48 (1): 72-81. YANG Haifeng,TU Xiang,ZHAO Dijiang,et al. Organic facies characteristics of source rocks of the third and fourth members of Shahejie Formation in the southern Laizhouwan Depression, Bohai Bay Basin,China[J]. Journal of Chengdu University of Technology (Science & Technology Edition)，2021,48 (1): 72-81.
[8] 汤国民,王飞龙,王清斌,等.渤海海域莱州湾凹陷高硫稠油成因及其成藏模式[J].石油与天然气地质,2019,40 (2): 284-293. TANG Guomin,WANG Feilong,WANG Qingbin,et al. Genesis and accumulation models of sulfur-rich heavy oil in Laizhou Bay Sag,Bohai Sea[J]. Oil & Gas Geology,2019,40 (2): 284-293.
[9] 王根照,牛成民,王亮,等.莱州湾凹陷勘探突破的启示[J].石油天然气学报,2012,34 (5): 39-43. WANG Genzhao,NIU Chengmin,WANG Liang,et al. Enlightenment of exploration breakthrough in Laizhouwan Depression[J]. Journal of Oil and Gas Technology,2012,34 (5): 39-43.
[10] 牛成民.渤海南部海域莱州湾凹陷构造演化与油气成藏[J]. 石油与天然气地质,2012,33 (3): 424-431. NIU Chengmin. Tectonic evolution and hydrocarbon accumulation of Laizhouwan depression in southern Bohai Sea[J]. Oil & Gas Geology,2012,33 (3): 424-431.
[11] 蔡东升,罗毓晖,姚长华.渤海莱州湾走滑拉分凹陷的构造研究及其石油勘探意义[J].石油学报,2001,22 (2): 19-25. CAI Dongsheng,LUO Yuhui,YAO Changhua. Structural study and petroleum exploration significance of strike-slip pull-apart sag in Laizhou Bay,Bohai Sea[J]. Acta Petrolei Sinica,2001, 22 (2): 19-25.
[12] 彭文绪,辛仁臣,孙和风,等.渤海海域莱州湾凹陷的形成和演化[J].石油学报,2009,30 (5): 654-660. PENG Wenxu,XIN Renchen,SUN Hefeng,et al. Formation and evolution of Laizhou Bay Sag in Bobai Bay[J]. Acta Petrolei Sinica,2009,30 (5): 654-660.
[13] 庞雄奇,郭永华,姜福杰,等.渤海海域优质烃源岩及其分布预测[J].石油与天然气地质,2009,30 (4): 393-397. PANG Xiongqi,GUO Yonghua,JIANG Fujie,et al. High-quality source rocks and their distribution prediction in the Bohai Sea waters[J]. Oil & Gas Geology,2009,30 (4): 393-397.
[14] 薛永安,杨海风,王航,等.渤海莱州湾凹陷深洼带垦利10-2新近系大型油田发现与意义[J].中国海上油气,2022,34 (1): 17-26. XUE Yongan,YANG Haifeng,WANG Hang,et al. Discovery and significance of KL10-2 Neogene large oilfield in deep subsag zone of Laizhouwan Sag,Bohai Sea[J]. China Offshore Oil and Gas,2022,34 (1): 17-26.
[15] 周连德,孙风涛,来又春,等.渤海莱州湾凹陷KL油田沙河街组混积背景下的沉积特征与沉积演化[J].中国海洋大学学报 (自然科学版)，2019,49 (9): 110-120. ZHOU Liande,SUN Fengtao,LAI Youchun,et al. Sedimentary characteristics and sedimentary evolution in mix sediments background of Shahejie Formation in KL oilfield,Laizhou Bay Depression,Bohai Bay Basin[J]. Periodical of Ocean University of China (Natural Science Edition)，2019,49 (9): 110-120.
[16] 汤国民,王飞龙,万琳,等.渤海海域莱州湾凹陷油源特征及原油成因类型[J].西安石油大学学报 (自然科学版)，2021,36 (1): 28-36. TANG Guomin,WANG Feilong,WAN Lin,et al. Characteristics of oil source and genetic types of crude oil in Laizhouwan Depression,Bohai Sea[J]. Journal of Xi'an Shiyou University (Natural Science Edition)，2021,36 (1): 28-36.
[17] 赵汉卿,温慧芸,穆朋飞,等.垦利A油田沙三上段近源辫状河三角洲沉积特征[J].岩性油气藏,2019,31 (3): 37-44. ZHAO Hanqing,WEN Huiyun,MU Pengfei,et al. Sedimentary characteristics of near-source braided river delta of the upper third member of Shahejie Formation in Kenli A oilfield[J]. Lithologic Reservoirs,2019,31 (3): 37-44.
[18] 牛成民,杨海风,赵弟江,等.渤海海域莱州湾凹陷油气超晚期成藏与油气运移滞后效应[J].地球科学,2022,47 (2): 464-478. NIU Chengmin,YANG Haifeng,ZHAO Dijiang,et al. Study on the ultra-late hydrocarbon accumulation and migration lagging effect in Laizhouwan Sag,Bohai Sea[J]. Earth Science,2022, 47 (2): 464-478.
[19] 李坤,董柔,徐国盛,等.莱州湾凹陷新生代走滑-伸展叠合断裂体系发育演化模式[J].成都理工大学学报 (自然科学版)， 2021,48 (1): 12-22. LI Kun,DONG Rou,XU Guosheng,et al. The development and evolution model of Cenozoic strike slip extension superposed fault system in Laizhou Bay Sag,China[J]. Journal of Chengdu University of Technology (Science & Technology Edition)， 2021,48 (1): 12-22.
[20] 中国国家标准化管理委员会.气相色谱-质谱法测定沉积物和原油中生物标志物: GB/T 18606-2017[S]. 北京: 中国标准出版社,2017. Standardization Administration of the People's Republic of China. The test method for biomarkers in sediment and crude oil by GCMS: GB/T 18606-2017[S]. Beijing: Standards Press of China, 2017.
[21] 中国国家标准化管理委员会.硅酸盐岩石化学分析方法 (第28部分: 16个主次成分量测定): GB/T 14506.28-2010[S]. 北京: 中国标准出版社,2010. Standardization Administration of the People's Republic of China. Methods for chemical analysis of silicate rocks-Part 28: Determination of 16 major and minor elements content: GB/T 14506.28- 2010[S]. Beijing: Standards Press of China,2010.
[22] 中国国家标准化管理委员会.硅酸盐岩石化学分析方法 (第30部分: 44个元素量测定): GB/T 14506.30-2010[S].北京: 中国标准出版社,2010. Standardization Administration of the People's Republic of China. Methods for chemical analysis of silicate rocks-Part 30: Determination of 44 elements: GB/T 14506.30-2010[S]. Beijing: Standards Press of China,2010.
[23] 侯读杰,冯子辉.油气地球化学[M].北京: 石油工业出版社, 2011. HOU Dujie,FENG Zihui. Petroleum geochemistry[M]. Beijing: Petroleum Industry Press,2011.
[24] 国家能源局. 烃源岩地球化学评价方法: SY/T 5735-2019[S].北京: 石油工业出版社,2019. National Energy Administration. Geochemical evaluation method for source rocks: SY/T 5735—2019[S]. Beijing: Petroleum Industry Press,2019.
[25] 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[J].岩性油气藏,2018,30 (1): 39-45. YUAN Yuan,DU Kefeng,GE Yunjin,et al. Geochemistry of hydrocarbon source rocks of Chang 7 in Ganquan-Fuxian area, Ordos Basin[J]. Lithologic Reservoirs,2018,30 (1): 39-45.
[26] 张小琴,李威,王飞龙,等.辽东湾地区古近系烃源岩生物标志物特征及其地质意义[J].岩性油气藏,2022,34 (1): 73-85. ZHANG Xiaoqin,LI Wei,WANG Feilong,et al. Biomarker characteristics and geological significance of Paleogene source rocks in Liaodong Bay[J]. Lithologic Reservoirs,2022,34 (1): 73-85.
[27] 王铁冠,钟宁宁,熊波,等.源岩生烃潜力的有机岩石学评价方法[J].石油学报,1994,15 (4): 9-16. WANG Tieguan,ZHONG Ningning,XIONG Bo,et al. Organic petrological evaluation method for hydrocarbon generation potential of source rocks[J]. Acta Petrolei Sinica,1994,15 (4): 9-16.
[28] 邬立言. 生油岩热解快速定量评价[M]. 北京: 科学出版社, 1986. WU Liyan. Rapid and quantitative evaluation of source rock pyrolysis[M]. Beijing: Science Press,1986.
[29] MACKENZIE A S,PATIENCE R L,MAXWELL J R,et al. Molecular parameters of maturation in the Toarcian shales,Paris Basin,France—Ⅰ. Changes in the configurations of acyclic isoprenoid alkanes,steranes and triterpanes[J]. Geochimica et Cosmochimica Acta,1980,44 (11): 1709-1721.
[30] PETERS K E,WALTERS C C,MOLDOWAN J M. The biomarker guide,biomarkers and isotopes in petroleum exploration and earth history[M]. 2nd ed. New York: Cambridge University Press,2005.
[31] 邓宏文,钱凯.沉积地球化学与环境分析[M].兰州: 甘肃科学技术出版社,1993: 1-150. DENG Hongwen,QIAN Kai. Sedimentary geochemistry and environmental analysis[M]. Lanzhou: Gansu Science and Technology Press,1993: 1-150.
[32] 许涛. 不同环境样品生物标志化合物的气候环境意义[D]. 兰州: 兰州大学,2008. XU Tao. Climatic and environmental significance of biomarkers from different environmental samples[D]. Lanzhou: Lanzhou University,2008.
[33] SEIFERT W K,MOLDOWAN J M. Use of biological markers in petroleum exploration[J]. Methods in Geochemistry and Geophysics,1986,24: 261-290.
[34] BRAY E E,EVANS E D. Distribution of n-paraffins as a clue to recognition of source beds[J]. Geochimica et Cosmochimica Acta,1961,22 (1): 2-15.
[35] HAO Fang,ZHOU Xinhai,ZHU Yangming,et al. Changing of the Neogene Penglai 19-3 field,Bohai Bay Basin,China oil accumulation in a young trap in an active fault zone[J]. AAPG Bulletin,2009,93 (2): 155-179.
[36] HAO Fang,ZHOU Xinhai,ZHU Yangming,et al. Mechanisms for oil depletion and enrichment on the Shijiutuo uplift,Bohai Bay Basin,China[J]. AAPG Bulletin,2009,93 (8): 1015-1037.
[37] 王亮,牛成民,杨波,等.莱州湾凹陷沙三段含油气系统与有利勘探方向[J].断块油气田,2011,18 (5): 545-548. WANG Liang,NIU Chengmin,YANG Bo,et al. Petroleum system and favorable exploration targets of the third member of Shahejie Formation in Laizhouwan Depression[J]. Fault-Block Oil & Gas Field,2011,18 (5): 545-548.
[38] MOLDOWAN J M,DAHL J,BRADLEY J,HUIZINGA B J,et al. The molecular fossil record of oleanane and its relation to angiosperms[J]. Science,1994,265 (5173): 768-771.
[39] 王铁玲.奥利烷在沉积物和原油中的分布及其地球化学意义[J].石油天然气学报,2011,33 (7): 13-18. WANG Tieling. The distribution of oleananes in sediments and oils and their geochemical significance[J]. Journal of Oil and Gas Technology,2011,33 (7): 13-18.
[40] HUANG Wenyen,MEINSCHEIN W G. Sterols as ecological indicators[J]. Geochimica et Cosmochimica Acta,1979,43 (5): 739-745.
[41] 孟凡巍,周传明,燕夔,等.通过C27/C29甾烷和有机碳同位素来判断早古生代和前寒武纪的烃源岩的生物来源[J].微体古生物学报,2006,23 (1): 51-56. MENG Fanwei,ZHOU Chuanming,YAN Kui,et al. Biological origin of early Paleozoic and Precambrian hydrocarbon source rocks based on C27/C29 sterane ratio and organic carbon isotope[J]. Acta Micropalaeontologica Sinica,2006,23 (1): 51-56.
[42] 傅家谟,徐芬芳,陈德玉,等.茂名油页岩中生物输入的标志化合物[J].地球化学,1985,14 (2): 99-114. FU Jiamo,XU Fenfang,CHEN Deyu,et al. Biomarker composition of biological inputs in Maoming oil shale[J]. Geochimica, 1985,14 (2): 99-114.
[43] NESBITT H W,YOUNG G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature,1982,299 (5885): 715-717.
[44] FEDO C M,NESBITT H W,YOUNG G M. Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols,with implications for paleoweathering conditions and provenance[J]. Geology,1995,23 (10): 921-924.
[45] ROY D K,ROSER B P. Climatic control on the composition of Carboniferous-Permian Gondwana sediments,Khalaspir Basin, Bangladesh[J]. Gondwana Research,2013,23 (3): 1163-1171.
[46] 刁帆,邹华耀,郝芳,等.渤海湾盆地廊固凹陷烃源岩特征及其发育模式[J].石油与天然气地质,2014,35 (3): 326-335. DIAO Fan,ZOU Huayao,HAO Fang,et al. Characteristics and depositional models of source rocks in Langgu Sag,Bohai Bay Basin[J]. Oil & Gas Geology,2014,35 (3): 326-335.
[47] 李被,刘池洋,黄雷,等.东濮凹陷北部沙河街组三段中亚段沉积环境分析[J].现代地质,2018,32 (2): 227-239. LI Bei,LIU Chiyang,HUANG Lei,et al. Analysis of the sedimentary environment in the north of Dongpu Depression during the deposition of the middle section of the third member of the Shahejie Formation[J]. Geoscience,2018,32 (2): 227-239.
[48] 黄梓桑,王兴志,杨西燕,等.沉积环境对页岩中有机质富集的约束: 以蜀南地区五峰组-龙马溪组为例[J]. 沉积学报, 2021,39 (3): 631-644. HUANG Zisang,WANG Xingzhi,YANG Xiyan,et al. Constraints of sedimentary environment on organic matter accumulation in shale: A case study of the Wufeng-Longmaxi Formations in the southern Sichuan Basin[J]. Acta Sedimentologica Sinica,2021,39 (3): 631-644.
[49] PIPER D Z. Seawater as the source of minor elements in black shales,phosphorites and other sedimentary rocks[J]. Chemical Geology,1994,114 (1/2): 95-114.
[50] 李成凤,肖继风.用微量元素研究胜利油田东营盆地沙河街组的古盐度[J].沉积学报,1988,6 (4): 100-107. LI Chengfeng,XIAO Jifeng. Study on paleosalinity of Shahejie Formation in Dongying Basin of Shengli Oilfield by trace elements[J]. Acta Sedimentologica Sinica,1988,6 (4): 100-107.
[51] JONES B,MANNING D A C. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J]. Chemical Geology,1994,111 (1/2/3/4): 111-129.
[52] 张参,阳宏,王飞龙,等. 渤中凹陷南洼东营组烃源岩有机地球化学特征[J].海洋地质前沿,2020,36 (11): 35-44. ZHANG Can,YANG Hong,WANG Feilong,et al. Organic geochemistry of the source rocks in the Dongying Formation of the south Bozhong subsag[J]. Marine Geology Frontiers,2020,36 (11): 35-44.
[1] 周自强, 朱正平, 潘仁芳, 董於, 金吉能. 基于波形相控反演的致密砂岩储层模拟预测方法——以黄骅坳陷沧东凹陷南部古近系孔二段为例[J]. 岩性油气藏, 2024, 36(5): 77-86.
[2] 张磊, 李莎, 罗波波, 吕伯强, 谢敏, 陈新平, 陈冬霞, 邓彩云. 东濮凹陷北部古近系沙三段超压岩性油气藏成藏机理[J]. 岩性油气藏, 2024, 36(4): 57-70.
[3] 朱康乐, 高岗, 杨光达, 张东伟, 张莉莉, 朱毅秀, 李婧. 辽河坳陷清水洼陷古近系沙河街组深层烃源岩特征及油气成藏模式[J]. 岩性油气藏, 2024, 36(3): 146-157.
[4] 西智博, 廖建平, 高荣锦, 周晓龙, 雷文文. 辽河坳陷陈家断裂带北部构造演化解析及油气成藏[J]. 岩性油气藏, 2024, 36(3): 127-136.
[5] 冯斌, 黄晓波, 何幼斌, 李华, 罗进雄, 李涛, 周晓光. 渤海湾盆地庙西北地区古近系沙河街组三段源-汇系统重建[J]. 岩性油气藏, 2024, 36(3): 84-95.
[6] 方旭庆, 钟骑, 张建国, 李军亮, 孟涛, 姜在兴, 赵海波. 渤海湾盆地沾化凹陷古近系沙三下亚段旋回地层学分析及地层划分[J]. 岩性油气藏, 2024, 36(3): 19-30.
[7] 刘仁静, 陆文明. 断块油藏注采耦合提高采收率机理及矿场实践[J]. 岩性油气藏, 2024, 36(3): 180-188.
[8] 王亚, 刘宗宾, 路研, 王永平, 刘超. 基于SSOM的流动单元划分方法及生产应用——以渤海湾盆地F油田古近系沙三中亚段湖底浊积水道为例[J]. 岩性油气藏, 2024, 36(2): 160-169.
[9] 牛成民, 惠冠洲, 杜晓峰, 官大勇, 王冰洁, 王启明, 张宏国. 辽中凹陷西斜坡古近系东三段湖底扇发育模式及大油田发现[J]. 岩性油气藏, 2024, 36(2): 33-42.
[10] 李二庭, 米巨磊, 张宇, 潘越扬, 迪丽达尔·肉孜, 王海静, 高秀伟. 准噶尔盆地东道海子凹陷二叠系平地泉组烃源岩特征[J]. 岩性油气藏, 2024, 36(1): 88-97.
[11] 郭谨豪, 胡国艺, 何坤, 米敬奎, 田连杰, 贺飞, 郭楚媛, 卢梦蝶. 川北地区二叠系大隆组烃源岩地球化学特征及沉积环境[J]. 岩性油气藏, 2023, 35(5): 139-152.
[12] 李盛谦, 曾溅辉, 刘亚洲, 李淼, 焦盼盼. 东海盆地西湖凹陷孔雀亭地区古近系平湖组储层成岩作用及孔隙演化[J]. 岩性油气藏, 2023, 35(5): 49-61.
[13] 胡望水, 高飞跃, 李明, 郭志杰, 王世超, 李相明, 李圣明, 揭琼. 渤海湾盆地廊固凹陷古近系沙河街组油藏单元精细表征[J]. 岩性油气藏, 2023, 35(5): 92-99.
[14] 徐中波, 汪利兵, 申春生, 陈铭阳, 甘立琴. 渤海蓬莱19-3油田新近系明下段曲流河储层构型表征[J]. 岩性油气藏, 2023, 35(5): 100-107.
[15] 姚秀田, 王超, 闫森, 王明鹏, 李婉. 渤海湾盆地沾化凹陷新生界断层精细表征及地质意义[J]. 岩性油气藏, 2023, 35(4): 50-60.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 庞雄奇, 陈冬霞, 张　俊. 隐蔽油气藏的概念与分类及其在实际应用中需要注意的问题[J]. 岩性油气藏, 2007, 19(1): 1 -8 .
[2] 雷卞军，张吉，王彩丽，王晓蓉，李世临，刘斌. 高分辨率层序地层对微相和储层的控制作者用——以靖边气田统5井区马五段上部为例[J]. 岩性油气藏, 2008, 20(1): 1 -7 .
[3] 杨杰，卫平生，李相博. 石油地震地质学的基本概念、内容和研究方法[J]. 岩性油气藏, 2010, 22(1): 1 -6 .
[4] 王延奇，胡明毅，刘富艳，王辉，胡治华. 鄂西利川见天坝长兴组海绵礁岩石类型及礁体演化阶段[J]. 岩性油气藏, 2008, 20(3): 44 -48 .
[5] 代黎明, 李建平, 周心怀, 崔忠国, 程建春. 渤海海域新近系浅水三角洲沉积体系分析[J]. 岩性油气藏, 2007, 19(4): 75 -81 .
[6] 段友祥, 曹婧, 孙歧峰. 自适应倾角导向技术在断层识别中的应用[J]. 岩性油气藏, 2017, 29(4): 101 -107 .
[7] 黄龙，田景春，肖玲，王峰. 鄂尔多斯盆地富县地区长6砂岩储层特征及评价[J]. 岩性油气藏, 2008, 20(1): 83 -88 .
[8] 杨仕维，李建明. 震积岩特征综述及地质意义[J]. 岩性油气藏, 2008, 20(1): 89 -94 .
[9] 李传亮，涂兴万. 储层岩石的2种应力敏感机制——应力敏感有利于驱油[J]. 岩性油气藏, 2008, 20(1): 111 -113 .
[10] 李君, 黄志龙, 李佳, 柳波. 松辽盆地东南隆起区长期隆升背景下的油气成藏模式[J]. 岩性油气藏, 2007, 19(1): 57 -61 .

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