天然气地球科学

• 天然气地球化学 • 上一篇    

柴达木盆地西部咸水湖相沉积有机质中二苯并噻吩类组成特征及环境意义

周叶骏,关平,吴颜雄,刘沛显,丁晓楠,谭宇,庞磊
 
  

  1. 1.北京大学地球与空间科学学院石油与天然气研究中心,北京100871;
    2.中国石油青海油田分公司,甘肃 敦煌 736202
  • 收稿日期:2018-03-16 修回日期:2018-05-28 出版日期:2018-06-10 发布日期:2018-06-10
  • 通讯作者: 关平(1960-),男,江苏南京人,教授,主要从事沉积学与沉积地球化学研究. E-mail:pguanl@pku.edu.cn.
  • 作者简介:周叶骏(1992-),男,江苏苏州人,硕士研究生,主要从事石油地质学与有机地球化学研究.E-mail:1501210272@pku.edu.cn.

Characterization on the composition of dibenzothiophene series in saline lacustrine sediments in western Qaidam Basin and its environmental implications

Zhou Ye-Jun,Guan Ping,Wu Yan-xiong,Liu Pei-Xian,Ding Xiao-Nan,Tan Yu,Pang Lei
  

  1. 1.Institute of Oil and Gas,School of Earth and Space Sciences,Peking University,Beijing 100871,China;
    2.PetroChina Qinghai Oilfield Company,Dunhuang 736202,China
  • Received:2018-03-16 Revised:2018-05-28 Online:2018-06-10 Published:2018-06-10

摘要: 对柴达木盆地西部地区新生代的原油及烃源岩样品中有机质进行饱和烃与芳烃馏分的色谱—质谱分析。在验证样品为沉积相以咸水湖相为主的多物源沉积的基础上,对于沉积有机质中包含的二苯并噻吩及其衍生物的含量及分布特征进行研究,并探索中低成熟度下热演化程度和沉积环境因素对于二苯并噻吩类异构体甲基重排作用及烷基化程度的影响。研究表明,前人研究中使用的一些用以判别成熟度的二苯并噻吩类异构体的比值参数,在中低成熟度条件下受沉积环境因素影响较大,如4-甲基二苯并噻吩/1-甲基二苯并噻吩(MDR)等指标可能会受盐度控制而增大,对有机质成熟度并无指示意义;二苯并噻吩类的烷基化程度可以作为区分咸水湖相、海相、淡水湖相等的参考指标,并在一定程度上表征沉积时的盐度,高盐度使烷基化程度更高。

关键词: 二苯并噻吩, 烷基化, 甲基重排, 柴达木盆地, 新生代

Abstract: The Cenozoic crude oil and source rock samples from western Qaidam Basin were collected,and the gas chromatgraphy-mass spectrometry (GC-MS) analysis of saturated hydrocarbon and aromatic components was conducted.The samples were proved to be mainly deposited in saline lacustrine environment with multiple depositional sources.Further,the composition characteristics of dibenzothiophene series were investigated,and the influence of thermal maturity and depositional environment on the alkylate and alkyl rearrangement effect of dibenzothiophene series was discussed for the low-to-medium maturity stages.As the results indicated,some parameters of the ratios of dibenzothiophene isomers,which were widely used to analyze the maturity stages in previous studies,are largely affected by depositional environment at low-to-medium maturity stages.The ratio of 4-MDBT/1-MDBT (MDR) can be enlarged with higher salinity,while may not be indicative of the maturity stages of the organic matter.The degree of alkylate of the dibenzothiophene series can be referred as an indicator to distinguish among saline lacustrine,fresh water lacustrine and marine facies,where the higher alkylate degree could have arisen from the higher salinity.

Key words: Dibenzothiophene, Alkylate, Alkyl rearrangement, Qaidam Basin, Cenozoic

中图分类号: 

  • TE122.1+13

[1]Wu Zhijun,Luo Binjie,Wang Youxiao,et al.Distribution of dibenzothiophenes in crude oils from Tarim Basin and identification of major source rock types[J].Acta Sedimentologica Sinica,1995,13(3):98-106.[ZK)]
[ZK(3#]吴治君,罗斌杰,王有孝,等.塔里木盆地原油中二苯并噻吩的分布及主力油源岩类型判识[J].沉积学报,1995,13(3):98-106.
[2]Damste J S S,De Leeuw J W.Analysis,structure and geochemical significance of organically-bound sulphur in the geosphere:State of the art and future research[J].Organic Geochemistry,1990,16(4):1077-1101.
[3]Song Zhiguang,Wang Maochun,Liu Zufa.Thermal evolution of typical organic sulfur compounds studied by hydrous pyrolysis[J].Geochimica,2007,36(3):247-252.
宋之光,王茂春,刘祖发.典型有机硫化合物热演化的加水热解实验研究[J].地球化学,2007,36(3):247-252.
[4]Hughes W B.Use of thiophenic organosulfur compounds in characterizing crude oils derived from carbonate versus siliciclastic sources[C]//Palacas J G.Petroleum Geochemisty and Source Rock Potential of Carbonate Rocks.Tulsa:Okahoma.AAPG Studies in Geology,1984:181-196.
[5]Radke M,Welte D H,Willsch H.Maturity parameters based on aromatic hydrocarbons:Influence of the organic matter type[J].Organic Geochemistry,1986,10(1/3):51-63.
[6]Fan P,Philip R P,Li Z X,et al.Geochemical characteristics of aromatic hydrocarbons of crude oils and source rocks from different sedimentary environments[J].Organic Geochemistry,1990,16(1):427-435.
[7]Ying Guangguo,Fan Pu.Geochemistry of aromatic hydrocarbons in Sunniland oils and source rocks in the South Florida Basin,USA[J].Acta Sedimentologica Sinica,1992,10(2):127-134.
应光国,范璞.美国Sunniland等地原油和油源岩中噻吩类化合物的对比研究[J].沉积学报,1992,10(2):127-134.
[8]Li Shuifu,He Sheng.Geochemical characteristics of dibenzathiophene,dibenzofuran and fluorine and their homologues and their environmental indication[J].Geochimica,2008,37(1):45-50.
李水福,何生.原油芳烃中三芴系列化合物的环境指示作用[J].地球化学,2008,37(1):45-50.
[9]Hughes W B,Holba A G,Dzou L I P.The ratios of dibenzothiophene to phenanthrene and pristane to phytane as indicators of depositional environment and lithology of petroleum source rocks[J].Geochimica et Cosmochimica Acta,1995,59(17):3581-3598.
[10]Chakhmakhchev A,Suzuki N.Saturate biomarkers and aromatic sulfur compounds in oils and condensates from different source rock lithologies of Kazakhstan,Japan and Russia[J].Organic Geochemistry,1995,23(4):289-299.
[11]Chakhmakhchev A,Suzuki M,Takayama K.Distribution of alkylated dibenzothiophenes in petroleum as a tool for maturity assessments[J].Organic Geochemistry,1997,26(7):483-489.
[12]Schou L,Myhr M B.Sulfur aromatic compounds as maturity parameters[C]//Mattavelli L,Novelli L.Organic Geochemistry in Petroleum Exploration.Amsterdam:Elsevier,1988:61-66.
[13]Zhang Runhe,Yang Bin.Thiophene compound:An ideal biological marker to distinguish marine crude oil type and evaluate maturity of carbonate source rock with high maturity[J].Marine Origin Petroleum Geology,1998,3(2):6-10.
张润合,杨斌.噻吩类化合物——判识海相原油类型和评价高演化碳酸盐岩烃源岩成熟度的理想生物标志物[J].海相油气地质,1998,3(2):6-10.
[14]Li Jinggui.Research development and prospect of maturity parameters of methylated dibenzothiophenes in marine carbonate rocks[J].Acta Sedimentologica Sinica,2000,18(3):480-483.
李景贵.海相碳酸盐岩二苯并噻吩类化合物成熟度参数研究进展与展望[J].沉积学报,2000,18(3):480-483.
[15]Wei Zhibin,Zhang Dajiang,Zhang Chuanlu,et al.Methyldibenzothiophenes distribution index as a tool for maturity assessments of source rocks[J].Geochimica,2001,30(3):242-247.
魏志彬,张大江,张传禄,等.甲基二苯并噻吩分布指数(MDBI)作为烃源岩成熟度标尺的探讨[J].地球化学,2001,30(3):242-247.
[16]Wang Tieguan,He Faqi,Li Meijun,et al.Methyldibenzothiophene series:Molecular marker to spike the filling pathway of oil[J].Chinese Science Bulletin,2005,50(2):176-182.
王铁冠,何发岐,李美俊,等.烷基二苯并噻吩类:示踪油藏充注途径的分子标志物[J].科学通报,2005,50(2):176-182.
[17]Li Meijun,Wang Tieguan,Liu Ju,et al.Application of using the total amount of methyldibenzothiophenes to spike the filling pathway of oil in Fushan Sag[J].Science in China:Series D,2008,38(supplement 1):122-138.
李美俊,王铁冠,刘菊,等.烷基二苯并噻吩总量示踪福山凹陷凝析油藏充注途径[J].中国科学:D辑,2008,38(增刊1):122-138.
[18]Xu Yaohui,Wang Tieguan,Chen Nengxue,et al.DBT parameters and dynamic monitoring during reservoir development,and distribution region prediction of remaining oil:A case study on the Sha-33 oil reservoir in the Liubei region,Nanpu sag[J].Science in China:Series D,2013,43(7):1141-1148.
徐耀辉,王铁冠,陈能学,等.二苯并噻吩参数与油藏动态监测,剩余油分布预测——以南堡凹陷柳北沙三—3油藏为例[J].中国科学:D辑,2013,43(7):1141-1148.
[19]Zhang Min,Zhang Jun.Composition characteristics and geochemical significance of thiophene-type compounds for crude oils in Tarim Basin[J].Acta Sedimentologica Sinica,1999,17(1):120-126.
张敏,张俊.塔里木盆地原油噻吩类化合物的组成特征及地球化学意义[J].沉积学报,1999,17(1):120-126.
[20]Jiang Naihuang,Zhu Guangyou,Zhang Shuichang,et al.The content of methyldibenzothiophenes in oil and its relationship with depositional environment and catagenesis[J].Earth Science Frontiers,2008,15(2):186-194.
姜乃煌,朱光有,张水昌,等.原油似甲基二苯并噻吩含量与沉积环境及次生变化的关系[J].地学前缘,2008,15(2):186-194.
[21]Xu Daqing.Establishment and application of GC-PFPD analytical method forthiophenic compounds[J].Petroleum Geology & Experiment,2010,32(3):301-304.
徐大庆.噻吩类化合物 GC-PFPD 分析方法的建立及应用[J].石油实验地质,2010,32(3):301-304.
[22]Shi Shengbao,Li Meijun,Zhu Lei.Identification and distribution of C1- and C2-alkylated dibenzothiophenes in petroleum and sedimentary organic matter[J].Petroleum Geology & Experiment,2014,32(5):612-617.
师生宝,李美俊,朱雷.石油及沉积有机质中C1—和 C2-烷基二苯并噻吩鉴定及分布[J].石油实验地质,2014,32(5):612-617.
[23]Li Meijun,Shi Shengbao,Wang Tieguan,et al.The identification and distribution of C3- and C4-alkylated dibenzothiophenes in petroleum and sedimentary organic matter[J].Geochimica,2014,43(2):157-165.
李美俊,师生宝,王铁冠,等.石油和沉积有机质中 C3-,C4-烷基取代二苯并噻吩的鉴定[J].地球化学,2014,43(2):157-165.
[24]Huang Difan,Zhang Dajiang,Li Jinchao,et al.The Tertiary oil source correlation in Qaidam Basin[ J].Acta Sedimentologica Sinica,1989,7(2):1-13.
黄第藩,张大江,李晋超,等.柴达木盆地第三系油源对比[J].沉积学报,1989,7(2):1-13.
[25]Zhang Zhihuan,Yang Fan.Geochemical characteristics and environment of organic matter of saline lakes in Tertiary,China[J].Journal of Xi′an Petroleum Institute:Natural Science Edition,2002,17(6):16-20.
张枝焕,杨藩.我国第三系咸化湖相有机质组成及环境意义[J].西安石油学院学报:自然科学版,2002,17(6):16-20.
[26]Zhang Zhihuan,Yang Fan.Biomarker assemblage characteristics of source rocks and associated crude oils in saline lake facies of Cenozoic in China[J].Acta Sedimentologica Sinica,1998,16(3):119-123.
张枝焕,杨藩.中国新生界咸水湖相烃源岩和原油生物标志物组合特征[J].沉积学报,1998,16(3):119-123.
[27]Li Hongbo,Zhang Min,Zhang Chunming,et al.Geochemical characteristics of Tertiary source rocks in the south area of western Qaidam Basin[J].Natural Gas Geoscience,2008,19(6):519-523.
李洪波,张敏,张春明,等.柴达木盆地西部南区第三系烃源岩地球化学特征[J].天然气地球科学,2008,19(6):519-523.
[28]Wang Li,Jin Qiang,Liu Yongchang,et al.Characteristics of quality Tertiary source rocks in west Qaidam Basin[J].Natural Gas Industry,2009,29(2):23-26,131.
王力,金强,林腊梅,等.柴达木盆地西部古近系—新近系优质烃源岩特征[J].天然气工业,2009,29(2):23-26,131.
[29]Zhou Fengying,Peng Dehua,Bian Lizeng,et al.Progress in the organic matter study of immature oils in Qaidam Basin[J].Acta Geologica Sinica,2002(1):107-113,147.
周凤英,彭德华,边立增,等.柴达木盆地未熟—低熟石油的生烃母质研究新进展[J].地质学报,2002(1):107-113,147.
[30]Li Hao,Xu Yanping,Huang Haining,et al.Study on Evolution of paleo-lake of Tertiary in western Chadam Basin[J].Fault-Block Oil and Gas Field,2002,9(2):27-29.
李浩,徐艳萍,黄海宁,等.柴达木盆地西部地区第三纪古湖泊研究[J].断块油气田,2002,9(2):27-29.
[31]Chen Nenggui,Wang Yanqing,Xu Feng,et al.Palaeosalinity characteristics and its sedimentary response to the Cenozoic salt-water lacustrine deposition in Qaidam Basin[J].Journal of Palaeogeography,2015,17(3):371-380.
陈能贵,王艳清,徐峰,等.柴达木盆地新生界湖盆咸化特征及沉积响应[J].古地理学报,2015,17(3):371-380.
[32]Peng Dehua.Geology,Geochemical Characteristics and Mechanism of Hydrocarbon-generating for Source Rocks from the Tertiary Salty Lacustrine Facies in the West Region of the Qaidam Basin[D].Guangzhou:Graduate University of Chinese Academy of Sciences,Guangzhou Institute of Geochemistry,2004.
彭德华.柴达木盆地西部第三系咸化湖泊烃源岩地质地球化学特征与生烃机理[D].广州:中国科学院研究生院,广州地球化学研究所,2004.
[33]Xu Fengyin,Yin Chengming,Gong Qinglin,et al.Mesozoic-Cenozoic structural evolution in Qaidam Basin and its control over oil and gas[J].China Petroleum Exploration,2006,11(6):9-16,37-129 
徐凤银,尹成明,巩庆林,等.柴达木盆地中、新生代构造演化及其对油气的控制[J].中国石油勘探,200,11(6):9-16,37-129.
[34]Métivier F,Gaudemer Y,Tapponnier P,et al.Northeastward growth of the tibet plateau deduced from balanced reconstruction of two Depositional areas:The Qaidam and Hexi corridor Basins,China[J].Tectonics,1998,17(6):823-842.
[35]Li Yanming.Study on the Evolution of Salt Structure and its Control Effect on Oil and Gas in the Yingxiongling Region of the Qaidam Basin[D].Chengdu:Southwest Petroleum University,2016.
李艳明.柴达木盆地英雄岭地区盐构造演化及其对油气控制作用研究[D].成都:西南石油大学,2016.
[36]Zhang Jinning,Zhang Jingong,Yang Qianzheng,et al.The control effect of gypsum-salt rocks on formation and distribution of overpressure:A case of Shizigou area,Qaidam Basin[J].Acta Sedimentologica Sinica,2016,34(3):563-570.
[37]Li Hongbo,Zhang Min,Zhang Chunmin,et al.Evaluation of Tertiary source rocks in the south area of western Qaidam Basin[J].Journal of Oil and Gas Technology,2006,12(6):41-43.
李洪波,张敏,张春明,等.柴达木盆地西部南区第三系烃源岩评价[J].石油天然气学报,2006,12(6):41-43.
[38]Zhu Yangmin,Su Aiguo,Liang Digang,et al.Distribution characterization and origin of n-alkanes in saline lacustrine source of Qaidam Basin[J].Geochimica,2003,32(2):117-123.
朱扬明,苏爱国,梁狄刚,等.柴达木盆地咸湖相生油岩正构烷烃分布特征及其成因[J].地球化学,2003,32(2):117-123.
[39]Peters K E,Moldowan J M,Walters C C.The Biomarker Guide[M].2ng Edition.Beijing:Petroleum Industry Press,2011:18,23-27,45-48,91-94,102-104,172-173.
彼得斯,沃尔特斯,莫尔多万.生物标志化合物指南·下册[M].第2版.北京:石油工业出版社,2011:18,23-27,45-48,91-94,102-104,172-173.
[40]Rao Zhiguo,Wu Yi,Zhu Zhaoyu,et al.Is the maximum carbon number of long-chain n-alkanes an indicator of grassland or forest:Evidence from surface soils and modern plants[J].Chinese Science Bulletin,2011,56(10):774-780.
饶志国,吴翼,朱照宇,等.长链正构烷烃主峰碳数作为判别草本和木本植物指标的讨论:来自表土和现代植物的证据[J].科学通报,2011,56(10):774-780.
[41]Fu Jiamo,Sheng Guoying.Molecular organic geochemistry and its application to the study of paleoclimate and paleoenvironments[J].Quaternary Sciences,1992,12(4):306-320.
傅家谟,盛国英.分子有机地球化学与古气候,古环境研究[J].第四纪研究,1992,12(4):306-320.
[42]Sheng Guoying,Fan Shanfa,Liu Dehan,et al.Charactristics of the n-alkanes with even-odd predominance[J].Oil & Gas Geology,1981,2(1):57-65.
盛国英,范善发,刘德汉,等.正烷烃的偶碳优势特征[J].石油与天然气地质,1981,2(1):57-65.
[43]Xiao Fei,Bao Jianping,Zhu Cuishan,et al.Comparison of the geochemical characteristics of crude oils from typical oilfields in western Qaidam Basin[J].Journal of Earch Sciences and Environment,2013,34(4):43-52.
肖飞,包建平,朱崔山,等.柴达木盆地西部典型油田原油地球化学特征对比[J].地球科学与环境学报,2013,34(4):43-52.
[44]Zhang Chunming,Zhang Yuqing,Zhang Min,et al.Compositional variabilities among crude oils from the southwestern part of the Qaidam Basin,NW China[J].Journal of Petroleum Science and Engineering,2008,62(3/4):87-92.
[45]Luo Jian,Cheng Keming,Fu Lixin,et al.Alkylated dibenzothiophene index:A new method to assess thermal maturity of source rocks[J].Acta Petrolei Sinica,2001,22(3):27-31.
罗健,程克明,付立新,等.烷基二苯并噻吩——烃源岩热演化新指标[J].石油学报,2001,22(3):27-31.
[46]Li Jinggui,Zhen Jianjing,Liu Wenhui,et al.Dibenzothiophene series from the carbonate rocks and their crude oils in Tabei and Tazhong areas,Tarim Basin[J].Acta Sedimentologica Sinica,2004,22(2):348-353.
李景贵,郑建京,刘文汇,等.塔北,塔中地区碳酸盐岩及其原油中的二苯并噻吩类化合物[J].沉积学报,2004,22(2):348-353.
[47]Huo Qiuli,Li Zhenguang,Fu Li,et al.Study on the correlation of methyldiben zothiophenes distribution and organic maturity[J].Petroleum Geology & Oilfield Development in Daqing,2008,27(2):32-35.
霍秋立,李振广,付丽,等.烷基二苯并噻吩的分布与有机质成熟度关系的探讨[J].大庆石油地质与开发,2008,27(2):32-35.
[48]Li Sumei,Zhang Baoshou,Zhang Haizu,et al.Geochemical characteristics and affecting factors of the unusually high dibenzothiophenes oils in the Tazhong Uplift[J].Geoscience,2011,25(6):1108-1120.
李素梅,张宝收,张海祖,等.塔中原油超高二苯并噻吩硫特征及其控制因素[J].现代地质,2011,25(6):1108-1120.
[49]Liu Qiong,He Sheng.Distribution characteristics and geochemical significance of organic sulfur compounds from crude oils in the Southwestern Jianghan Basin[J].Geological Science and Technology Information,2008,27(2):56-62.
刘琼,何生.江汉盆地西南缘原油中含硫化合物的分布特征及其地球化学意义[J].地质科技情报,2008,27(2):56-62.
[50]Requejo A G,Sassen R,McDonald T,et al.Polynuclear aromatic hydrocarbons(PAH) as indicators of the source and maturity of marine crude oils[J].Organic Geochemistry,1996,24(10-11):1017-1033.
[51]Li Meijun,Zhong Ningning,Shi Shengbao,et al.The origin of trimethyldibenzothiophenes and their application as maturity indicators in sediments from the Liaohe Basin,East China[J].Fuel,2013,103:299-307.
[52]Asif M,Alexander  R,Fazeelat T,et al.Geosynthesis of dibenzothiophene and alkyl dibenzothiophenes in crude oils and sediments by carbon catalysis[J].Organic Geochemistry,2009,40(8):895-901.

[1] 韩伟, 刘文进, 李玉宏, 周俊林, 张文, 张云鹏, 陈晓宏, 黄斌. 柴达木盆地北缘稀有气体同位素特征及氦气富集主控因素[J]. 天然气地球科学, 2020, 31(3): 385-392.
[2] 吴因业, 吕佳蕾, 方向, 杨智, 王岚, 马达德, 陶士振. 湖相碳酸盐岩—混积岩储层有利相带分析——以柴达木盆地古近系为例[J]. 天然气地球科学, 2019, 30(8): 1150-1157.
[3] 李延丽, 苟迎春, 马新民, 李程程, 王朴, 陈芳芳. 柴达木盆地坪西地区基岩气藏储层特征[J]. 天然气地球科学, 2019, 30(2): 219-227.
[4] 周飞,王波,李哲翔,隋国杰,祁文珍,崔守凯,马进业,成定树. 柴达木盆地冷湖构造带天然气地球化学特征及成藏主控因素[J]. 天然气地球科学, 2019, 30(10): 1496-1507.
[5] 曾旭, 李剑, 田继先, 王波, 国建英, 沙威.  柴达木盆地腹部晚期构造带成藏模拟实验研究[J]. 天然气地球科学, 2018, 29(9): 1301-1309.
[6] 黄成刚,关新,倪祥龙,常海燕,张世铭,杨森. 柴达木盆地英西地区E23咸化湖盆白云岩储集层特征及发育主控因素[J]. 天然气地球科学, 2017, 28(2): 219-231.
[7] 郭佳佳,孙国强,龙国徽,管斌,康健,夏维民,陈波,史基安. 柴达木盆地北缘冷湖五号构造下侏罗统沉积—成岩环境分析[J]. 天然气地球科学, 2017, 28(12): 1839-1845.
[8] 王琳,赵孟军,孟庆洋,王鹏,王科,袁海莉,申磊军,雷刚. 柴达木盆地英西地区中深层油气成藏过程分析[J]. 天然气地球科学, 2017, 28(12): 1846-1854.
[9] 陈波, 王波, 管斌, 蔡智洪, 孙国强, 史基安. 柴北缘西段古近系优质储层孔隙成因类型及其控制因素[J]. 天然气地球科学, 2016, 27(8): 1454-1465.
[10] 周飞, 张永庶, 王彩霞, 隋国杰, 王波, 张继红, 张建杰, 吴志雄. 柴达木盆地东坪—牛东地区天然气地球化学特征及来源探讨[J]. 天然气地球科学, 2016, 27(7): 1312-1323.
[11] 包建平,汪立群,朱翠山,陈琰,蒋兴超,袁莉,周飞. 柴达木盆地开特米里克油田凝析油成因研究——基于金刚烷烃类化合物[J]. 天然气地球科学, 2016, 27(2): 330-340.
[12] 王万春, 王成, 孙敏卓, 丁万仁. 成岩阶段微生物作用及其油气地质意义[J]. 天然气地球科学, 2016, 27(11): 1970-1978.
[13] 孙敏卓,张鹏,周莉,刘海珍,李国艳,陈建州,谭和勇,房嬛,王国仓. 柴达木盆地苏探1井原油生物标志化合物特征和成藏分析[J]. 天然气地球科学, 2015, 26(5): 922-929.
[14] 李军亮,肖永军,林武,柴先平,张俊锋. 柴达木盆地东部地区中、下侏罗统残留分布及控制因素[J]. 天然气地球科学, 2015, 26(10): 1893-1900.
[15] 张焕旭,陈世加,王力,邹贤利,黄囿霖,姚宜同,占盼. 油气分段捕获原理在天然气成藏研究中的应用——以柴达木盆地南翼山和开特米里克地区为例[J]. 天然气地球科学, 2015, 26(10): 1901-1909.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 旷理雄,郭建华,王英明,冯永宏,李广才 . 柴窝堡凹陷达坂城次凹油气成藏条件及勘探方向[J]. 天然气地球科学, 2005, 16(1): 20 -24 .
[2] 邵荣;叶加仁;陈章玉;. 流体包裹体在断陷盆地含油气系统研究中的应用概述[J]. 天然气地球科学, 2000, 11(6): 11 -14 .
[3] 何家雄;李明兴;陈伟煌;. 莺歌海盆地热流体上侵活动与天然气运聚富集关系探讨[J]. 天然气地球科学, 2000, 11(6): 29 -43 .
[4] 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 .
[5] 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 .
[6] 廖成君. VSP技术在锦612复杂断块油藏开发部署研究中的应用[J]. 天然气地球科学, 2005, 16(1): 117 -122 .
[7] 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 .
[8] 杜乐天;. 地球的5个气圈与中地壳天然气开发[J]. 天然气地球科学, 2006, 17(1): 25 -30 .
[9] 周世新;邹红亮;解启来;贾星亮;. 沉积盆地油气形成过程中有机-无机相互作用[J]. 天然气地球科学, 2006, 17(1): 42 -47 .
[10] 曹华;龚晶晶;汪贵锋;. 超压的成因及其与油气成藏的关系[J]. 天然气地球科学, 2006, 17(3): 422 -425 .