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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2007  >  29(2): 154-161
Yang Xiaoyong, Liu Deliang, Wang Baichang, Li Zhensheng, Tan Yin, Yang Qiang. STUDY ON FORMATION OF INORGANIC CARBON DIOXIDE GAS RESERVOIRS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(2): 154-161. doi: 10.11781/sysydz200702154
Citation: Yang Xiaoyong, Liu Deliang, Wang Baichang, Li Zhensheng, Tan Yin, Yang Qiang. STUDY ON FORMATION OF INORGANIC CARBON DIOXIDE GAS RESERVOIRS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(2): 154-161. doi: 10.11781/sysydz200702154
shu

STUDY ON FORMATION OF INORGANIC CARBON DIOXIDE GAS RESERVOIRS

doi: 10.11781/sysydz200702154
  • 1.

    School of Earth and Space Sciences, The Research Center of Petroleum and Natural Gases, University of Science & Technology of China, Hefei, Anhui 230026, China

  • 2. Exploration Department, Daqing Oil Limited Company, Daqing, Heilongjiang 163453, China

  • Received Date: 2006-04-11
  • Rev Recd Date: 2007-03-12
  • Publish Date: 2007-03-28
    Abstract
  • This paper presents the general situation on the geological and geochemical characteristics of CO2 pools,their forming condition and distributions as well as their controlled geological-tectonic environments.The degassing experiment of volcanic rocks in Songliao Basin presents the CO2 releasing parameters for different types of volcanic rocks.Geochemical modeling calculation of CO2 releasing has been done based on dynamic metamorphism caused by ductile-brittle shearing deformation.The amount of CO2 releasing is calculated and its relative calculation model is proposed during the contact metamorphism in carbonate rocks.Based on research,the model for the calculation of CO2 degassing and formation of CO2 pools under the condition of degassing from volcanic rocks,dynamic and contact metamorphism have been established.The distributions of CO2 pools and their exploration localities in China have also been proposed.

     

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    • References(44)
  • [1]
    戴金星,宋岩,戴春森等.中国东部无机成因气及其气藏形成条件[M].北京:科学出版社,1995.1～212
    [2]
    徐永昌.天然气成因理论与应用[M].北京:科学出版社,1994.1～414
    [3]
    王先彬.稀有气体同位素地球化学和宇宙化学[M].北京:科学出版社,1989.1～451
    [4]
    戴金星.五大连池地幔成因天然气[J].石油实验地质,1992,14(2):200～203
    [5]
    戴金星,戴春森,宋岩等.中国一些地区温泉中天然气的地球化学特征及碳、氦同位素组成[J].中国科学(B辑),1994,24(4):426～433
    [6]
    涂光炽.关于CO2的若干问题[J].地学前缘,1996,3(3～4):53～62
    [7]
    关效如.我国东部高纯二氧化碳成因[J].石油实验地质,1990,12(3):248～257
    [8]
    杨晓勇,刘德良,陈永见等.接触变质作用条件下无机天然气成藏模型:以郯庐断裂带南段双山为例[J].石油学报,2003,24(6):18～23
    [9]
    杨玉峰,张秋,黄海平等.松辽盆地徐家围子断陷无机成因天然气及其成藏模式[J].地学前缘,2000,7(4):523～533
    [10]
    陈永见,刘德良,杨晓勇.郯庐断裂系统与中国东部幔源岩浆成因CO2关系初探[J].地质地球化学,1999,27(1):38～48
    [11]
    郭占谦,王先彬.松辽盆地无机成因气的成藏特征[J].中国科学(D辑),1997,27(2):100～106
    [12]
    罗开平,夏遵义,徐言岗等.二氧化碳:中国东部中、新生代盆地的重要资源[J].石油与天然气地质,1998,19(2):165～168
    [13]
    Cornides I.Magmatic carbon dioxide at the crust's Sulface in the carpathian Basin[J].Geochemical.Journal,1993,27(2):241～249
    [14]
    上官志冠,白春华,孙明良.腾冲热海地区现代幔源岩浆气体释放特征[J].中国科学(D辑),2000,30(4):407～414
    [15]
    王先彬,陈践发,徐胜等.地震区温泉气体的地球化学特征[J].中国科学(B辑),1992,22(8):849～854
    [16]
    陈践发,廖永胜,孙明良.济阳坳陷天然气氦同位素特征及二氧化碳成因与第三纪岩浆活动的关系[J].地球化学,1996,25(5):350～356
    [17]
    赫英.胜利油田边缘及外围找寻不同类型深部天然气的可能性[J].地质论评,1999,45(1):32～35
    [18]
    杜乐天.地流体与软流层(体)地球化学[M].北京:科学出版社,1996.1～466
    [19]
    樊祺诚,刘若新,林卓然等.中国东部地幔CO2流体包裹体的碳同位素初步研究[J].地球化学,1996,25(3):264～269
    [20]
    杨晓勇,刘德良,陶士振.中国东部典型地幔岩包裹体成分研究及意义[J].石油学报,1999,20(1):19～24
    [21]
    杨晓勇,郑永飞,刘德良等.中国东部橄榄岩和榴辉岩中CO2流体包裹体的碳同位素组成[J].岩石学报,2000,16(4):473～481
    [22]
    Yang Xiaoyong,Zheng Yongfei,Liu Deliang,et al.Study on chemical compositions of fluid inclusions from peridotite and eclogites in Eastern—Central China:The geodynamic implications[J].Phys Chem Earth,2001,26(7-8):705～718
    [23]
    Nadeau S.Carbon concentration and isotopic ratios in fluid-inclusion-bearing upper-mantle xenoliths along the northwestern margin of North America[J].Chem Geol,1990,81(2):271～297
    [24]
    Sugisaki R,Mimura K.Mantle hydrocarbons:Abiotic or biotic?[J].Geochimica et Cosmochimica Acta,1994,58(11):2527～2542
    [25]
    Anovitz L M,Essene E J.Phase equilibrium in the system CaCO3-MgCO3-FeCO3[J].Journal of Petrology,1987,28:389～414
    [26]
    Dipple G,Ferry J M.Identification of the scales of differential element mobility in fault zone[J].J Metamorphic Geol,1990,8(6):645～661
    [27]
    Ferry J M.Dehydration and decarbonation reactions as a record of fluid infiltration[J].Reviews in Mineralogy,1991,26(3):351～393
    [28]
    Ferry J M,Gerdes M L.Chemically reactive fluid flow during metamorphism[J].Annual Rev Earth Planet Sci,1998,26(2):255～287
    [29]
    Ferry J M.Regional metamorphism of the Waits River Formation,Eastern Vermont:delineation of a new type of giant metamorphic hydrothermal system[J].Journal of Petrology,1992,33(1):45～94
    [30]
    Kreulen R.High integrated fluid/rock ratios during metamorphism at Naxos:evidence from carbon isotopes of calcite in schists and fluid inclusions[J].Contrib Mineral Petrol,1988,98(1):28～32
    [31]
    Lasaga A C.Rye D M.Fluid flow and chemical reaction kinetics in metamorphic systems[J].Am J Sci,1993,293(3):361～404
    [32]
    Leger A,Ferry J M.Fluid infiltration and regional metamorphism of the Waits River Formation,north-east Vermont,USA[J].J Metamorphic Geol,1993,11(1):3～29
    [33]
    Ferry J M.Mineral reactions and element migration during metamorphism of calcareous sediments from the Vassalboro Formation,South-central Maine[J].American Mineralogist,1983,68(3):334～354
    [34]
    O'hara K.Fluid flow and volume loss during mylonization:an origin for phyllonite in an overthust setting,North California[J].Tectonophysics,1988,156(1);21～36
    [35]
    Yang Xiaoyong,Yang Xueming,Liu Deliang,et al.Study on the characteristics of migration in mylonites of the ductile shear zones from the southern part of Tancheng-Lujiang fault belt,Anhui Province[J].Acta Geol Sinica,1998,72(1):35～48
    [36]
    杨晓勇,刘德良,张交东等.郯庐断裂带南段双山韧-脆性剪切带物质迁移与CO2释放研究[J].地质学报,2002,76(3):335～346
    [37]
    谈迎,刘德良,李振生等.松辽盆地北部二氧化碳气藏成因地球化学研究[J].石油实验地质,2006,28(5):480～483
    [38]
    Xu J W,Zhu G,Tong W X,et al.Formation and evolution of the Tancheng-Lujiang wrench fault system:a major shear system to the northwest of the Pacific Ocean[J].Tectonophysics,1987,134(2):273～310
    [39]
    马锦龙,陶明信.郯庐断裂带中段幔源岩包体中的流体组成特征[J].兰州大学学报(自然科学版),2004,40(1):85～89
    [40]
    袁彩萍,徐思煌,贾霍甫等.渤海湾盆地东营凹陷孔店组烃源岩特征研究[J].石油实验地质,2006,28(2):177～181
    [41]
    黄泽光,高长林.南华北中生代火山岩与前渊盆地[J].石油实验地质,2006,28(1):1～7
    [42]
    苏惠,曲丽萍,张金川等.渤海湾盆地东濮凹陷天然气成藏条件与富集规律[J].石油实验地质,2006,28(2):123～128
    [43]
    程有义.济阳坳陷阳信-花沟-平南地区CO2气藏的储层和盖层[J].沉积学报,2001,19(3):405～409
    [44]
    Yang Xiao yong,Lju Deliang,Dai Jinxing.Extremely high H2-bearing fluid inclusions in eclogite from Dabie Shan orogenic belt,eastern China[J].Geol Soc India,2002,61(1):101～102
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