深部流体及有机-无机相互作用下油气形成的基本内涵
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:The scientific connotation of oil and gas formations under deep fluids and organic-inorganic interaction
  • 作者:刘全有 ; 朱东亚 ; 孟庆强 ; 刘佳宜 ; 吴小奇 ; 周冰 ; Qi ; FU ; 金之钧
  • 英文作者:Liu Q;Zhu D;Meng Q;Liu J;Wu X;Zhou B;Fu Q;Jin Z;
  • 关键词:有机无机相互作用 ; 深部流体 ; 加氢生烃 ; 溶蚀改造 ; 驱替
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:页岩油气富集机理与有效开发国家重点实验室;中国石油化工股份有限公司石油勘探开发研究院构造-沉积储层实验室;Department of Earth and Atmospheric Sciences, University of Houston;
  • 出版日期:2019-03-04
  • 出版单位:中国科学:地球科学
  • 年:2019
  • 期:v.49
  • 基金:国家自然科学基金项目(批准号:41625009、U1663201、41872122);; 中国科学院战略性先导科技专项A类项目(编号:XDA14010404);; 国家重点研究计划项目(编号:2017YFC0603102)资助
  • 语种:中文;
  • 页:JDXK201903002
  • 页数:22
  • CN:03
  • ISSN:11-5842/P
  • 分类号:17-38
摘要
含油气盆地作为地球系统中相对稳定的克拉通块体,从早期烃源岩发育环境、油气形成、储层溶蚀改造到油气聚集或者破坏都受到地球系统演化的影响.深部流体作为联系盆地内、外因素的纽带,以有机-无机相互作用的方式贯穿了油气形成和聚集的全过程.深部流体携带的营养物质促进了成烃生物的勃发和碳氢源的额外补充,有利于优质烃源岩的发育和提高烃源岩生烃潜力,其携带的能量促进了烃源岩早熟和高成熟烃源活化加氢生烃.深部富CO_2流体对碳酸盐岩、碎屑岩储层的溶蚀改造,改善了深层储集体空间,使得油气储集空间向更深延伸.深部超临界CO_2对深层滞留原油的萃取和泥页岩中CH_4的驱替,提高了深层和致密储层中烃类流动性.同时,深部流体携带的物质(C、H、催化物质)和能量不仅能够促使费托合成无机CH_4,促使有机质热演化生烃形成"热液石油",而且也能使得有机来源的原油发生热蚀变.因此,从地球层圈相互作用的视角看,深部流体不仅对沉积盆地输入了大量的外源C和H,改善了油气赋存空间,而且也提高了油气富集聚集效率.
        
引文
蔡郁文,王华建,王晓梅,何坤,张水昌,吴朝东.2017.铀在海相烃源岩中富集的条件及主控因素.地球科学进展,32:199-208
    车燕,姜慧超,穆星,李军亮.2001.花沟气田气藏类型及成藏规律.油气地质及采收率,8:32-34
    冯子辉,霍秋立,王雪.2001.松辽盆地北部氦气成藏特征研究.天然气工业,21:29-30
    高玉巧,刘立,杨会东,尤丽,刘娜.2007.松辽盆地孤店二氧化碳气田片钠铝石的特征及成因.石油学报,28:62-67
    韩崇仁.2001.加氢裂化工艺与工程.北京:中国石化出版社.224-226
    何治亮,魏修成,钱一雄,鲍征宇,范明,焦存礼,彭守涛,陈冬.2011.海相碳酸盐岩优质储层形成机理与分布预测.石油与天然气地质,32:489-498
    胡文瑄.2016.盆地深部流体主要来源及判识标志研究.矿物岩石地球化学通报,35:817-826
    胡文瑄,陈琪,王小林,曹剑.2010.白云岩储层形成演化过程中不同流体作用的稀土元素判别模式.石油与天然气地质,31:810-818
    胡文瑄,朱井泉,王小林,由雪莲,何凯.2014.塔里木盆地柯坪地区寒武系微生物白云岩特征、成因及意义.石油与天然气地质,35:860-869
    蒋裕强,陶艳忠,王珏博,强子同,江娜,林刚,蒋婵.2016.四川盆地高石梯-磨溪地区灯影组热液白云石化作用.石油勘探与开发,43:1-10
    焦念志.2012.海洋固碳与储碳--并论微型生物在其中的重要作用.中国科学:地球科学,42:1473-1486
    金之钧,胡文瑄,张刘平,陶明信.2007.深部流体活动及油气成藏效应.北京:科学出版社
    金之钧,朱东亚,胡文瑄,张学丰,王毅,闫相宾.2006.塔里木盆地热液活动地质地球化学特征及其对储层影响.地质学报,80:245-253
    李曙光.2015.深部碳循环的Mg同位素示踪.地学前缘,22:143-159
    刘国勇,张刘平,金之钧.2005.深部流体活动对油气运移影响初探.石油实验地质,27:269-275
    刘立,高玉巧,曲希玉,蒙启安,高福红,任延广,朱德丰.2006.海拉尔盆地乌尔逊凹陷无机CO2气储层的岩石学与碳氧同位素特征.岩石学报,22:1861-1868
    罗平,王石,李朋威,宋金民,金廷福,王果谦,杨式升.2013.微生物碳酸盐岩油气储层研究现状与展望.沉积学报,31:807-823
    罗渝然.2004.化学键能数据手册.北京:科学出版社.1-396
    马安来,黎玉战,张玺科,张忠民.2015.桑托斯盆地盐下J油气田CO2成因、烷烃气地球化学特征及成藏模式.中国海上油气,27:13-20
    孟庆强,陶成,朱东亚,金之钧,王强,郑伦举.2011.微量氢气定量富集方法初探.石油实验地质,33:314-316
    钱一雄,冯菊芳,何治亮,张克银,金婷,董少峰,尤东华,张永东.2017.从岩石学及微区同位素探讨四川盆地灯影组皮壳-葡萄状白云石成因.石油与天然气地质,38:665-676
    上官志冠,霍卫国.2001.腾冲热海地区逸出H2的δD值及其成员.科学通报,46:1316-1320
    舒晓辉,张军涛,李国蓉,龙胜祥,吴世祥,李宏涛.2012.四川盆地北部栖霞组-茅口组热液白云岩特征与成因.石油与天然气地质,33:442-448
    帅燕华,张水昌,苏爱国,王汇彤,蔡报元,王慧.2010.柴达木盆地三湖地区产甲烷作用仍在强烈进行的地球化学证据.中国科学:地球科学,39:734-740
    宋金民,刘树根,李智武,罗平,杨迪,孙玮,彭瀚霖,余永强.2017.四川盆地上震旦统灯影组微生物碳酸盐岩储层特征与主控因素.石油与天然气地质,38:741-752
    王顺玉,李兴甫.1999.威远和资阳震旦系天然气地球化学特征与含气系统研究.天然气地球科学,10:63-69
    吴亮亮,廖玉宏,方允鑫,耿安松.2012.不同成熟度烃源岩的催化加氢热解与索氏抽提在生物标志物特征上的对比.科学通报,57:3067-3077
    徐永昌,沈平,李玉成.1989.中国最古老的气藏--四川威远震旦纪气藏.沉积学报,7:3-14
    杨长清,姚俊祥.2004.三水盆地二氧化碳气成藏模式.天然气工业,24:36-39
    张立飞,陶仁彪,朱建江.2017.俯冲带深部碳循环:问题与讨论.矿物岩石地球化学通报,36:185-196
    张泉兴,李雨梁,胡忠良,张启明.1989.莺歌海盆地梅山组的石油深热成因和水相运移.中国海上油气,3:25-33
    张子枢.1987.我国氦资源及其开发与保护.资源开发与市场,3:28-31
    赵斐宇,姜素华,李三忠,曹伟,汪刚,张慧璇,高嵩.2017.中国无机CO2气藏与(古)太平洋板块俯冲关联.地学前缘,24:370-384
    赵文智,沈安江,周进高,王小芳,陆俊明.2014.礁滩储集层类型、特征、成因及勘探意义--以塔里木和四川盆地为例.石油勘探与开发,41:257-267
    朱东亚,金之钧,胡文瑄,张学丰.2008.塔里木盆地深部流体对碳酸盐岩储层影响.地质论评,54:348-354
    朱东亚,金之钧,胡文瑄.2010.塔北地区下奥陶统白云岩热液重结晶作用及其油气储集意义.中国科学:地球科学,40:156-170
    Abrajano T A,Sturchio N C,Bohlke J K,Lyon G L,Poreda R J,Stevens C M.1988.Methane-hydrogen gas seeps,Zambales Ophiolite,Philippines:Deep or shallow origin?Chem Geol,71:211-222
    Akinlua A,Torto N,Ajayi T R.2008.Supercritical fluid extraction of aliphatic hydrocarbons from Niger Delta sedimentary rock.JSupercrit Fluid,45:57-63
    Al-Aasm I.2003.Origin and characterization of hydrothermal dolomite in the Western Canada sedimentary basin.J Geochem Explor,78-79:9-15
    Alemu B L,Aagaard P,Munz I A,Skurtveit E.2011.Caprock interaction with CO2:A laboratory study of reactivity of shale with supercritical CO2and brine.Appl Geochem,26:1975-1989
    Algeo T J,Rowe H.2012.Paleoceanographic applications of tracemetal concentration data.Chem Geol,324-325:6-18
    Anders E,Hayatsu R,Studier M H.1973.Organic compounds in meteorites:They may have formed in the solar nebula,by catalytic reactions of carbon monoxide,hydrogen,and ammonia.Science,182:781-790
    Anderson R B,K?llbel H,Rálek M.1984.The Fischer-Tropsch Synthesis.New York:Academic Press.1-30
    Armitage P J,Faulkner D R,Worden R H,Aplin A C,Butcher A R,Iliffe J.2011.Experimental measurement of,and controls on,permeability and permeability anisotropy of caprocks from the CO2storage project at the Krechba Field,Algeria.J Geophys Res,116:B12208
    Bauld J.1984.Microbial mats in marginal marine environments:Shark Bay,Western Australia,and Spencer Gulf,South Australia.In:Cohen Y,Castenholz R W,Halvorson H O,eds.Microbial Mats:Stromatolites.New York:Alan Liss.39-58
    Bertier P,Swennen R,Laenen B,Lagrou D,Dreesen R.2006.Experimental identification of CO2-water-rock interactions caused by sequestration of CO2in Westphalian and Buntsandstein sandstones of the Campine Basin(NE-Belgium).J Geochem Explor,89:10-14
    Bishop A N,Love G D,McAulay A D,Snape C E,Farrimond P.1998.Release of kerogen-bound hopanoids by hydropyrolysis.Org Geochem,29:989-1001
    Bohdanowic C.1934.Natural gas occurrence in Russia(U.S.S.R).AAPG Bull,18:746-759
    Bondar E,Koel M.1998.Application of supercritical fluid extraction to organic geochemical studies of oil shales.Fuel,77:211-213
    Browning T J,Bouman H A,Henderson G M,Mather T A,Pyle D M,Schlosser C,Woodward E M S,Moore C M.2014.Strong responses of Southern Ocean phytoplankton communities to volcanic ash.Geophys Res Lett,41:2851-2857
    Burne R V,Moore L S.1987.Microbialites:Organosedimentary deposits of benthic microbial communities.Palaios,2:241-254
    Clifton C G,Walters C C,Simoneit B R T.1990.Hydrothermal petroleums from Yellowstone National Park,Wyoming,U.S.A..Appl Geochem,5:169-191
    Dai J,Yang S,Chen H,Shen X.2005.Geochemistry and occurrence of inorganic gas accumulations in Chinese sedimentary basins.Org Geochem,36:1664-1688
    Dasgupta R,Hirschmann M M,Withers A C.2004.Deep global cycling of carbon constrained by the solidus of anhydrous,carbonated eclogite under upper mantle conditions.Earth Planet Sci Lett,227:73-85
    Davies G R,Smith Jr.L B.2006.Structurally controlled hydrothermal dolomite reservoir facies:An overview.AAPG Bull,90:1641-1690
    Dehghanpour H,Zubair H A,Chhabra A,Ullah A.2012.Liquid intake of organic shales.Energy Fuels,26:5750-5758
    Demaison G J,Moore G T.1980.Anoxic environments and oil source bed genesis.Org Geochem,2:9-31
    Dick G J,Anantharaman K,Baker B J,Li M,Reed D C,Sheik C S.2013.The microbiology of deep-sea hydrothermal vent plumes:Ecological and biogeographic linkages to seafloor and water column habitats.Front Microbiol,4:124
    Dick G J,Tebo B M.2010.Microbial diversity and biogeochemistry of the Guaymas Basin deep-sea hydrothermal plume.Environ Microbiol,12:1334-1347
    Didyk B M,Simoneit B R T.1990.Petroleum characteristics of the oil in a Guaymas Basin hydrothermal chimney.Appl Geochem,5:29-40
    Duan Z,Li D.2008.Coupled phase and aqueous species equilibrium of the H2O-CO2-NaCl-CaCO3system from 0 to 250°C,1 to 1000 bar with NaCl concentrations up to saturation of halite.Geochim Cosmochim Acta,72:5128-5145
    Etiope G.2017.Abiotic methane in continental serpentinization sites:An overview.Procedia Earth Planet Sci,17:9-12
    Fang Y,Liao Y,Wu L,Geng A.2014.The origin of solid bitumen in the Honghuayuan Formation(O1h)of the Majiang paleo-reservoir-Evidence from catalytic hydropyrolysates.Org Geochem,68:107-117
    Fitzsimmons J N,John S G,Marsay C M,Hoffman C L,Nicholas S L,Toner B M,German C R,Sherrell R M.2017.Iron persistence in a distal hydrothermal plume supported by dissolved-particulate exchange.Nat Geosci,10:195-201
    Frezzotti M L,Huizenga J M,Compagnoni R,Selverstone J.2014.Diamond formation by carbon saturation in C-O-H fluids during cold subduction of oceanic lithosphere.Geochim Cosmochim Acta,143:68-86
    Frogner P,Reynir Gíslason S,óskarsson N.2001.Fertilizing potential of volcanic ash in ocean surface water.Geology,29:487-490
    Frost D J,McCammon C A.2008.The redox state of Earth’s mantle.Annu Rev Earth Planet Sci,36:389-420
    Fu Q,Sherwood Lollar B,Horita J,Lacrampe-Couloume G,Seyfried Jr.W E.2007.Abiotic formation of hydrocarbons under hydrothermal conditions:Constraints from chemical and isotope data.Geochim Cosmochim Acta,71:1982-1998
    Gao Y,Liu L,Hu W.2009.Petrology and isotopic geochemistry of dawsonite-bearing sandstones in Hailaer basin,northeastern China.Appl Geochem,24:1724-1738
    Goebel E D,Coveney R M J,Angino E E,Zeller E J.1983.Naturally occurring hydrogen gas from a borehole on the western flank of Nemaha anticline in Kansas.AAPG Bull,67:1324
    Pagès A,Grice K,Ertefai T,Skrzypek G,Jahnert R,Greenwood P.2014.Organic geochemical studies of modern microbial mats from Shark Bay:Part I:Influence of depth and salinity on lipid biomarkers and their isotopic signatures.Geobiology,12:469-487
    Hawkes H E.1972.Free hydrogen in genesis of petroleum.AAPG Bull,56:2268-2270
    Hecht L,Freiberger R,Gilg H A,Grundmann G,Kostitsyn Y A.1999.Rare earth element and isotope(C,O,Sr)characteristics of hydrothermal carbonates:Genetic implications for dolomite-hosted talc mineralization at G?pfersgrün(Fichtelgebirge,Germany).Chem Geol,155:115-130
    Heller R,Zoback M.2014.Adsorption of methane and carbon dioxide on gas shale and pure mineral samples.J Unconv Oil Gas Resour,8:14-24
    Hoffmann L J,Breitbarth E,Ardelan M V,Duggen S,Olgun N,Hassell?v M,W?ngberg S?.2012.Influence of trace metal release from volcanic ash on growth of Thalassiosira pseudonana and Emiliania huxleyi.Mar Chem,132-133:28-33
    Hooper E C D.1991.Fluid migration along growth faults in compacting sediments.J Pet Geol,14:161-180
    Horita J,Berndt M E.1999.Abiogenic methane formation and isotopic fractionation under hydrothermal conditions.Science,285:1055-1057
    Huang B,Tian H,Huang H,Yang J,Xiao X,Li L.2015.Origin and accumulation of CO2and its natural displacement of oils in the continental basins,northern South China Sea.AAPG Bull,99:1349-1369
    Huang B,Xiao X,Zhu W.2004.Geochemistry,origin,and accumulation of CO2in natural gases of the Yinggehai Basin,offshore South China Sea.AAPG Bull,88:1277-1293
    Hurley N F,Budros R.1990.Albion-Scipio and Stoney Point FieldsUSA Michigan Basin.AAPG Special Volumes.1-37
    Hyatt J A.1984.Liquid and supercritical carbon dioxide as organic solvents.J Org Chem,49:5097-5101
    Jacquemyn C,El Desouky H,Hunt D,Casini G,Swennen R.2014.Dolomitization of the Latemar platform:Fluid flow and dolomite evolution.Mar Pet Geol,55:43-67
    Jeffrey A W A,Kaplan I R.1988.Hydrocarbons and inorganic gases in the Gravberg-1 well,Siljan Ring,Sweden.Chem Geol,71:237-255
    Jin Z,Yuan Y,Sun D,Liu Q,Li S.2014.Models for dynamic evaluation of mudstone/shale cap rocks and their applications in the Lower Paleozoic sequences,Sichuan Basin,SW China.Mar Pet Geol,49:121-128
    Jin Z J,Zhang L P,Yang L,Hu W X.2004.A preliminary study of mantle-derived fluids and their effects on oil/gas generation in sedimentary basins.J Pet Sci Eng,41:45-55
    Jones R W,Edison T A.1978.Microscopic observations of kerogen related to geochemical parameters with emphasis on thermal maturation.Pacific Section SEPM.1-12
    Jung J W,Espinoza D N,Santamarina J C.2010.Properties and phenomena relevant to CH4-CO2replacement in hydrate-bearing sediments.J Geophys Res,115:B10102
    Kerrick D M,Connolly J A D.1998.Subduction of ophicarbonates and recycling of CO2and H2O.Geology,26:375-378
    Kvenvolden K A,Rapp J B,Hostettler F D,Morton J L,King J D,Claypool G E.1986.Petroleum associated with polymetallic sulfide in sediment from Gorda Ridge.Science,234:1231-1234
    Lancet M S,Anders E.1970.Carbon isotope fractionation in the Fischer-Tropsch synthesis and in meteorites.Science,170:980-982
    Lee C T A,Jiang H,Ronay E,Minisini D,Stiles J,Neal M.2018.Volcanic ash as a driver of enhanced organic carbon burial in the Cretaceous.Sci Rep,8:4197
    Lewan M.1993.Laboratory simulation of petroleum formation:Hydrous pyrolysis.In:Engel M H,Macko S A,eds.Organic Geochemistry-Principle and Applications.New York:Plenum Press.419-422
    Lewan M D,Winters J C,McDonald J H.1979.Generation of oil-like pyrolyzates from organic-rich shales.Science,203:897-899
    Li J,Cui J,Yang Q,Cui G,Wei B,Wu Z,Wang Y,Zhou H.2017.Oxidative weathering and microbial diversity of an inactive seafloor hydrothermal sulfide chimney.Front Microbiol,8:1378
    Liao Y,Fang Y,Wu L,Geng A,Hsu C S.2012.The characteristics of the biomarkers andδ13C of n-alkanes released from thermally altered solid bitumens at various maturities by catalytic hydropyrolysis.Org Geochem,46:56-65
    Liu N,Liu L,Qu X,Yang H,Wang L,Zhao S.2011.Genesis of authigene carbonate minerals in the Upper Cretaceous reservoir,Honggang Anticline,Songliao Basin:A natural analog for mineral trapping of natural CO2storage.Sediment Geol,237:166-178
    Liu Q,Dai J,Jin Z,Li J,Wu X,Meng Q,Yang C,Zhou Q,Feng Z,Zhu D.2016.Abnormal carbon and hydrogen isotopes of alkane gases from the Qingshen gas field,Songliao Basin,China,suggesting abiogenic alkanes?J Asian Earth Sci,115:285-297
    Liu Q,Liu W,Dai J.2007.Characterization of pyrolysates from maceral components of Tarim coals in closed system experiments and implications to natural gas generation.Org Geochem,38:921-934
    Liu Q,Zhu D,Jin Z,Meng Q,Wu X,Yu H.2017.Effects of deep CO2on petroleum and thermal alteration:The case of the Huangqiao oil and gas field.Chem Geol,469:214-229
    Liu S,Huang W,Jansa L F,Wang G,Song G,Zhang C,Sun W,Ma W.2014.Hydrothermal dolomite in the Upper Sinian(Upper Proterozoic)Dengying Formation,East Sichuan Basin,China.Acta Geol Sin-Engl Ed,88:1466-1487
    Liu S A,Wu H,Shen S,Jiang G,Zhang S,Lv Y,Zhang H,Li S.2017.Zinc isotope evidence for intensive magmatism immediately before the end-Permian mass extinction.Geology,45:343-346
    Love G D,Snape C E,Carr A D,Houghton R C.1995.Release of covalently-bound alkane biomarkers in high yields from kerogen via catalytic hydropyrolysis.Org Geochem,23:981-986
    Lu J,Wilkinson M,Haszeldine R S,Fallick A E.2009.Long-term performance of a mudrock seal in natural CO2storage.Geology,37:35-38
    Makhanov K,Habibi A,Dehghanpour H,Kuru E.2014.Liquid uptake of gas shales:A workflow to estimate water loss during shut-in periods after fracturing operations.J Unconv Oil Gas Resour,7:22-32
    Martin J H,Fitzwater S E.1988.Iron deficiency limits phytoplankton growth in the north-east Pacific subarctic.Nature,331:341-343
    Marty B,Gunnlaugsson E,Jambon A,Oskarsson N,Ozima M,Pineau F,Torssander P.1991.Gas geochemistry of geothermal fluids,the Hengill area,southwest rift zone of Iceland.Chem Geol,91:207-225
    McCollom T M,Seewald J S,Lollar B S,Lacrampe-Couloume G.2006.Isotopic signatures of abiotic organic synthesis under geologic conditions.Geochim Cosmochim Acta,70:A0407
    Meng Q,Sun Y,Tong J,Fu Q,Zhu J,Zhu D,Jin Z.2015.Distribution and geochemical characteristics of hydrogen in natural gas from the Jiyang Depression,Eastern China.Acta Geol Sin-Engl Ed,89:1616-1624
    Michaelis W,Jenisch A,Richnow H H.1990.Hydrothermal petroleum generation in Red Sea sediments from the Kebrit and Shaban Deeps.Appl Geochem,5:103-114
    Middag R,de Baar H J W,Laan P,Cai P H,van Ooijen J C.2011.Dissolved manganese in the Atlantic sector of the Southern Ocean.Deep-Sea Res Part II-Top Stud Oceanogr,58:2661-2677
    Middleton R S,Carey J W,Currier R P,Hyman J D,Kang Q,Karra S,Jiménez-Martínez J,Porter M L,Viswanathan H S.2015.Shale gas and non-aqueous fracturing fluids:Opportunities and challenges for supercritical CO2.Appl Energy,147:500-509
    Milesi V,Prinzhofer A,Guyot F,Benedetti M,Rodrigues R.2016.Contribution of siderite-water interaction for the unconventional generation of hydrocarbon gases in the Solim?es basin,north-west Brazil.Mar Pet Geol,71:168-182
    Monin J C,Barth D,Perrut M,EspitaliéM,Durand B.1988.Extraction of hydrocarbons from sedimentary rocks by supercritical carbon dioxide.Org Geochem,13:1079-1086
    Moore C M,Mills M M,Arrigo K R,Berman-Frank I,Bopp L,Boyd PW,Galbraith E D,Geider R J,Guieu C,Jaccard S L,Jickells T D,La Roche J,Lenton T M,Mahowald N M,Mara?ón E,Marinov I,Moore J K,Nakatsuka T,Oschlies A,Saito M A,Thingstad T F,Tsuda A,Ulloa O.2013.Processes and patterns of oceanic nutrient limitation.Nat Geosci,6:701-710
    Moore J,Adams M,Allis R,Lutz S,Rauzi S.2005.Mineralogical and geochemical consequences of the long-term presence of CO2in natural reservoirs:An example from the Springerville-St.Johns Field,Arizona,and New Mexico,U.S.A.Chem Geol,217:365-385
    Morel F M M,Milligan A J,Saito M A.2003.Marine bioinorganic chemistry:The role of trace metals in the ocean cycles of major nutrients.Treat Geochem,6:113-143
    Neal C,Stanger G.1983.Hydrogen generation from mantle source rocks in Oman.Earth Planet Sci Lett,66:315-320
    Newell K D,Doveton J H,Merriam D F,Lollar B S,Waggoner W M,Magnuson L M.2007.H2-rich and hydrocarbon gas recovered in a deep Precambrian well in Northeastern Kansas.Nat Resour Res,16:277-292
    Nishijima A,Kameoka T,Sato T,Matsubayashi N,Nishimura Y.1998.Catalyst design and development for upgrading aromatic hydrocarbons.Catal Today,45:261-269
    Nyg?rd R,Gutierrez M,Bratli R K,H?eg K.2006.Brittle-ductile transition,shear failure and leakage in shales and mudrocks.Mar Pet Geol,23:201-212
    Oelkers E H,Cole D R.2008.Carbon dioxide sequestration a solution to a global problem.Elements,4:305-310
    Ogawa H,Amagai Y,Koike I,Kaiser K,Benner R.2001.Production of refractory dissolved organic matter by bacteria.Science,292:917-920
    Olgun N?,Duggen S,Andronico D,Kutterolf S,Croot P L,Giammanco S,Censi P,Randazzo L.2013.Possible impacts of volcanic ash emissions of Mount Etna on the primary productivity in the oligotrophic Mediterranean Sea:Results from nutrient-release experiments in seawater.Mar Chem,152:32-42
    Pedersen R B,Rapp H T,Thorseth I H,Lilley M D,Barriga F J A S,Baumberger T,Flesland K,Fonseca R,Früh-Green G L,Jorgensen S L.2010.Discovery of a black smoker vent field and vent fauna at the Arctic Mid-Ocean Ridge.Nat Commun,1:126
    Peter J M,Peltonen P,Scott S D,Simoneit B R T,Kawka O E.1991.14C ages of hydrothermal petroleum and carbonate in Guaymas Basin,Gulf of California:Implications for oil generation,expulsion,and migration.Geology,19:253-256
    Price L C,Wenger L M.1992.The influence of pressure on petroleum generation and maturation as suggested by aqueous pyrolysis.Org Geochem,19:141-159
    Qing H,Bosence D W J,Rose E P F.2001.Dolomitization by penesaline sea water in Early Jurassic peritidal platform carbonates,Gibraltar,western Mediterranean.Sedimentology,48:153-163
    Reeves E P,Seewald J S,Sylva S P.2012.Hydrogen isotope exchange between n-alkanes and water under hydrothermal conditions.Geochim Cosmochim Acta,77:582-599
    Rona P A,Klinkhammer G,Nelsen T A,Trefry J H,Elderfield H.1986.Black smokers,massive sulphides and vent biota at the Mid-Atlantic Ridge.Nature,321:33-37
    Saxby J D,Riley K W.1984.Petroleum generation by laboratory-scale pyrolysis over six years simulating conditions in a subsiding basin.Nature,308:177-179
    Schimmelmann A,Lewan M D,Wintsch R P.1999.D/H isotope ratios of kerogen,bitumen,oil,and water in hydrous pyrolysis of source rocks containing kerogen types I,II,IIS,and III.Geochim Cosmochim Acta,63:3751-3766
    Schimmelmann A,Mastalerz M,Gao L,Sauer P E,Topalov K.2009.Dike intrusions into bituminous coal,Illinois Basin:H,C,N,Oisotopic responses to rapid and brief heating.Geochim Cosmochim Acta,73:6264-6281
    Shen Y,Farquhar J,Zhang H,Masterson A,Zhang T,Wing B A.2011.Multiple S-isotopic evidence for episodic shoaling of anoxic water during Late Permian mass extinction.Nat Commun,2:210
    Sherwood Lollar B,Onstott T C,Lacrampe-Couloume G,Ballentine CJ.2014.The contribution of the Precambrian continental lithosphere to global H2production.Nature,516:379-382
    Shiraki R,Dunn T L.2000.Experimental study on water-rock interactions during CO2flooding in the Tensleep Formation,Wyoming,USA.Appl Geochem,15:265-279
    Simoneit B R T.1984.Hydrothermal effects on organic matter-High vs low temperature components.Org Geochem,6:857-864
    Simoneit B R T.1990.Selected papers from the symposium:Organic matter in hydrothermal systems-maturation,migration and biogeochemistry at the third chemical congress of North America and the195th American chemical society national meeting.Appl Geochem,5:1-15
    Simoneit B R T,Aboul-Kassim T A T,Tiercelin J J.2000.Hydrothermal petroleum from lacustrine sedimentary organic matter in the East African Rift.Appl Geochem,15:355-368
    Simoneit B R T,Lonsdale P F.1982.Hydrothermal petroleum in mineralized mounds at the seabed of Guaymas Basin.Nature,295:198-202
    Simoneit B R T,Kvenvolden K A.1994.Comparison of14C ages of hydrothermal petroleums.Org Geochem,21:525-529
    Simoneit B R T,Lein A Y,Peresypkin V I,Osipov G A.2004.Composition and origin of hydrothermal petroleum and associated lipids in the sulfide deposits of the Rainbow field(Mid-Atlantic Ridge at 36°N).Geochim Cosmochim Acta,68:2275-2294
    S?owakiewicz M,Tucker M E,Pancost R D,Perri E,Mawson M.2013.Upper Permian(Zechstein)microbialites:Supratidal through deep subtidal deposition,source rock,and reservoir potential.AAPGBull,97:1921-1936
    Suda K,Ueno Y,Yoshizaki M,Nakamura H,Kurokawa K,Nishiyama E,Yoshino K,Hongoh Y,Kawachi K,Omori S,Yamada K,Yoshida N,Maruyama S.2014.Origin of methane in serpentinite-hosted hydrothermal systems:The CH4-H2-H2O hydrogen isotope systematics of the Hakuba Happo hot spring.Earth Planet Sci Lett,386:112-125
    Thayer T P.1966.Serpentinization considered as a constant-volume metasomatic process.Miner Soc Amer,51:685-710
    Tissot B T,Durand B,Espitalie J,Combaz A.1974.Influence of nature and diagenesis of organic matter in formation of petroleum.AAPGBull,58:499-506
    Van Cappellen P,Ingall E D.1994.Benthic phosphorus regeneration,net primary production,and ocean anoxia:A model of the coupled marine biogeochemical cycles of carbon and phosphorus.Paleoceanography,9:677-692
    Vasconcelos C,McKenzie J A.1997.Microbial mediation of modern dolomite precipitation and diagenesis under anoxic conditions(Lagoa Vermelha,Rio de Janeiro,Brazil).J Sediment Res,67:378-390
    Von Damm K L.1990.Seafloor hydrothermal activity:Black smoker chemistry and chimneys.Annu Rev Earth Planet Sci,18:173-204
    Wei J,Ge Q,Yao R,Wen Z,Fang C,Guo L,Xu H,Sun J.2017.Directly converting CO2into a gasoline fuel.Nat Commun,8:15174
    Weitkamp J,Raichle A,Traa Y.2001.Novel zeolite catalysis to create value from surplus aromatics:Preparation of C2+-n-alkanes,a highquality synthetic steamcracker feedstock.Appl Catal A-General,222:277-297
    Welhan J A,Craig H.1979.Methane and hydrogen in East Pacific rise hydrothermal fluids.Geophys Res Lett,6:829-831
    Wilkinson M,Haszeldine R S,Fallick A E,Odling N,Stoker S J,Gatliff R W.2009.CO2-mineral reaction in a natural analogue for CO2storage-Implications for modeling.J Sediment Res,79:486-494
    Woolnough W G.1934.Natural gas in Australia and New Guinea.AAPG Bull,18:226-242
    Worden R H.2006.Dawsonite cement in the Triassic Lam Formation,Shabwa Basin,Yemen:A natural analogue for a potential mineral product of subsurface CO2storage for greenhouse gas reduction.Mar Pet Geol,23:61-77
    Yamanaka T,Ishibashi J,Hashimoto J.2000.Organic Geochemistry of hydrothermal petroleum generated in the submarine Wakamiko caldera,southern Kyushu,Japan.Org Geochem,31:1117-1132
    Zhang G,Zhang X,Hu D,Li D,Algeo T J,Farquhar J,Henderson C M,Qin L,Shen M,Shen D,Schoepfer S D,Chen K,Shen Y.2017.Redox chemistry changes in the Panthalassic Ocean linked to the end-Permian mass extinction and delayed Early Triassic biotic recovery.Proc Natl Acad Sci USA,114:1806-1810
    Zhang S,He K,Hu G,Mi J,Ma Q,Liu K,Tang Y.2018.Unique chemical and isotopic characteristics and origins of natural gases in the Paleozoic marine formations in the Sichuan Basin,SW China:Isotope fractionation of deep and high mature carbonate reservoir gases.Mar Pet Geol,89:68-82
    Zhang S,Mi J,He K.2013.Synthesis of hydrocarbon gases from four different carbon sources and hydrogen gas using a gold-tube system by Fischer-Tropsch method.Chem Geol,349-350:27-35
    Zhong L,Cantrell K,Mitroshkov A,Shewell J.2014.Mobilization and transport of organic compounds from reservoir rock and caprock in geological carbon sequestration sites.Environ Earth Sci,71:4261-4272
    Zhu D,Liu Q,Jin Z,Meng Q,Hu W.2017.Effects of deep fluids on hydrocarbon generation and accumulation in Chinese Petroliferous Basins.Acta Geol Sin-Engl Ed,91:301-319
    Zhu D,Meng Q,Jin Z,Liu Q,Hu W.2015a.Formation mechanism of deep Cambrian dolomite reservoirs in the Tarim basin,northwestern China.Mar Pet Geol,59:232-244
    Zhu D,Meng Q,Liu Q,Zhou B,Jin Z,Hu W.2018.Natural enhancement and mobility of oil reservoirs by supercritical CO2and implication for vertical multi-trap CO2geological storage.J Pet Sci Eng,161:77-95
    Zhu D,Meng Q,Jin Z,Hu W.2015b.Fluid environment for preservation of pore spaces in a deep dolomite reservoir.Geofluids,15:527-545
    Zhu J,Li S,SunXZhu J,Xin M,Xu H.1994.Discovery of early tertiary hydrothermal activity and its significance in oil/gas geology,Dongpu Depression,Henan Province,China.Chin J Geochem,13:270-283

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700