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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2011  >  33(1): 56-60
Wang Furong, He Sheng, Yang Xingye. Diagenetic environments of calcite veins hosted in marine carbonate rocks in middle Yangtze region of South China[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(1): 56-60. doi: 10.11781/sysydz201101056
Citation: Wang Furong, He Sheng, Yang Xingye. Diagenetic environments of calcite veins hosted in marine carbonate rocks in middle Yangtze region of South China[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(1): 56-60. doi: 10.11781/sysydz201101056
shu

Diagenetic environments of calcite veins hosted in marine carbonate rocks in middle Yangtze region of South China

doi: 10.11781/sysydz201101056
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan, Hubei 430074, China

  • 2. Faculty of Earth Resources, China University of Geosciences, Wuhan, Hubei 430074, China

  • Received Date: 2010-09-07
  • Rev Recd Date: 2010-12-24
  • Publish Date: 2011-02-28
    Abstract
  • Analyses of thin slices,cathodoluminescence and carbon—oxygen isotope of calcite veins hosted in marine carbonate rocks distributed around Jingshan County in the middle Yangtze region of South China indicated that,two crystal forms including radial calcite and isometric texture calcite could be identified in calcite veins in the Triassic and the cathodoluminescence intensity was different.The Permian and Ordovician fractures were mainly filled with isometric texture calcite veins and the cathodoluminescence intensity was similar with that of the surrounding rocks.The δ13CPDB value of calcite veins ranged from -6.76‰ to 4.01‰ and the δ18OPDB value ranged from -17.95‰ to -5.67‰,indicating the marine phreatic environment and the mixing phreatic environment for calcite veins deposition.Calcite veins in the Triassic were sedimentary origin,and part of calcite veins in the Permian and the Ordovician suffered latter diagenetic fluid dissolution.Fluid generated from organic-matter maturation effected the formation of calcite veins in the Permian to some degree.

     

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    • References(31)
  • [1]
    Suchy Y,Hdilen W,Sykorova I.et al.Geochemical study of calcite veins in the Silurian and Devonian of the Barrandian Basin(Czech Republic):evidence for widespread postVariscan fluid flow in the central part of the Bohemian Massif[J].Sedimentary Geology,2000,131:201-219.
    [2]
    Lee Y J.Morse J W.Calcite precipitation in synthetic veins:implications for the time and fluid volume necessary for vein filling[J].Chemical Geology,1999,156:151-170.
    [3]
    Budd D A,Saller A H.Harris P M.Uneonfc,rmities and Poroslty in Carbonate strata[M]//AAPG Memoir 63.Tulsa,Oklahoma:AAPG,1995.
    [4]
    HayesM J,Boles J R.Evidence for meteoric recharge in the San Joaquin basin.California provided by isotope and trace element chemistry of calcite[J].Marine and Petroleum Geology,1993,10:136-144.
    [5]
    Cicero A D,Lohmann K C.Sr/Mg variation during rock-water interaction;Implications for secular changes in the elemental chemistry of ancient seawater[J].Geochimiea et Cosmochimica Acta,2001,65(5):741-761.
    [6]
    Heward A P.Chuenbunehom S.Makel G,et al.Nang Nuan oil field,B6/27,Gulf of Thailand:karst reservoir of meteoric or deep-burial origin[J].Petroleum Geoscience,2000,6:15-27.
    [7]
    黄文明,刘树根,张长俊,等.四川盆地震旦系储层孔洞形成机理与胶结充填物特征研究[J].石油实验地质,2009,31(5):449-454.
    [8]
    Boles J R.Carbonate Cementation in Tertiary Sandstones,San Joaquin Basin,California[M]//Morad S,ed.Carbonate Cementation in Sandstones:Diistribution Pattems and Geochemical Evolution.New York:John Wiley & Sons Inc,1998.
    [9]
    Heasley E C,Woden R H,Handry J P.Cement distribution in a carbonate reservoir:recognition of a palaeo oil-water contact and its relationship to reservoir quality in the humbly grove field,Onshore,UK[J].Marine and Petroleum Geology,2000,17(2):639-654.
    [10]
    史基安,王金鹏,毛明陆,等.鄂尔多斯盆地西峰油田三叠系延长组长6-8段储层砂岩成岩作用研究[J].沉积学报,2003,21(3):373-380.
    [11]
    刘立,孙晓明,董福湘,等.大港滩海区沙一段下部方解石脉的地球化学与包裹体特征:以港深67井为例[J].吉林大学学报:地球科学版,2004,34(1):49-54.
    [12]
    刘德良,孙先如,李振生,等.鄂尔多斯盆地奥陶系碳酸盐岩脉流体包裹体碳氧同位素分析[J].石油学报,2007,28(3):68-74.
    [13]
    高福红,刘立,邹海峰.大港探区早古生代碳酸盐岩中方解石脉特征[J].世界地质,2001,20(3):257-261.
    [14]
    刘行松,史兰斌,唐汉军,等.方解石脉在断层新活动研究中的应用[J].中国国科学 B辑,1993,23(4):430-436.
    [15]
    李保利,澍忠怀,陈长贞.济阳坳陷早占生代方解石脉成因分析[J].油气地质与采收率,2006,13(5):22-23.
    [16]
    Moore C H.Carbonate Diagenesis and Porosity[M].New York:Elsevier,1989.
    [17]
    钱一雄,陈强路.陈跃,等.碳酸盐岩中缝洞方解石成岩环境的矿物地球化学判识:以塔河油田的沙 79井和沙85井为例[J].沉积学报,2009,27(6):1027-1032.
    [18]
    刘金连,刘伟新,张庆珍,等.电子探针与阴极荧光技术在碳酸盐矿物研究中的应用[J].石油实验地质,2010,32(4):393-396.
    [19]
    Veizer J,Ala D,Azmy K.et al.87Sr/86Sr,δ13C and δ18O evolution of Phanerozoic seawater[J].Chem Geol,1999,161:59-88.
    [20]
    Walter M R,Veevers J J,Calver C R.et al.Dating the 840-544 Ma Neoproterozoic interval by isotopes of strcmfium,carbon,and sulfur in seawater,and some interpretative models[J].Precambrian Research,2000,100:371-433.
    [21]
    黄思静,石和.毛晓冬,等.早古生代海相碳酸盐的成岩蚀变性及其对海水信息的保存性[J].成都理工大学学报(自然科学版),2003,30(1):9-18.
    [22]
    黄思静,卿海若,裴昌蓉,等.川东三叠系飞仙关组自云岩锶含量、锶同位素组成与白云岩化流体[J].岩石学报,2006,22(8):2123-2132.
    [23]
    黄思静,卿海若,胡作维,等.川东三叠系飞仙关组碳酸盐岩的阴极发光特征与成岩作用[J].地球科学:中国地质大学学报,2008,33(1):26-34.
    [24]
    宋志敏.阴极发光地质学基础[M].武汉:中国地质大学出版社,1993.
    [25]
    Allan J R.Wiggins W D.Dolomite reservoirs:Geochemical techniques for evaluating origin and distribution[J].AAPG Short Course Nore Series,1993,36:129-132.
    [26]
    Denies P.The isotopic composition of reduced organic carbon[M]//Fritz P.Fontes J C H,eds.Handbook of Environmental Isotope Geochemistry,Volume 1:The Terrestrial Environment.Atasterdam:Elsevier,1980:329-406.
    [27]
    Keith M L,Weber J N.Geochemistry Cosmoch[J].Asts,1964:1786-1816.
    [28]
    王大锐,张映红.渤海湾油气区火成岩外变质带储集层中碳酸盐胶结物成因研究及意义[J].石油勘探与开发,2001,28(2):40-42.
    [29]
    Kaufman A J,Knoll A H.Neop roterozoic variations in the C-isotopic composition of seawater:stratigraphic and biogeochmical imp lications[J].Precambrian Research,1995,73:27-49.
    [30]
    钱一雄,蔡立国,李国蓉,等.碳酸盐岩岩溶作用的元素地球化学表征:以塔河1号的S60井为例[J].沉积学报,2002,20(4):70-75.
    [31]
    曹剑,胡文瑄,姚索平.等.准噶尔盆地石炭一二叠系方解石脉的碳、氧、锶同位家组成与含油气流体运移[J].沉积学报,2007,25(5):722-729.
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