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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2012  >  34(6): 635-640
Fan Min, Xu Liangfa, Liu Weixin, Yu Lingjie, Zhang Wentao, Li Zhimin, Tenger, Li Songyang. Experiment geology research of carbonate dolomitization[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(6): 635-640. doi: 10.11781/sysydz201206635
Citation: Fan Min, Xu Liangfa, Liu Weixin, Yu Lingjie, Zhang Wentao, Li Zhimin, Tenger, Li Songyang. Experiment geology research of carbonate dolomitization[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(6): 635-640. doi: 10.11781/sysydz201206635
shu

Experiment geology research of carbonate dolomitization

doi: 10.11781/sysydz201206635
  • 1.

    Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • 2. Beijing University of Posts and Telecommunications, Beijing 100876, China

  • Received Date: 2012-06-20
  • Rev Recd Date: 2012-11-05
  • Publish Date: 2012-11-28
    Abstract
  • According to the dynamic mechanisms of dissolution and preciptation of carbonate rocks,two modelling approaches for dolomitization were proposed: 1)repeated heating and cooling;2)convectional circulation.The modelling products were characterized using several different instruments.The results suggested that dolomites could be obtained by both of the two methods.Through thermodynamic analysis and experimental study,the influences of Mg/Ca concentration ratio,sulfate ion and temperature on dolomitization process were discussed.The study suggested that it was hard to obtain dolomite in the lab because of the difficulty in the growth of dolomite germ.Once the germ appeard,the growing speed of dolomite would be faster than that of calcite.This paper explained why no young age dolomite exists in the natural environment and supplied new thoughts on dolomitization research and carbonate reservoir prediction.

     

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    • References(24)
  • [1]
    Badiozamani K.The Dorag dolomitization model:Application to the Middle Ordovician of Wisconsin[J].Journal of Sedimentary Petrology,1973,43:965-984.
    [2]
    Luczaj J A.Evidence against the Dorag(Mixing-Zone)model for dolomitization along the Wisconsin arch:A case for hydrothermal diagenesis[J].AAPG Bulletin,2006,90:1719-1738.
    [3]
    Luczaj J A,Harrison III W B,Williams N S.Fractured hydrothermal dolomite reservoirs in the Devonian Dundee Formation of the central Michigan Basin[J].AAPG Bulletin,2006,90:1787-1801.
    [4]
    Luczaj J A.Sulfur isotopes from Mississippi Valley-Type mineralization in Eastern Wisconsin//Day J,Luczaj J A.New perspecives and advances in understanding of Lower and Middle Paleozoic,2006,25:137-142.
    [5]
    Luczaj J A.Evidence against the Dorag(mixingzone)model for dolomitization along the Wisconsin arch: A case for hydrothermal diagenesis[J].AAPG Bulletin,2006,90(11):1719-1738.
    [6]
    Vasconcels C,McKenzis J A,Bernasconi S,et al.Microbial dolomite precipitation using sulfate reducing and halophilic bacteria:Results from Qinghai Lake,Tibetan Plateau,NW China[J].Nature,2010,377:220-222.
    [7]
    Shi Xiaoying,Zhang Chuanheng,Jiang Ganqing,et al.Microbial nucleation of Mg-rich dolomite in exopolymeric substancesunder anoxic modern seawater salinity:New insight into an old enigma[J].Journal of China University of Geosciences,2008,19(5):549-566.
    [8]
    范明,蒋小琼,刘伟新,等.不同温度条件下CO2对碳酸盐岩的溶蚀作用[J].沉积学报,2007,25(6):39-44.
    [9]
    范明,胡凯,蒋小琼,等.有机酸及H2S水溶液对碳酸盐岩储层的改造作用[J].地球化学,2008,30(6):643-647.
    [10]
    罗开平,黄泽光,蒋小琼,等.川东北地区优质碳酸盐岩储层改造机制探讨[J].石油实验地质,2011,33(6):559-563.
    [11]
    鲍云杰,王恕一,蒋小琼,等.建南气田飞三段储层成岩作用研究[J].石油实验地质,2011,33(6): 564-568.
    [12]
    管宏林,蒋小琼,王恕一,等.普光气田与建南气田长兴组、飞仙关组储层对比研究[J].石油实验地质,2010,32(2):130-135.
    [13]
    李亚辉,段宏亮,邱旭明,等.苏北盆地古潜山岩溶储层形成机制探讨[J].石油实验地质,2011,33(5):495-498.
    [14]
    孙国昕,杨玉芳,江胜国,等.塔中寒武—奥陶系白云岩储层特征及主控因素[J].断块油气田,2010,17(3):257-261.
    [15]
    李得立,谭先锋,夏敏全,等.东营凹陷沙四段湖相白云岩沉积特征及成因[J].断块油气田,2010,17(4):418-422.
    [16]
    付金华,王宝清,孙六一,等.鄂尔多斯盆地苏里格地区奥陶系马家沟组白云石化[J].石油实验地质,2011,33(3):266-273.
    [17]
    邢秀娟,焦存礼,王毅.塔北地区寒武系白云岩特征与成因研究[J].石油实验地质,2011,33(2):130-136.
    [18]
    王恕一,蒋小琼,管宏林,等.川东北普光气田下三叠统飞仙关组储层成岩作用研究[J].石油实验地质,2010,32(4):366-372.
    [19]
    陈莉琼,沈昭国,侯方浩,等.四川盆地三叠纪蒸发岩盆地形成环境及白云岩储层[J].石油实验地质,2010,32(4):334-346.
    [20]
    Wood J R,Hewett T A.Fluid convection and mass transfer in porous sandstones:a theoretical model[J].Geochim et Cosmochim Acta,1982,46:1707-1713.
    [21]
    Wood J R,Hewett T A Reservoir diagenesis and convective fluid flow[M]//McDonald D A,Surdam R C.Clastic Diagenesis,AAPG Memior 37.Tulsa:AAPG Press,1984:99-110.
    [22]
    Dean J A.Lange's handbook of chemistry[M].15th ed.Beijing:Beijing World Pub,1999:6.8-6.142.
    [23]
    林传仙,白正华,张哲儒.矿物及有关化合物热力学数据手册[M].北京:科学出版社,1985:13-265.
    [24]
    Lippmann F.Stable and metastable solubility diagrams for the system CaCO3-MgCO3-H2O at ordinary temperatures[J].Bull Mineral,1982,105:273-279.(编辑 徐文明)
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