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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 1995  >  17(1): 55-62
Li Shuangying, Jin Fuquan, Wang Daoxuan. GEOCHEMICAL CHARACTERISTICS OF CARBONATE ROCK DIAGENESIS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(1): 55-62. doi: 10.11781/sysydz199501055
Citation: Li Shuangying, Jin Fuquan, Wang Daoxuan. GEOCHEMICAL CHARACTERISTICS OF CARBONATE ROCK DIAGENESIS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(1): 55-62. doi: 10.11781/sysydz199501055
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GEOCHEMICAL CHARACTERISTICS OF CARBONATE ROCK DIAGENESIS

doi: 10.11781/sysydz199501055

  • Department of Resources and Environment Sciences, Hefei University of Technology

  • Received Date: 1993-11-25
  • Publish Date: 1995-01-25
    Abstract
  • The paper deals with the distribution of trace elements,such as Sr.Na,Fe.Mn in carbonate rocks occurred under various diagenetic environments with a case study of the carbonate rocks(Z-T)in the Chao County.The limestones(O,upper part of C1h.C2h.C2c)origined mainly from meteoric diagenesis are characterized by low concentrations of Sr(188ppm),Na(132ppm),Mn(149ppm),while the limestones(Clj,lower part of C1h.P1q,T1n)mainly derived from submarine diagenesis by high concentrations of Sr(515ppm),Na(396ppm),Mn(404ppm).The penecontemporaneous sabkha dolomites(T2d),in comparison with penecontemporaneous-back poly-origin dolomites(Z-∈)which origin mainly from diagenesis dolomitization,has high concentrations of Sr(138ppm),Na(806ppm),and the later have low concentrations of S(103ppm)and Na(604ppm).It is significant for the difference in Mn content between the dolomites.The dolomite rocks,in comparison with the limestones,have high Na and low Sr,Mn.Moreover,it is obvious that Fe content tends to be negative correlation with Ca+Mg content and it is suggested that Fe content should be influenced by terrigenous cleposits.

     

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    • References(14)
  • [1]
    罗宾·巴瑟斯特.碳酸盐沉积物及其成岩作用(中译本),北京:科学出版社,1977
    [2]
    Pingitore Jr.N E The behaviour of Zn2+ and Mn2+ during carbonate diagenesis,theory and application.J.Sed.Petrol.,1978,48,799-814.
    [3]
    王英华等.中、下扬子区海相碳酸盐岩成岩作用研究,北京:科学技术出版社,1991
    [4]
    Land L S.Goreau T F.Submarine Lithification of Jamaican reefs,J.Std.Petrol.,1970 40,457-462
    [5]
    Kinsman D J J.Interpretation of Sr2+ concentrations in carbonate minerals and rocks.J.Sed.Petrol.,1969.39:486-508
    [6]
    Baker P A.and Burns S J.Occurrence and formation of dolomite in organic-rich continental margin sediments.Brell.Am.Ass.Petrol.Ceol.,1985,69.,1917-1930
    [7]
    Tucker M E.and Wright V P.Carbonate sedimentology,Blackwell Scientific Publications.Orford Loxdon.1990.314-400
    [8]
    Wallace M W.Origin of dolomitization on the Barbwire Terrace,Canning Basin,Western Australia,Sedixeextology.1990,37,105-122
    [9]
    Erik Flugel.Microfacies analysis of limestone,Berlin,Springer-Verlag,1982
    [10]
    Churnet H G.and Misra K C.Genetic implications of the trace element distribution pattern in the Upper Knox car-bonate rocks,Copper Ridge District,East Tennessee,Sediment.Gtol.,1981,30;173-194
    [11]
    Cioni R.et al.Sr-distribution and carbonate mineralogy in the "Calcare Masiccio" formation of non一metamorphic Tuscan series.North of Auno River.Boll.Soc.Ctol.,1973.92,363-389
    [12]
    Badiozamani K.The dorag dolomitization model-application to the Middle Ordovician of Wisconsin.J.Sedi-meat.Petrol..1973.43,965-984
    [13]
    Bencini A.and Turi A.Mn distribution in the Mesozoic carbonate rocks from Lima Valley.northern Apennines.J.Sed.Petrod.,1974.44(3)0774 -782
    [14]
    Land L S.and Hoops G K.Sodium in carbonate sediments and rocks:a possible index to the salinity of diagenetic solution.J.Sed.Petrol.,1973.43:614-617
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