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    Volume 33 Issue 4
    Jul.  2008
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    ZHANG Liang, DU Yuan-sheng, ZUO Jing-xun, ZHOU Qi, 2008. Negative Anomaly of Carbon Isotope from Carbonates of Sinian Dongpo Formation in Ruzhou and Lushan, Henan Province and Its Geological Significance. Earth Science, 33(4): 523-530.
    Citation: ZHANG Liang, DU Yuan-sheng, ZUO Jing-xun, ZHOU Qi, 2008. Negative Anomaly of Carbon Isotope from Carbonates of Sinian Dongpo Formation in Ruzhou and Lushan, Henan Province and Its Geological Significance. Earth Science, 33(4): 523-530.

    Negative Anomaly of Carbon Isotope from Carbonates of Sinian Dongpo Formation in Ruzhou and Lushan, Henan Province and Its Geological Significance

    • Received Date: 2008-04-12
    • Publish Date: 2008-07-25
    • Sinian Dongpo Formation overlying tillite of Luoquan Formation consists mainly of shales, silty shales and siltstones.Lenticular dolomites, dolomitic siltstones and sandstones are unexpectedly found in Dongpo Formation.Soft-sediment reformation occurs in dolomitic siltstones which are inconsistent with the shales of Dongpo Formation.Negative anomaly of δ13C is found in lenticular dolomites and dolomitic siltstones.δ13C of lenticular dolomites is-4.19‰ to-6.18‰ and δ13C of dolomitic siltstones mostly between-2‰ to-4‰.So it is considered that lenticular dolomites, dolomitic siltstones and sandstones in Dongpo Formation, similar to cap dolomite of Sinian and seep carbonates overlying tillite of Sturtian ice-age in South China, have been formed by interaction between CO2 seeped from gas hydrate and Mg2+ in sea water, that is, lenticular dolomites, dolomitic siltstones and sandstones in Dongpo Formation are the cause of formation of cold spring.

       

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