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- W1966285477 abstract "Abstract Increased seawater circulation within a carbonate platform, generated through transgression and flooding of the platform, is proposed here as a cause of the common selective dolomitization of calcitic silts in the upper part of limestone sequences of the Barremian-Aptian Urgonian platform of SE France, which underwent selective porosity creation as a result of karstification during an Aptian relative sea-level fall. Parts of this porosity are infilled by microcrystalline dolomite, and some of the host limestone is partially to completely dolomitized. The microcrystalline dolomite is considered to have formed by dolomitization of calcitic silt internal sediment within the karstic cavities as a result of the pumping of seawater through the upper layers of the platform during subsequent transgression. The calcitic silt provided abundant nucleation sites for the dolomitization. Seawater dolomitization following subaerial exposure of limestone is likely to be a common phenomenon if there is sufficient meteoric diagenesis and porosity production and a prolonged period of submarine erosion, winnowing and condensed sequence formation, enhancing the amount of circulation of seawater as seafloor sediment is lithified." @default.
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- W1966285477 date "1996-12-01" @default.
- W1966285477 modified "2023-10-14" @default.
- W1966285477 title "Dolomitization associated with transgressive surfaces— a mid-Cretaceous example" @default.
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- W1966285477 doi "https://doi.org/10.1016/s0037-0738(96)00066-8" @default.
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