A multidisciplinary study of the dolomitized bodies present among the Late Triassic to Late Cretaceous
carbonate deposits of the Monti Lattari belt (Southern Apennines of Italy) compares the different
dolomitization styles present within this succession of these Mesozoic platform carbonates and furnishes
an overview of their formative genetic models. The revealing traces of the diverse modes of diagenesis in this
region include both surface and subsurface mechanisms, utilizing: a geometric reconstruction of the
dolomitized bodies, an integrated facies and petrographic analysis of the components, and a geochemical
characterization of the sediments including detailed mineralogy and associated stable isotope values
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