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- W2891969680 abstract "The messinian evaporitic sediments embedded between lacustrine clays and the Pycnodonta clays, outcropping in the Montalcinello area, exhibit the following sedimentary characters : - at the base of the sequence, primary selenite reef-like clusters (cavoli) and grass-like structures are made of blades of arrows-head twins, up to 2 meters high. They are embedded in roughly laminated gyps-arenites ; - on the upper part the gyps-arenites develop in fine-grained laminated gypsum with intercalations of sandy lenses or beds. The grain size of those sandy bodies ranges from fine grained to coarse-grained sand, sometimes well sorted, sometimes graded. Parallel and cross lamination are frequent. Lithoclasts, gyps-clasts calcareous peloids and fossils are the most important grains of the arenites. The fossils sometimes very aboundant are mainly represented by serpulids, Chara oogons and steams, ostracods, brakish foraminifera (Ammonia tepida) sometimes associated with Melanopsis, pelecipods and vegetal lignitified debris. The depositional environment of those sediments is ascribed to a low energy confined lagoom characterized by a marine hyperhaline feeding and a fresh-water supply." @default.
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- W2891969680 date "1980-01-01" @default.
- W2891969680 modified "2023-09-26" @default.
- W2891969680 title "Le milieu sédimentaire des gypses messiniens affleurant près de Montalcinello (bassin de Radicondoli, Toscane méridionale Italie)" @default.
- W2891969680 cites W2890468704 @default.
- W2891969680 doi "https://doi.org/10.3406/geolm.1980.1123" @default.
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