Sedimentary facies analysis of a high-frequency, small-scale, peritidal carbonate sequence in the Lower Jurassic of the Tripolis carbonate unit (central western Crete, Greece): Long-lasting emergence and fossil laminar dolocretes horizons
Keywords: External Hellenides; Lower Jurassic; Tripolis carbonate unit; Peritidal environment; Cyclothems; Penesaline dolomites; Dolocrete horizons; “flower spar” dolomite cement