Interpretación sedimentológica y paleogeográfica del nivel de areniscas eocénicas de Sarrià de Ter(Prov. de Gerona)

Abstract

There is in this work a description of sedimentological cliaracters of the medium Eocene sandstone leve1 from Sarriá de Ter (Gerona province* Spain) and an interpretation of their genesis and situation in the regional paleogeography. The conclusion is that these sandstones form a deltaic channel (delta front). To wards the E and NE the become fluvial deposits, to wards the W, Plana de Vic, they become clay and silstones considered as a prodelta.