Tóm tắt
Abstract
Marine facies ranging in age from Liassic to Eocene are present in the Stenico region (southern Alps, Trento province, Italy). The facies represent a transition between the Trentino flexure to the east and the Lombardy depression to the west. Neritic deposits in the Liassic are succeeded by pelagic deposits; pelagic sedimentation predominated from the upper Jurassic through the lower Eocene and became neritic in the middle Eocene. Evidence from brecciated formations indicates that movement at the beginning of the upper Cretaceous caused emergence in certain sections and reworking of submarine deposits in others.
