The Sogli Bianchi face in the Pasubio Massif (Venetian Alps) shows a well exposed roll-over anticline. The structure originated by a hanging wall bending in response to slip on a normal listric fault dipping towards the SE. The age of the deformation suggests that the rapid Sinemurian relative sea-level rise recorded throughout the Trento platform by the deposition of the oolitic Middle Member of the Calcari Grigi Fm was caused by a tectonic collapse.
L'anticlinale di rollover liassica dei Sogli Bianchi nel Monte Pasubio (Vicenza)
ZAMPIERI, DARIO
1995
Abstract
The Sogli Bianchi face in the Pasubio Massif (Venetian Alps) shows a well exposed roll-over anticline. The structure originated by a hanging wall bending in response to slip on a normal listric fault dipping towards the SE. The age of the deformation suggests that the rapid Sinemurian relative sea-level rise recorded throughout the Trento platform by the deposition of the oolitic Middle Member of the Calcari Grigi Fm was caused by a tectonic collapse.
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