Facies character, diagenesis, geochemical signature, porosity, permeability, and geometry
of the upper Pleistocene Tivoli travertines were investigated integrating information from six …

The Mirandola anticline represents a buried fault-propagation fold which has been growing
during Quaternary due to the seismogenic activity of a blind segment belonging to the …

The continental crust involved in the Alpine orogeny was largely shaped by Paleozoic
tectono‐metamorphic and igneous events during oblique collision between Gondwana and …

Fault roughness is a measure of the dimensions and distribution of fault asperities, which
can act as stress concentrators affecting fault frictional behaviour and the dynamics of …

Abstract In the Central Mediterranean the Africa‐Eurasia convergence led to the
development of complex orogenic systems and back‐arc basins. Throughout Pliocene …

For any scientist working in seismotectonics, the Calabrian Arc represents the most
challenging area of Italy. Lying on top of a subduction zone, it is characterised by a complex …

A methodology to evaluate the undrained cyclic resistance of sandy deposits from cone
penetration tests through the state parameter is applied to the case history of the village of …

Deep-seated rock slope failures represent effective mechanisms of natural rock mass-
wasting, able to radically change mountain-valley morphology. In the northern Cottian Alps …

Abstract The 2012 Emilia Romagna (Italy) seismic sequence has been extensively studied
given the occurrence of two mainshocks, both temporally and spatially close to each other …

A main volcanic marker has been identified for the first time on the continental shelf of the
northern Phlegraean Fields in the Gulf of Gaeta (Campania region, eastern Tyrrhenian …