An outline of the geology of the Italian Northern Apennines, to accompany a geological map
at 1: 250,000 scale covering the Emilia-Romagna, Marche, Tuscany and Umbria regions, is …

Carbonation of ultramafic rocks is a key piece of the global carbon cycle taking place from
the seafloor to the surficial environment and becoming particularly efficient in the genesis of …

We review and refine the geological setting of an area located nearby the Tyrrhenian
seacoast, in the inner zone of the Northern Apennines (southern Tuscany), where a …

Abstract Travertines from Tivoli area (Central Italy) possess abundant shrub-like fabrics that
are laterally continuous over hundreds of square meters. They occur dominantly in …

Comparison between fossil and analogue active geothermal systems permit to obtain key-
parameters to define a conceptual model of the area under exploration. The approach is …

High‐temperature geothermal areas are often characterized by widespread surficial
manifestations, whose location is strictly controlled by sets of faults of regional relevance …

Magma emplacing at shallow crustal levels may cause significant deformation in the
overlying country rock (ie, forced folding, fracturing and faulting), both at a local and/or …

Abstract We studied the Zuccale Fault (ZF) on Elba, part of the Northern Apennines, to
unravel the complex deformation history that is responsible for the remarkable architectural …

Studying travertine deposits and the network of banded calcite veins that form their roots in
the substratum can place important constraints on neotectonic activity and the …

Zones of advanced argillic alteration with general low permeability (ie, lithocaps) are
common place in the shallow parts of porphyry and epithermal ore deposits and active …