Quantification of carbon fluxes between solid Earth and its atmosphere is necessary to
understand the global geological carbon cycle. Some of the main CO 2 contributors are …

Abstract The Quaternary Roman Volcanic Province extends for over 200 km along the
Tyrrhenian margin of the Italian peninsula and is composed of several caldera complexes …

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 …

Banded Ca‐carbonate veins in travertine deposits are efficient recorders of the
compositional fluctuations of geothermal fluids flowing (or flowed) from deep reservoirs up to …

Carbon capture and sequestration (CCS) is necessary to mitigate global warming caused by
anthropogenic CO _ 2 CO 2 emissions in the atmosphere. However, due to very high …

We report the results of a multiproxy study that combines structural analysis of a fracture–
stylolite network and isotopic characterization of calcite vein cements and/or fault coating …

A giant carbonate vein (≥ 50 m thick; fissure ridge travertines) and nearby travertine
plateaus in the Semproniano area (Mt. Amiata geothermal field, southern Tuscany, Italy) are …

This study examines the impact of polyphase tectonics on the development of structurally
controlled hydrothermal fluid pathways in carbonate geothermal reservoirs. Our case study …

Rift-basins are the shallow effects of lithosphere-scale extensional processes often
producing polyphase faulting. Their sedimentary evolution depends on the mutual interplay …

Abstract The Neogene–Quaternary Albegna basin (southern Tuscany, central Italy), located
to the south of the active geothermal field of Monte Amiata, hosts fossil and active …