The formation of the Tyrrhenian–Apennines system has been characterized by a complex
distribution of major tectonic events, such as opening of basins, migration and distortion of …

The tectonic evolution of the Mt Amiata volcano-geothermal area is under discussion. Some
authors state that this region, as well as the hinterland of the Northern Apennines, were …

In this paper we describe an example of travertine fissure-ridge development along the trace
of a normal fault with metre displacement, located in the eastern margin of the Neogene …

The quaternary volcanic complex of Mount Amiata is located in southern Tuscany (Italy) and
represents the most recent manifestation of the Tuscan Magmatic Province. The region is …

In geothermal areas the evaluation of the active stress field from local earthquakes is
generally contradictory, mainly suggesting normal to strike-slip tectonic regime. This feature …

Carbon dioxide is one of the most important gasses naturally released from geothermal
systems. Establishing the processes and pathways that regulate the CO 2 diffuse degassing …

We have examined the data of 600 geothermal wells and re‐interpreted approximately 500
km seismic profiles through the field of Larderello, Italy. We conclude that the two main …

The back arc extensional area of Tuscany is characterized by anomalously high heat flow as
a result of lithospheric thinning facilitated by locally intruded granite, which ultimately led to …

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 …

This paper presents an integrated study directed toward an understanding of the tectonic
control on the hydrothermal circulation and resulting deposition of Middle–Late Pleistocene …