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 …

The Variscan orogeny occurred as a result of the Late Devonian to Late Carboniferous
collision and accretion of Gondwana-derived microcontinents and continental masses with …

This paper summarises the geological features of the Larderello-Travale and Monte Amiata
areas, where the world's most ancient exploited geothermal fields are located. In both …

The Northern Apennines (NA) hinterland area is characterized by a complex Neogene‐
Quaternary tectonics where both crustal extension, associated with the Tyrrhenian Basin …

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 …

A revision of late Palaeozoic tectonics recorded in Tuscany, Calabria and Corsica is here
presented. We propose that, in Tuscany, upper Carboniferous-Permian shallow-marine to …

Abstract The Mt. Amiata mining district (Southern Tuscany, Italy) is a world class Hg district,
with a cumulate production of more than 100,000 tonnes of Hg, mostly occurring between …

This paper and the associated 1: 50,000 geological map are devoted to describe the
geological features of the Monte Amiata region. The tectono-stratigraphic setting of Monte …

Nel lavoro viene illustrata una revisione critica delle conoscenze sulla giacimentologia e
minerogenesi delle principali mineralizzazioni della Toscana, con particolare riferimento a …

Monte Amiata is a small volcano composed by trachytic to olivine latitic lava flows and
domes emplaced in a very short time between 305 and 231 ka. The main petrographic …