M. Di Filippo et al., Volcano-tectonic structures, gravity and helium in geothermal areas of Tuscany and Latium (Vulsini volcanic district), Italy, GEOTHERMICS, 28(3), 1999, pp. 377-393
Since the early 1980s, geological and structural mapping, gravity, and heli
um soil-gas studies have been performed in the eastern sector of the Vulsin
i Volcanic District (Roman Magmatic Province) in an attempt to locate poten
tial geothermal reservoirs. This area is characterised by an anomalous geot
hermal gradient of >100 degrees C/km, and by widespread hydrothermal minera
lization, thermal springs, high gas fluxes, and fossil and current traverti
ne deposits. The results of these surveys indicate the existence of a numbe
r of fault systems, with N-S and E-W structures that appear to be superimpo
sed on older NW-SE and NE-SW features, Comparison of the results of the var
ious studies also reveals differences in permeability and potential reservo
ir structures at depth. (C) 1999 CNR. Published by Elsevier Science I,td, A
ll rights reserved.