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The AAPG/Datapages Combined Publications Database
Environmental Geosciences (DEG)
Abstract
A Geochemical Survey of the Telese Hypothermal Spring, Southern Italy: Sulfate Anomalies Induced by Crustal Deformation
1 Dipartimento di Scienze Geologiche, University of Basilicata, Campus Macchia Romana, 85100 Potenza, Italy
2 Dipartimento di Scienze Geologiche, University of Basilicata, Campus Macchia Romana, 85100 Potenza, Italy
3 Dipartimento di Chimica e Fisica della Terra (C.F.T.A.), University of Palermo, Via Archirafi 36, 90123 Palermo, Italy
Paolo Harabaglia holds a B.S. in geological sciences from the
University of Trieste and an M.S. in earth sciences from MIT. Currently
he is a researcher at the University of Basilicata. His main areas of
research are seismology and global geodynamics. In particular, he is
pursuing an interest in understanding stress diffusion in the crust,
with particular regard to its interaction with deep-seated fluids. He
is also in charge of a local accelerometric network.
Dr. Giovanni holds a B.S. in geological sciences and a Ph.D. in earth
sciences from the University of Bari. From 1993 to the present, he has
been a lecturer in geochemistry at the University of Basilicata. From
1994 to 1996, he has been a coordinator of the Basilicata University
unit of the national project "Composition and evolution of the
continental crust: the crystalline basement in Italy". From 1997 to
1998, he has been a coordinator of the Basilicata University unit of
the national project "Modelization of the petrographic and geochemical
composition of the continental crust in selected Italian areas." In
1997, he won the "L. Dell’Anna" award, Association International
pour l’Etude des Argiles. His areas of research specialization
are sedimentary geochemistry and waterrock interaction processes.
Michele Paternoster received his B.S. in geological sciences in 1999
from the University of Basilicata-Potenza, and is currently pursuing a
Ph.D. in geochemistry from the University of Palermo. His current
interests include water-rock interaction processes, fluids
geochemistry, and the significance of earthquake-related anomalies in
fluids.
ABSTRACT
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