The study of exhumed geothermal systems can provide useful information for the understanding of the role of brittle structures in controlling the circulation of geothermal fluids at deeper levels. This offers the possibility to evaluate the secondary permeability within the rock masses and, at same time, to reconstruct the chemical/physical proprieties of fluids through the analyses of mineralization (e.g. fluid inclusions and geochemical analyses).
Geological structures, HT-fluids flow and permeability in the exhumed geothermal system of eastern Elba Island (Italy): the case of Cala Stagnone / Rimondi V.. - In: RENDICONTI ONLINE DELLA SOCIETÀ GEOLOGICA ITALIANA. - ISSN 2035-8008. - ELETTRONICO. - 40:(2016), pp. 141-141. (Intervento presentato al convegno Congresso Società Geologica Italiana tenutosi a Napoli nel 7-9 settembre 2016).
Geological structures, HT-fluids flow and permeability in the exhumed geothermal system of eastern Elba Island (Italy): the case of Cala Stagnone
Rimondi V.
2016
Abstract
The study of exhumed geothermal systems can provide useful information for the understanding of the role of brittle structures in controlling the circulation of geothermal fluids at deeper levels. This offers the possibility to evaluate the secondary permeability within the rock masses and, at same time, to reconstruct the chemical/physical proprieties of fluids through the analyses of mineralization (e.g. fluid inclusions and geochemical analyses).
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