Deep hydrothermal circulation in a granite intrusion beneath Larderello geothermal area (Italy): constraints from mineralogy, fluid inclusions and stable isotopes

A shallow (∼2 km) granite body has been intersected by the MONT-4 well in new producing areas of the Larderello geothermal field. The granite at 2.2–2.5 km and below 3 km underwent pervasive propylitic alteration that is dominated by the assemblage chlorite+adularia+quartz+illite+calcite+albite±epid...

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Veröffentlicht in:Journal of volcanology and geothermal research 2003-08, Vol.126 (3), p.243-262
Hauptverfasser: Boyce, A.J, Fulignati, P, Sbrana, A
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Sprache:eng
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