Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1162
Title: IPOTESI DI UN MODELLO DI CROSTA SUPERIORE PER LE AREE GEOTERMICHE TOSCANE
Authors: GIANELLI, G.
Keywords: faglia e rocce di faglia - alterazione idrotermale - interazione acqua-roccia - campo geotermico
fault and fault rocks - brittle-ductile boundary - hydrothermal alteration - rock-water interaction - geothermal field
Issue Date: 1994
Publisher: Università di Camerino
Citation: Studi geologici camerti, n. speciale, 1994, pp.195-200
Abstract: Phyllite, micaschist and gneiss, found in the intermediate-deep geothermal wells in Tuscany, show evidence of faults, joints and dilational veins atpresent-day temperatures of350- 450°C. Fluid inclusions in hydrothermal quartz associated with biotite and tourmaline show trapping temperatures higher than 550°C. [...]
URI: http://193.204.8.201:8080/jspui/handle/1336/517
ISSN: 0392-0631
Appears in Volumess:1994/1: "Studi preliminari all'acquisizione dati del profilo CROP 18 Larderello-M.te Amiata"

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