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" |
Files in This Item:
File | Description | Size | Format | |
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Vol. Speciale 1994-1 Capitolo 19.pdf | n. speciale, 1994, pp. 195-200 | 521,37 kB | Adobe PDF | View/Open |
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