Deep fluid circulation in the Travale geothermal area and its relation with tectonic structure investigated by a magnetotelluric survey

Autor: Manzella A. (1), Spichack V. (2), Pushkarev P. (3), Sileva D. (3), Oskooi B. (4), Ruggieri G. (1), Sizov Yu. (2)

Publikováno v: Thirty-First Workshop on Geothermal energy Reservoir Engineering, Stanford, California, 30 Gennaio-1 Febbraio 2006
info:cnr-pdr/source/autori:Manzella A. (1), Spichack V. (2), Pushkarev P. (3), Sileva D. (3), Oskooi B. (4), Ruggieri G. (1), Sizov Yu. (2)/congresso_nome:Thirty-First Workshop on Geothermal energy Reservoir Engineering/congresso_luogo:Stanford, California/congresso_data:30 Gennaio-1 Febbraio 2006/anno:2006/pagina_da:/pagina_a:/intervallo_pagine

The high enthalpy Italian geothermal fields are located in southern Tuscany and are characterized by shallow and deep reservoirs defined by fractures within sedimentary or metamorphic rocks, showing an apparent heterogeneously distributed permeabilit

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::b131302885fb5b2a67a54532aab4fc7c
http://www.cnr.it/prodotto/i/256275