The Thermal Structure of the Upper Crust in Central-Southern Italy and its Correlation with the Distribution of Geothermal Resources

Autor: Gola G.[1], Botteghi S.[1], Brozzetti F.[2], Chiarabba C.[3], De Nardis R.[2], Ferrarini F.[2], Groppelli G.[4], Lavecchia G.[2], Limoni P.P.[5], Montanari D.[6], Norini G.[4], Petracchini L.[7], Polemio M.[5], Santaloia F.[5], Santilano A.[1], Scrocca D.[7], Trumpy E.[1], Manzella A.[1]

Publikováno v: World Geothermal Congress (WGC) 2020+1, pp. 1–7, Reykjavik, Iceland, April-October 2021
info:cnr-pdr/source/autori:Gola G.[1], Botteghi S.[1], Brozzetti F.[2], Chiarabba C.[3], De Nardis R.[2], Ferrarini F.[2], Groppelli G.[4], Lavecchia G.[2], Limoni P.P.[5], Montanari D.[6], Norini G.[4], Petracchini L.[7], Polemio M.[5], Santaloia F.[5], Santilano A.[1], Scrocca D.[7], Trumpy E.[1], Manzella A.[1]/congresso_nome:World Geothermal Congress (WGC) 2020+1/congresso_luogo:Reykjavik, Iceland/congresso_data:April-October 2021/anno:2021/pagina_da:1/pagina_a:7/intervallo_pagine:1–7

Temperature is a key parameter in controlling the in-situ petrophysical properties, the solid and fluid phase equilibria, the stress-strain relationships as well as the occurrence and potential of geothermal resources. Thermal field anomalies are det

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::e88c7ac7285a42103eae49a53d206c7c
https://publications.cnr.it/doc/459224