Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1075
Title: DENSITA' DI FLUSSO DI CALORE DAL MAR LIGURE ALLE ALPI ORIENTALI
Authors: PASQUALE, V.
VERDOYA, M.
CHIOZZI, P.
Keywords: Campo geotermico - bacino marginale ligure - estensione litosferica - sovrascorrimenti appenninici e sudalpini
Geothermal field - Ligurian marginal basin - lithospheric stretching - Apennines and southern Alps overthru­stings
Issue Date: 1992
Publisher: Università di Camerino
Citation: Studi geologici camerti, n. speciale, 1992, pp.115-122
Abstract: We discuss the thermal-flux field in connection with the geologica! and geodynamical framework in the areas adjacent to profile CROP 1-lA. In the Hercynian units and in the convergent ones of Alpine age, the thermal flux is around 60-85 mW/m2, excepting the Pedealpine-Adriatic homocline and the more external arcuate systems of the southern Alps and northern Apennines, showing lower heat-flux values, which may be partly due to the thermal effect of post-Miocenic overthrustings. [...]
URI: http://193.204.8.201:8080/jspui/handle/1336/434
ISSN: 0392-0631
Appears in Volumess:1992/2: "Studi preliminari all'acquisizione dati del profilo CROP 1-1A La Spezia-Alpi orientali"

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