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Abstract

Magnetotelluric and geomagnetic depth soundings have been carried out in the area of the strongest geothermal anomaly in continental Europe - the western part of the Tuscany - in the years 1978 and 1979 to study the distribution of electrical conductivity in the crust and upper mantle. During the same time the crustal structure of Tuscany has been under study by seismic refraction measurements from a German - Italian Research Group. The aim of these projects was to develop a geothermal model of Tuscany.

Additional information

Authors: HAAK J, FREIE UNIVERSITAET BERLIN (GERMANY);SCHWARZ G FREIE UNIVERSITAET BERLIN (GERMANY), FREIE UNIVERSITAET BERLIN (GERMANY)
Bibliographic Reference: EUR 8299 DE (1984) MF, 108 P., BFR 240, EUROFFICE, LUXEMBOURG, POB 1003
Availability: Can be ordered online
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