Baldi, P.

Geothermal research in western Campania - southern Italy: a revised interpretation of the qualiano - parete structure - Pisa: ENEL, 1976 - 14 p. cuadros.

Impreso

06316

The campanian plain is a sinking area of the Tyrrhenian side of the apennine chain, which formed during the plio - quaternary tensional tectonic phases affecting the southern apennines. Subsidence, as estimated from the rate of sedimentation, was shown to be considerable in certain parts of the plain...


Energía Geotérmica
Geotermia
Geología

621.44 / B177