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...