Geothermal research in western Campania - southern Italy : a revised interpretation of the qualiano - parete structure
1976
621.44
B177
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...
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