The purpose of this work is to analyse the local-site seismic response in the Castel Caldes area, located in an alpine valley (Val di Sole) of the north-western Trentino region. The final result is the seismic microzonation map of this area. The seismic microzonation aims to characterize at a small scale two contiguous localities in which the seismic motion is amplified (and how), due to the lithostratigraphic and geomorphological specific characteristics

Local site seismic response in an alpine valley: seismic microzonation of the Castel Caldes area (North-western Trentino)

Carrer, Michela
2013/2014

Abstract

The purpose of this work is to analyse the local-site seismic response in the Castel Caldes area, located in an alpine valley (Val di Sole) of the north-western Trentino region. The final result is the seismic microzonation map of this area. The seismic microzonation aims to characterize at a small scale two contiguous localities in which the seismic motion is amplified (and how), due to the lithostratigraphic and geomorphological specific characteristics
2013-11-12
seismic microzonation, Vs, subsoil schematization, response spectra, amplification
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.12608/17615