A planar seismic source approximates a real fault. In nature, several faults are activated in the volume during a quake and are rather undulated. In the shallow cold crustal layer, rocks are disaggregated in a breccia, whose thickness varies with tectonic style, being larger in extensional settings.

Double-couple troubles

Davide Zaccagnino
Primo
;
Carlo Doglioni
Secondo
2022

Abstract

A planar seismic source approximates a real fault. In nature, several faults are activated in the volume during a quake and are rather undulated. In the shallow cold crustal layer, rocks are disaggregated in a breccia, whose thickness varies with tectonic style, being larger in extensional settings.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/1657742
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