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 / Zaccagnino, Davide; Doglioni, Carlo. - (2022).
Double-couple troubles
Davide Zaccagnino
Primo
;Carlo DoglioniSecondo
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.File allegati a questo prodotto
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