Seismic-Scale Evidence of Thrust-Perpendicular Normal Faulting in the Western Outer Carpathians, Poland

Based on the interpretation of 2D seismic profiles integrated with surface geological investigations, a mechanism responsible for the formation of a large scale normal fault zone has been proposed. The fault, here referred to as the Rycerka Fault, has a predominantly normal dip-slip component with t...

Description complète

Enregistré dans:
Détails bibliographiques
Auteurs principaux: Jan Barmuta, Krzysztof Starzec, Wojciech Schnabel
Format: article
Langue:EN
Publié: MDPI AG 2021
Sujets:
Accès en ligne:https://doaj.org/article/8d6d944283c44a35aebefa83b967b33d
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!