Physics‐Based Earthquake Simulations in Slow‐Moving Faults: A Case Study From the Eastern Betic Shear Zone (SE Iberian Peninsula)
Author:
Affiliation:
1. Department of Geodynamics Stratigraphy and Paleontology Universidad Complutense de Madrid Madrid Spain
2. GNS Science Lower Hutt New Zealand
3. Geosciences Institute (UCM‐CSIC) Madrid Spain
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB021133
Reference113 articles.
1. Alfaro P. Bartolomé R. Borque Arancón M. J. Estévez A. García Mayordomo J. García‐Tortosa F. J. et al. (2012). The Bajo Segura Fault Zone: Active blind thrusting in the Eastern Betic Cordillera (SE Spain).
2. Application of the analytic model of general triclinic transpression with oblique extrusion to an active deformation zone: The Alhama de Murcia Fault (SE Iberian Peninsula)
3. Potencial de encadenamiento de roturas sísmicas en la zona de cizalla de las Béticas Orientales por transferencia de esfuerzos de Coulomb – Seismic ruptures linking potential on the Eastern Betics Shear Zone by Coulomb Stress Transfer;Álvarez‐Gómez J. A.;Avances en el estudio de fallas activas, terremotos y peligrosidad sísmica de Iberia. III Reunión Ibérica sobre Fallas Activas y Paleosismología. Volumen de resúmenes,2018
4. Batlló J. Martínez‐Solares J. M. Macià R. Stich D. Morales J. Garrido L. et al. (2015). The autumn 1919 Torremendo (Jacarilla) earthquake series (SE Spain).
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