Stress changes induced at neighbouring faults by the June 2000 earthquakes, South Iceland Seismic Zone

• Published in: Terra Nova
• Main Authors: Plateaux, R., Angelier, Jacques, Bergerat, Françoise, Cappa, F., Stefansson, R.
• Other Authors: Géoazur (GEOAZUR 6526), Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS), Institut des Sciences de la Terre de Paris (iSTeP), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Department of Business and Natural Sciences, University of Akureyri
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2010
• Subjects: [SDU.STU]Sciences of the Universe [physics]/Earth Sciences; Leirubakki; Skard; Iceland
• Online Access: https://hal.science/hal-00456864; https://doi.org/10.1111/j.1365-3121.2009.00919.x

International audience The South Iceland Seismic Zone (SISZ) is an E-W trending active transform zone with high seismicity. N-S trending right-lateral strike-slip faults accommodate the left-lateral transform motion. Using seismological data recorded from 1991 to 2007, we carried out stress inversion of focal mechanisms of 1340 earthquakes that affected the Skard and Leirubakki faults, eastern SISZ. Not only did the inversion show typical deviations of stress across the faults, it also revealed anticlockwise and clockwise rotations of stress axes with time. Numerical models of the Leirubakki Fault show that these rotations are consistent with the mechanical effect of a lowered friction coefficient during the post-seismic period relative to the pre-seismic period. The Skard Fault reveals a more complex behaviour associated with a higher post-seismic friction, resulting from a higher density of pre-existing fracturing and probable stress interaction between faults. Our results suggest that faults where micro-earthquakes occur during neighbouring major seismic events may undergo significant stress changes at the scale of several kilometres and on time-scales of several years.