TY - JOUR
T1 - Simulation and properties of a non-homogeneous spring-block earthquake model with asperities
AU - Muñoz-Diosdado, Alejandro
AU - Rudolf-Navarro, Adolfo H.
AU - Angulo-Brown, Fernando
PY - 2012/6
Y1 - 2012/6
N2 - The spring-block model proposed by Olami, Feder and Christensen (OFC) has several properties that are similar to those observed in real seismicity. In this paper we propose a modification of the original model in order to take into account that in a real fault there are several regions with different properties (non-homogeneity). We define regions in the network that is reminiscent of the real seismic fault, with different sizes and elastic parameter values. We obtain the Gutenberg-Richter law for the synthetic earthquake distributions of magnitude and the stair-shaped plots for the cumulative seismicity. Again, as in the OFC-homogeneous case, we obtain the stability for the cumulative seismicity stair-shaped graphs in the long-term situation; this means that the straight line slopes that are superior bounds of the staircases have a behavior akin to the homogeneous case. We show that with this non-homogeneous OFC model it is possible to include the asperity concept to describe high-stress zones in the fault.
AB - The spring-block model proposed by Olami, Feder and Christensen (OFC) has several properties that are similar to those observed in real seismicity. In this paper we propose a modification of the original model in order to take into account that in a real fault there are several regions with different properties (non-homogeneity). We define regions in the network that is reminiscent of the real seismic fault, with different sizes and elastic parameter values. We obtain the Gutenberg-Richter law for the synthetic earthquake distributions of magnitude and the stair-shaped plots for the cumulative seismicity. Again, as in the OFC-homogeneous case, we obtain the stability for the cumulative seismicity stair-shaped graphs in the long-term situation; this means that the straight line slopes that are superior bounds of the staircases have a behavior akin to the homogeneous case. We show that with this non-homogeneous OFC model it is possible to include the asperity concept to describe high-stress zones in the fault.
KW - OFC model
KW - cellular automata
KW - earthquake
KW - faulting
UR - http://www.scopus.com/inward/record.url?scp=84860486997&partnerID=8YFLogxK
U2 - 10.2478/s11600-012-0027-7
DO - 10.2478/s11600-012-0027-7
M3 - Artículo
SN - 1895-6572
VL - 60
SP - 740
EP - 757
JO - Acta Geophysica
JF - Acta Geophysica
IS - 3
ER -