6) is estimated using the b-values and seismic strain rates.Recurrence interval of large earthquakes in southern parts of the Zagros (7 and 8 years) are shorter than northern parts of the Zagros (19 and 45 years).]]>
p. 199−218
2821-2541
Vol.18/No.4
p. 231−254
2821-2541
Vol.18/No.4
p. 263−273
2821-2541
Vol.18/No.4
p. 219−230
2821-2541
Vol.18/No.4
p. 275−284
2821-2541
Vol.18/No.4
p. 255−262
2821-2541
Vol.18/No.4