Writers : Hasanzade,Hamid;Zare,mahdi;gharashi,Manouchehr
Refference : The 20th Symposium on Geoscience;Tehran
Publishing Year : 1380

Abstract :
Displacement of both side blocks of a rupture associated with an earthquake، cause changes in static stress around the rupture and these stress changes effect on the slip planes by load adding and load removing. The stress change on the receiver planes near the source fault are calculable with Coulomb stress method. In this paper، static stress changes cause by 1968 Dashte Bayaz earthquake on the ruptures associated with Qaenat earhuqakes that occurred later، have been calculated by coulomb.
Subject List : Seismic