faulting in the study area, we used the Coulomb v3.3 application (Toda et al., 2005) which resolves the shear and normal components of the stress change on a grid or on specified ‘receiver’ fault planes, of a homogeneous
faulting in the study area, we used the Coulomb v3.3application (Toda et al., 2005) which resolves the shearand normal components of the stress change on a gridor on specified ‘receiver’ fault planes, of a homogeneous