Application of this relation to the 82 profiles gives (Formula presented.). The narrowness of that range can be explained if the primary source of heat on the subduction interface is frictional heating during earthquakes with shear stresses limited by thermal pressurization of pore fluids. Apparent ...
We examine seismic waveforms generated by clusters of similar earthquakes and additional events located on the Karadere-Duzce branch of the North Anatolian fault to investigate possible scaling between proposed early signals in the P waveforms and magnitudes. The employed signals can be divided into ...
The spatial and chronologic distribution and intensity of the various types of deformation structures suggest that they were produced around different epicenters repeated by earthquakes of varying magnitudes associated with the synsedimentary strike-slip tectonics....