The results of recent stress measurements along the San Andreas fault near Palmdale, California, which show a rapid decrease in shear stress in the proximity of the fault, may be due to the stress drop connected with the great 1857 earthquake, superimposed onto a preseismic ground deformation. This suggestion is made on the basis of a fault model where a preseismic phase of stable sliding at depth is responsible, through stress concentration, for the occurrence of seismic ruptures in the upper lithosphere.
Interpretation of a stress profile across the San Andreas fault / Bonafede, Maurizio; Boschi, Enzo; Dragoni, Michele. - In: ANNALES GEOPHYSICAE. - ISSN 0755-0685. - STAMPA. - 1:3(1983), pp. 195-198.
Interpretation of a stress profile across the San Andreas fault
Bonafede, Maurizio;Boschi, Enzo;Dragoni, Michele
1983
Abstract
The results of recent stress measurements along the San Andreas fault near Palmdale, California, which show a rapid decrease in shear stress in the proximity of the fault, may be due to the stress drop connected with the great 1857 earthquake, superimposed onto a preseismic ground deformation. This suggestion is made on the basis of a fault model where a preseismic phase of stable sliding at depth is responsible, through stress concentration, for the occurrence of seismic ruptures in the upper lithosphere.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.