Vm. Zobin, APPARENT STRESS OF EARTHQUAKES WITHIN THE SHALLOW SUBDUCTION ZONE NEAR KAMCHATKA PENINSULA, Bulletin of the Seismological Society of America, 86(3), 1996, pp. 811-820
Apparent stresses of 105 moderate-sized (magnitude mb from 4.5 to 6.0)
shallow earthquakes from the subduction zone near Kamchatka Peninsula
(NW Pacific) were analyzed. Our results allowed us to formulate the f
ollowing properties of the earthquake apparent stress for the seismic
moment range 10(15) to 10(18) N-m and the focal depth range from 0 to
60 km: (1) Apparent stresses depend on the fault nature of earthquakes
; they are greater for thrusts and smaller for normal faults, a differ
ence of a factor of 3. (2) Average apparent stresses were greater in t
he coastal zone near Kamchatka, where subducting oceanic and overridin
g continental plates interact (2.5 MPa) and just under the trench axis
(2.9 MPa), but lower in near-trench zones on the western slope of the
trench (0.4 MPa); this difference is a factor of 6.