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Bulletin of the Seismological Society of America; February 1966; v. 56; no. 1; p. 119-124
© 1966 Seismological Society of America
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A comparison of earthquake magnitude with T-phase strength

R. H. JOHNSON and J. NORTHROP

HAWAII INSTITUTE OF GEOPHYSICS UNIVERSITY OF HAWAII,, HONOLULU, HAWAII
SCRIPPS INSTITUTION OF OCEANOGRAPHY, UNIVERSITY OF CALIFORNIA,, SAN DIEGOHAWAII INSTITUTE OF GEOPHYSICS

Abstract

Records from SOFAR-depth hydrophones at widely spaced locations in the North Pacific were scanned for earthquake T phases. A source solution was obtained by computer for T-phase arrivals correlated at four or more hydrophones. Using this method, the number of events located on the North Pacific rim is about ten times greater than the number located by conventional body-wave determinations. It is concluded that the capability for location of earthquakes by T-phase arrivals extends down to about magnitude 3.6 for the North Pacific rim.




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