Abstract
abstract
A detailed discussion of the data of Part I† is here presented. The departures of surface-wave arrivals from station-to-epicenter great-circle paths, when interpreted on the basis of the theory of ray paths on a spherical shell, are shown to be consistent with the known differences between Pacific and continental structure. It is also shown that the apparent transverse motion in Rayleigh Waves recorded at Berkeley is due to the fact that the arrivals are from other than the station-to-epicenter great-circle path. Thus, the observed motions are consistent with the simple isotropic theory. Experimental phase and group velocity curves for Rayleigh Waves, derived from the observed data, are included. They should apply to the layering in the tripartite area.
† Part I was published in the Bulletin; see Vol. 43, pp. 335-374 (1953).
Publisher
Seismological Society of America (SSA)
Subject
Geochemistry and Petrology,Geophysics
Cited by
25 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献