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Bulletin of the Seismological Society of America; October 1969; v. 59; no. 5; p. 1983-1999
© 1969 Seismological Society of America
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Shear wave velocities in the lower mantle

J. W. FAIRBORN*

DEPARTMENT OF GEOLOGY AND GEOPHYSICS MASSACHUSETTS INSTITUTE OF TECHNOLOGY, CAMBRIDGE, MASSACHUSETTS

Abstract

The Large Aperture Seismic Array in eastern Montana was used to measure the travel times and dT/d{Delta} of earthquake-generated shear waves for the purpose of determining lower-mantle shear velocities. The data were limited to epicentral distances between 27 and 95 degrees. To convert uncertainties in the dT/d{Delta} measurements to uncertainties in the computed velocities, the data were inverted by a Monte Carlo procedure. The computer randomly generated velocity models, and those which satisfied prescribed travel time and dT/d{Delta}-versus-{Delta} limits were considered as possible models for the real earth. The dT/d{Delta} curve possessed anomalously steep slopes between 27-30 and 65-75 degrees, and the corresponding velocity models had increased gradients between the approximate depths of 700-800 and 1550-2100 kilometers. The slope of the dT/d{Delta} curve also decreased at about 88 degrees which may indicate a decrease in velocity gradient several hundred kilometers above the core-mantle boundary. For epicentral distances greater than 27 degrees the observed travel times to LASA were greater than the expected J-B times. Although vague, a systematic increase in the observed residuals appeared to exist between 40 and 60 degrees which agreed with the J-B residuals of the computed models.

Footnotes

* Now at Chevron Oil Field Research Company, La Habra, California.




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