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INSTITUTE OF EARTH AND PLANETARY PHYSICS UNIVERSITY OF ALBERTA, EDMONTON, ALBERTA, Canada, T6G 2J1
Abstract
A new method, using only available array data, is developed to determine the dip and the strike of a major velocity discontinuity such as the Mohorovi
i
discontinuity. The method employs the coherencies of body waves in the P coda from both the vertical and horizontal detectors to obtain the slowness and azimuth of the direct and the converted wave from a major discontinuity. An example is given from array measurements in southern Alberta.
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