P-wave travel time gradient measurements and lower mantle structure

Details P-wave travel time gradient measurements and lower mantle structure P-wave travel time gradient measurements and lower mantle structure

Mar 1970

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1970e%26psl...8...41w&link_type=abstract

Earth and Planetary Science Letters, Volume 8, Issue 1, p. 41-44.

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Scientific paper

535 values of the P-wave travel time gradient have been derived from 192 events recorded at the Warramunga Seismic Array over the distance range 28°-99°. ThesedTdΔ measurements have indicated the presence of regions of anomalous velocity gradient in the lower mantle. The results are compared with those of other recent array investigations.

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