Seismic velocity structure using array data

Details Seismic velocity structure using array data Seismic velocity structure using array data

Jan 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981pepi...24...33d&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 24, Issue 1, p. 33-52.

Physics

4

Scientific paper

The fine structure of regional travel-time curves is investigated. About 200 events from the region north of Australia, recorded at the Warramunga array, are analysed to give the P-wave velocity structure for that region. The events were confined to a very narrow azimuth range. Results show that the 20° discontinuity is more complicated than a single velocity increase near 400 km depth, and that there are regions of rapid or discontinuous velocity increase at depths below 650 km.

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