What is it about?
P and S velocity structure is determined from deep earthquake travel times
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Why is it important?
Velocity determinations are obtained at deep earthquake focal depths
Perspectives
A comparison with the observed seismogram section could be made in this region
Krishna V.G. Dr.
Read the Original
This page is a summary of: Preliminary models of upper mantle P and S wave velocity structure in the western South America region, Journal of Geodynamics, March 1999, Elsevier,
DOI: 10.1016/s0264-3707(98)00016-7.
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