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Detection of waves converted from P to SV in the mantle Export

Physics of the Earth and Planetary Interiors, Vol. 15, No. 1. (September 1977), pp. 39-45.

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mantle methods receiver-functions seismology

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A method is described for the detection of P to SV converted waves in the long-period P coda. The procedure involves axis rotation, transformation of records to a standard form and stacking of processed records from events of various epicentral distances. When applied to NORSAR records, the procedure detected converted phases corresponding to the boundaries in the 410–440- and 640–690-km depth ranges.


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