P-coda at distances 80-120 deg and structure beneath subduction zones - Example of Chile

Details P-coda at distances 80-120 deg and structure beneath subduction zones - Example of Chile P-coda at distances 80-120 deg and structure beneath subduction zones - Example of Chile

Dec 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988georl..15.1479s&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 15, Dec. 1988, p. 1479-1482. Research supported by CNRS.

Physics

1

Chile, Earthquakes, P Waves, Subduction (Geology), Earth Mantle, Radiation Distribution, S Waves

Scientific paper

The strong phases sometimes observed between P and PP for earthquakes at distances between 80 and 120 deg are examined, using the Chilean earthquake of March 5, 1987 as an example. For this earthquake, phases in the P-coda were observed only by European stations. It is suggested that these phases are best explained as reflections and conversions at a strong reflector about 200 km deep. The possible origin of this reflector is examined.

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