Heterogeneities in the mantle transition zone from observations of P-to-SV converted waves

Details Heterogeneities in the mantle transition zone from observations of P-to-SV converted waves Heterogeneities in the mantle transition zone from observations of P-to-SV converted waves

Oct 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983pepi...33..149v&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 33, Issue 3, p. 149-163.

Physics

32

Scientific paper

The method of detection of P-to-SV converted waves from distant earthquakes (Vinnik, 1977) was applied to sets of long-period records from a few seismograph stations in Europe and the west of North America. The results obtained suggest that the converted phases related to the major boundaries in the mantle can be reliably detected and the depths of conversion evaluated with an accuracy of a few kilometres. The depth of the olivine-spinel transition is close to 400 km and no difference between the estimates for the north of Europe and the west of North America is found. The depth of the boundary separating the upper and lower mantle is close to 640 km, which is 30 km less than in the recent Earth-reference models. Fine S velocity stratification of this transition changes laterally from a high-gradient layer 50 km thick, terminated at the bottom by a sharp discontinuity, to a gradient layer 100 km or more thick without the discontinuity. A striking anomaly of the mantle transition zone is found in the Rio Grande rift area where a well pronounced boundary is found at 510 km depth.

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