Bulk sound travel times and implications for mantle composition and outer core heterogeneity

We present a new methodology for constraining mantle composition directly from observed seismic travel times. By measuring travel times of PcP, PcS, ScS, and PKiKP phases generated by the Chinese nuclear explosion of 21 May 1992 and recorded at epicentral distances of similar to 10 degrees, we directly determine bulk sound travel times (T-Phi) for the mantle and outer core. This eliminates the need to combine independent V-P and V-S profiles, characterizing different paths and frequencies, to obtain a reference V-Phi profile. Our observed PKiKP - PcP differential travel time indicates that the outer core model of AK135 is slow by 2.1 s (that of IASP91 by 2.3 s) while that of PREM is slow by only 0.7 s and suggests, through comparison with other data, relative lateral homogeneity of the outer core. Furthermore, we find that T-0(Phi) for the crust and mantle in this region exceeds the AK135 prediction by 3.5 s (IASP91 by 3.9 s) +/-1.0 s. Since the lower mantle contribution to this delay depends upon how much arises in the upper mantle, we present two end-member models for such a slower mantle V-Phi, in which the delay resides entirely above or below 660 km depth. The latter yields best-fitting lower mantle compositions which are less enriched in Si than those fit to T-o(Phi) for AK135 (or IASP91) for the former, and neither supports Fe-enrichment of the lower mantle. Applicability of such localized observations to the larger mantle is suggested. by tomographic results indicating that lateral heterogeneity in V-Phi is very small relative to that in V-S. Our results illustrate the potential utility of T-0(Phi) in constraining mantle composition.