Bina, C. R., Mutually consistent estimates of upper mantle composition
from seismic velocity contrasts at 400 km depth,
*Pure and Applied Geophysics, 141*, 101-109,
doi:10.1007/BF00876237, 1993.

**Abstract.**
Seismologically determined properties of the 400 km discontinuity may
be compared to experimentally determined properties of the associated
phase transformation in order to place constraints upon upper mantle
bulk composition.
Disagreement among previous studies is commonly ascribed to differences
in elastic equations of state (especially to assumptions about pressure and
temperature derivatives) between studies.
However, much of the disparity between studies is actually due to
the selection of different seismic data functionals (P-wave velocity,
S-wave velocity, etc.) for comparison to mineral elasticity calculations,
rather than to the differences in elasticity datasets and equations of
state.
Within any given study, bulk sound velocity comparisons generally
yield more olivine-rich compositional estimates than do P-wave velocity
comparisons, which in turn indicate more olivine than S-wave velocities.
Indeed, such variation in compositional estimates within a given study
(arising from choice of data functional) exceeds the variation between
studies (arising from elastic equation of state approximations).
It can be argued that bulk sound velocities are better constrained
seismologically than densities and, being independent of assumptions
about shear moduli, should provide more reliable compositional estimates
than P- or S-wave velocities.

Using recently measured bulk and shear moduli equations of state, mutually consistent estimates of upper mantle olivine content can be obtained from P-wave, S-wave, and bulk sound velocity contrasts at 400 km only if d ln mu / d T of beta has a value of about -2.e-04 / K, yielding approximately 52% olivine by volume. A value of d ln mu / d T smaller in magnitude would require reassessment of several underlying assumptions.

Copyright © 1993 Birkhaüser Verlag, BaselReturn to Craig's publications page.

Copyright © 1995 Craig R. Bina.