The Nature of the 660-Kilometer Upper-Mantle Seismic
Discontinuity from Precursors to the PP Phase
Charles H. Estabrook
*
and
Rainer Kind
Global Seismic Network data were used to image upper-mantle seismic
discontinuities. Stacks of phases that precede the PP phase,
thought to be underside reflections from the upper-mantle discontinuities at depths of 410 and 660 kilometers, show that the
reflection from 410 kilometers is present, but the reflection from 660 kilometers is not observed. A continuous Lamé's constant
and
seismic parameter at the 660-kilometer discontinuity explain the
missing underside P reflections and lead to a
P-wave velocity jump of only 2 percent, whereas the
S-wave velocity and density remain unchanged with respect to
previous global models. The model deemphasizes the role of
Lamé's constant
with regard to the shear modulus and
constrains the mineralogical composition across the discontinuity.
GeoForschungsZentrum Potsdam, Telegrafenberg, D- 14473 Potsdam,
Germany.
*
To whom correspondence should be addressed.
Also at Freie Universität Berlin, Berlin, Germany.