Polycrystalline specimens of two pyrope-majorite garnets(2) (Py(62)Mj(38) a
nd Py(62)Mj(38)) were synthesized in a 2000-ton uniaxial split-sphere appar
atus (USSA-2000) at pressures of 16 GPa and temperatures of 1670 K for run
durations of about 2 h using homogeneous glasses as starting materials. Ult
rasonic interferometric measurements on these specimens were conducted at p
ressures up to 9 GPa at room temperature using a 1000-ton uniaxial split-cy
linder apparatus (USCA-1000) with Bi as an internal pressure marker. From t
he measurements of the travel times for compressional (P) and shear (S) wav
es, the velocities and elastic moduli are calculated using length/density c
hanges determined from the travel-time data. Third-order Eulerian finite st
rain analysis of these data yield the longitudinal (L) and shear (G) moduli
and their pressure derivatives [M-0' = (partial derivative M/partial deriv
ative P)(T)]: for Py(62)Mj(38), L-0 = 291 +/- 0.6 GPa and L-0' = 9.1 +/- 0.
6, G(0) = 90 +/- 1 GPa and Gb = 1.9 +/- 0.2, from which we calculate the va
lues for the adiabatic bulk modulus (K = L - 4/3 G) to be K-0 = 171 +/- 5 G
Pa and K-0' = 6.2 +/- 0.5. These new data for the shear modulus and its pre
ssure derivative are in agreement with the previous values for the same com
position (Rigden, S.M., Gwanmesia, G.D., Liebermann, R.C., 1994. Elastic wa
ve velocities of a pyrope-majorite garnet to 3 GPa. Phys. Earth Planet. Int
er. 86, 35-44.), but the P wave velocity, the bulk modulus and its pressure
derivative are somewhat higher. For the Py(50)Mj(50) composition, these va
lues are L-0 = 289 +/- 6 GPa, L-0' = 9.2 +/- 0.7, G(0) = 89 +/- 1 GPa, G(0)
' = 2.1 +/- 0.2, K-0 = 170 +/- 5 GPa, and K-0' = 6.4 + 0.5. The high-pressu
re derivatives of K and G for these Py-Mj garnets may be important in expla
ining the high velocity gradients observed in seismic models of the transit
ion zone of the Earth's mantle. (C) 2000 Elsevier Science B.V. All rights r
eserved.