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000418077 1001_ $$0P:(DE-HGF)0$$aVasiukov, D. M.$$b0$$eCorresponding author
000418077 245__ $$aSound velocities of skiagite–iron–majorite solid solution to 56 GPa probed by nuclear inelastic scattering
000418077 260__ $$aHeidelberg$$bSpringer$$c2018
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000418077 520__ $$aHigh-pressure experimental data on sound velocities of garnets are used for interpretation of seismological data related to the Earth’s upper mantle and the mantle transition zone. We have carried out a Nuclear Inelastic Scattering study of iron-silicate garnet with skiagite (77 mol%)–iron–majorite composition in a diamond anvil cell up to 56 GPa at room temperature. The determined sound velocities are considerably lower than sound velocities of a number of silicate garnet end-members, such as grossular, pyrope, Mg–majorite, andradite, and almandine. The obtained sound velocities have the following pressure dependencies: $V_p$ [km/s] = 7.43(9) + 0.039(4) × P [GPa] and $V_s$ [km/s] = 3.56(12) + 0.012(6) × P [GPa]. We estimated sound velocities of pure skiagite and khoharite, and conclude that the presence of the iron–majorite component in skiagite strongly decreases $V_s$ . We analysed the influence of Fe$^{3+}$ on sound velocities of garnet solid solution relevant to the mantle transition zone and consider that it may reduce sound velocities up to 1% relative to compositions with only Fe$^{2+}$ in the cubic site.
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000418077 7001_ $$0P:(DE-H253)PIP1023995$$aIsmailova, L.$$b1
000418077 7001_ $$0P:(DE-H253)PIP1014563$$aKupenko, I.$$b2
000418077 7001_ $$0P:(DE-H253)PIP1019116$$aCerantola, V.$$b3
000418077 7001_ $$aSinmyo, R.$$b4
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000418077 7001_ $$0P:(DE-H253)PIP1081721$$aMcCammon, C.$$b6
000418077 7001_ $$aChumakov, A. I.$$b7
000418077 7001_ $$aDubrovinsky, L.$$b8
000418077 7001_ $$aDubrovinskaia, N.$$b9
000418077 773__ $$0PERI:(DE-600)1463021-7$$a10.1007/s00269-017-0928-8$$gVol. 45, no. 5, p. 397 - 404$$n5$$p397 - 404$$tPhysics and chemistry of minerals$$v45$$x1432-2021$$y2018
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