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- W1984874108 abstract "The velocity of the compressional wave (VP) was measured for olivine aggregate at temperatures up to 1000°C at 1 GPa using a piston-cylinder high-pressure apparatus. The samples used in the present study were hot-pressed olivine aggregate with uniform chemical composition. The value of VP at 1 GPa and an ambient temperature, is 8.42 km s−1, which is identical to that in previous measurements of olivine single-crystals. The temperature derivative of VP (∂VP/∂T=−4.7×10−4kms−1K−1) obtained from the present experiments at 1 GPa is smaller than the previously reported value at an ambient pressure. The temperature gradient for constant velocity (dT/dZ)c allowing the effect of anelasticity is calculated to be 4°C km−1. Taking into account, the temperature gradient in the upper mantle (15°C km−1 within the lithosphere and 0.6°C km−1 within the asthenosphere), it is suggested that the low velocity zone in the upper mantle could be caused by a drastic change in the temperature gradient at the lithosphere/asthenosphere boundary." @default.
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- W1984874108 date "2001-09-01" @default.
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- W1984874108 title "Experimental determination of compressional wave velocities of olivine aggregate up to 1000°C at 1GPa" @default.
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- W1984874108 doi "https://doi.org/10.1016/s0040-1951(01)00133-0" @default.
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