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- W1986171639 abstract "Phase transformation of (Mg0.89Fe0.11)2SiO4 olivine, the proposed major composition of upper mantle, is related to the mechanism of deep focus earthquakes and the interaction between subduction zones and their ambient mantle. Nucleation rate and growth rate are two important parameters in the computation of the phase transformation. However, the nucleation rate has not been derived from the experimental data partly for technical difficulties. We modify the dimensionless parameter describing the impingement under grain boundary nucleation through physical analysis on the image of the impingement. Based on this modification and the experimental data, we first evaluate the nucleation of olivine. By fitting the new nucleation rates, we get the parameters K0 and γø1/3. The best fitting results are K0 = 6.9 × 1024s−1·m−2·K−1, γø 1/3=0.16 J·m−2." @default.
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- W1986171639 date "2007-01-01" @default.
- W1986171639 modified "2023-09-25" @default.
- W1986171639 title "Evaluation of the Nucleation Rate of Olivine" @default.
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- W1986171639 doi "https://doi.org/10.1002/cjg2.1018" @default.
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