Article ID Journal Published Year Pages File Type
4739577 Russian Geology and Geophysics 2008 13 Pages PDF
Abstract

Experimental data on the diffusion coefficients of Fe, Mn, Mg, and Ca in garnets are generalized. Frequency factors (cm2/s), activation energies (cal/mole), and activation volumes (cm3/mole) are optimized. Based on the compensation law, the dependences of diffusion coefficients on pressure (kbar) and temperature (K) have been derived:D˜Fe=1.0·10−3exp[−(61450+23.9·8·P)/(RT)],D˜Mn=2.3·10−6exp[−(44600+23.9·6·P)/(RT)],D˜Mg=4.9·10−3exp[−(65900+23.9·9.2·P)/(RT)],D˜Ca=4.1·10−5exp[−(62450+23.9·11.2·P)/(RT)].

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Physical Sciences and Engineering Earth and Planetary Sciences Geology
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