Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4739577 | Russian Geology and Geophysics | 2008 | 13 Pages |
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)].
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
V.N. Korolyuk, G.G. Lepezin,