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Detailed Reference Information |
Kirkpatrick, R.J., Robinson, G.R. and Hays, J.F. (1976). Kinetics of crystal growth from silicate melts: Anorthite and diopside. Journal of Geophysical Research 81: doi: 10.1029/JB081i032p05715. issn: 0148-0227. |
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Rates of linear crystal growth have been measured for diopside and anorthite growing from their own melts by using a microscope heating stage. Rates were obtained for undercoolings of as little as 13 ¿C. The rates are higher for diopside than for anorthite. Maximum growth rates observed ar 1.5¿10-2 cm/s(ΔT=194 ¿C) for anorthite and 2.2¿10-2 cm/s(ΔT=105 ¿C) for diopside. For diopside this probably does not represent the maximum rate. Both phases grow with a faceted morphology. Plots of Y&eegr;/ΔT versus ΔT indicate that anorphite grows by a surface nucleation mechanism, while diopside grows by a screw dislocation mechanism. These plots can also be used to calculate growth rates at undercoolings less than those at which data have been obtained. |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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