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Dagma Derdau Robert Freer Kate Wright 《Contributions to Mineralogy and Petrology》1998,133(1-2):199-204
Oxygen exchange experiments have been performed between single crystals of sanidine feldspar and oxygen gas enriched in 18O, at temperatures in the range 869–1053 °C, total pressure 1 atmosphere, for times up to 28 days. Oxygen isotope diffusion
profiles in a direction perpendicular to (001) were determined with an ion microprobe. The experimental data obey a single
Arrhenius relationship of the form D = 8.4 × 10−11 exp. (−245 ± 15 kJ mol−1/RT) m2s−1. The results indicate that oxygen diffusion in anhydrous sanidine feldspar is marginally slower than oxygen diffusion in
anhydrous anorthite. Comparison with published atomistic simulation studies suggests that oxygen transport in feldspar is
by an interstitial mechanism.
Received: 17 October 1997 / Accepted: 6 July 1998 相似文献
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