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Detailed Reference Information |
Li, D., Secco, R.A., Bancroft, G.M. and Fleet, M.E. (1995). Pressure induced coordination change of Al in silicate melts from Al K edge XANES of high pressure NaAlSi2O6-NaAlSi3O8 glasses. Geophysical Research Letters 22: doi: 10.1029/95GL03175. issn: 0094-8276. |
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Aluminum K-edge XANES spectra of high pressure and high temperature (4.4 GPa and 1575 ¿C) glasses along the NaAlSi2O6(Jd)-NaAlSi3O8(Ab) join are reported using synchrotron radiation, and shown to provide direct experimental evidence for the pressure-induced coordination change of Al. Five- and six-fold coordinated Al ([5>Al and [6>Al), characterized by Al K-edge positions at 1567.8 and 1568.7 eV, respectively, first appear in glass of composition Jd60Ab40 and increase in proportion progressively with increasing Jd content. The end-member jadeite glass contains about 6% of each of [5>Al and [6>Al. The present direct measurements confirm literature suggestions for the important role of Al in controlling viscosity and diffusion in mantle melts. ¿ American Geophysical Union 1995 |
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Abstract |
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Keywords
Mineral Physics, X ray, neutron, and electron spectroscopy and diffraction, Mineral Physics, High-pressure behavior |
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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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