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Science 22 December 1995: Vol. 270. no. 5244, pp. 1964 - 1967 DOI: 10.1126/science.270.5244.1964
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Reports
Al Coordination Changes in High-Pressure Aluminosilicate
Liquids
J. L. Yarger (1),
K. H. Smith,
R. A. Nieman,
J. Diefenbacher,
G. H. Wolf,
B. T. Poe,
P. F. McMillan (1)
Understanding the effect of pressure on aluminosilicate glass and
liquid structure is critical to understanding magma flow at depth.
Aluminum coordination has been predicted by mineral phase analysis and
molecular dynamic calculations to change with increasing pressure.
Nuclear magnetic resonance studies of glasses quenched from high
pressure provide clear evidence for an increase in the average
coordination of Al with pressure.
J. L. Yarger, K. H. Smith, R. A. Nieman, Department of Chemistry
and Biochemistry, Arizona State University, Tempe, AZ 85287, USA.
J. Diefenbacher, G. H. Wolf, P. F. McMillan, Material Research Group in
High-Pressure Synthesis, Arizona State University, Tempe AZ 85287, USA.
B. T. Poe, Bayerisches Geoinstitut, Universitat Bayreuth, Bayreuth,
Germany D-95440.
(1) To whom correspondence should be addressed.
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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PNAS
105, 7925-7929
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- J. R. Allwardt, B. T. Poe, and J. F. Stebbins (2005)
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- Self diffusion of Si and O in dacitic liquid at high pressures.
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American Mineralogist
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- Aluminium coordination in tektites: A XANES study.
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American Mineralogist
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- Silicon and Oxygen Self-Diffusivities in Silicate Liquids Measured to 15 Gigapascals and 2800 Kelvin.
- B. T. Poe, P. F. McMillan, D. C. Rubie, S. Chakraborty, J. Yarger, and J. Diefenbacher (1997)
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276, 1245-1248
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