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GSA Special Papers
Advances in High-Pressure Mineralogy
Author(s)
Eiji Ohtani
Eiji Ohtani
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University, Sendai 980-8578, Japan
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Geological Society of America

Volume
421
Copyright:
Geological Society of America
ISBN print:
9780813724218
Publication date:
January 01, 2007
Book Chapter
Melting of ice VII and new high-pressure, high-temperature amorphous ice
Author(s)
Leonid Dubrovinsky
Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany
;
Leonid Dubrovinsky
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Natalia Dubrovinskaia
Mineralphysik und Strukturforschung, Mineralogisches Institut, Universität Heidelberg, 69120 Heidelberg, Germany and Lehrstuhl für Kristallographie, Physikalisches Institut, Universität Bayreuth,D- 95440 Bayreuth, Germany, and Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany
Natalia Dubrovinskaia
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Published:January 01, 2007
Properties of H2O at elevated pressure and temperature are of fundamental importance in both condensed matter physics and planetary sciences. We studied behavior of H2O in externally heated diamond anvil cells (DACs) at pressures up to 50 GPa and temperatures to 1150 K by combining visual observations, Raman spectroscopy, and X-ray powder diffraction. The melting curve of H2O was found to be well described by the Simon equation P(GPa) = 2.2 + 1.31{[T(K)/364]3.3 – 1}. Above 30 GPa and 950 K, using visual observations and Raman spectroscopy, we found an...
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