Exploratory studies of silicate melt structure at high pressures and temperatures by in situ X-ray diffraction
We have developed synchrotron X‐ray diffraction techniques for studying the structure of silicate melts and have applied them to measuring the structures of MgSiO3 and CaSiO3 melts up to 6 GPa. In both melts, it appears that the changes in the local structure around the divalent ions and in the netw...
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Veröffentlicht in: | Journal of Geophysical Research. B. Solid Earth 2004-03, Vol.109 (B3), p.B03203.1-n/a |
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