An experimental study of the kinetics of decompression-induced crystallization in silicic melt
Experiments were conducted to study the temporal evolution of feldspar crystallization kinetics during isothermal decompression. Pinatubo dacite was held at 780°C, 220 MPa, fO2 = NNO + 2, H2O‐saturated conditions for an equilibration period, decompressed to final pressures, Pf, ranging from 175 to 5...
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Veröffentlicht in: | Journal of Geophysical Research: Solid Earth 2002-01, Vol.107 (B1), p.ECV 8-1-ECV 8-24 |
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Sprache: | eng |
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