about
Slab melting versus slab dehydration in subduction-zone magmatism.Separation of supercritical slab-fluids to form aqueous fluid and melt components in subduction zone magmatism.Olivine water contents in the continental lithosphere and the longevity of cratons.X-ray imaging for studying behavior of liquids at high pressures and high temperatures using Paris-Edinburgh press.
P2860
description
im März 2007 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в березні 2007
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name
Second critical endpoint in the peridotite-H2O system
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Second critical endpoint in the peridotite-H2O system
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type
label
Second critical endpoint in the peridotite-H2O system
@en
Second critical endpoint in the peridotite-H2O system
@nl
prefLabel
Second critical endpoint in the peridotite-H2O system
@en
Second critical endpoint in the peridotite-H2O system
@nl
P50
P356
P1476
Second critical endpoint in the peridotite-H2O system
@en
P2093
Kenji Mibe
Kyoko N. Matsukage
P2860
P356
10.1029/2005JB004125
P407
P577
2007-03-01T00:00:00Z