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High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions
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Journal Article
High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions
2001
Overview
Fluids and melts have been trapped and analysed in high pressure experiments in the model mantle system MgO-SiO2-H2O at 6 to 10.5 GPa and 900 to 1,200 degreesC. The fluid/melt traps consisted of a diamond layer that was added to the experimental charge and was separate from the silicate phases.
Publisher
Springer Nature B.V
Subject
