High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions
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.
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| Veröffentlicht in: | Contributions to mineralogy and petrology 2001-02, Vol.140 (5), p.607-618 |
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| container_issue | 5 |
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| container_title | Contributions to mineralogy and petrology |
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| creator | Stalder, R. Ulmer, P. Thompson, A. Günther, D. |
| description | 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. |
| doi_str_mv | 10.1007/s004100000212 |
| format | Article |
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| ispartof | Contributions to mineralogy and petrology, 2001-02, Vol.140 (5), p.607-618 |
| issn | 0010-7999 1432-0967 |
| language | eng |
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| source | SpringerLink Journals |
| subjects | Geology High pressure Mineralogy Petrology Pressure Temperature Upper mantle |
| title | High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions |
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