Hydrothermal experiments with variable pore pressure and shear stress in part of the MgO – SiO2 – H2O system.
In the systematic hydrothermal investigation or mineral systems in modern laboratories, the influence of several variables can be determined. In most recent studies the variables have been three: composition of the solid phase, temperature, pressure of water in contact with the solid phase. In gener...
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| Format: | Others |
| Language: | en |
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McGill University
1957
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111368 |