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Melting under the conditions of the upper mantle
Modern petrological models describe the melting process as thermodynamically balanced. It has been shown in the work that initial melting is possible at the depth not less than 220 km. Phase diagrams plotted according to the results of experimental studies on melting of mantle lerzolite, demonstrate...
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| Main Author: | |
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| Format: | Article |
| Language: | rus |
| Published: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2011
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/116899 |
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