GEODYNAMIC PROCESSES DURING ASCENT OF A PLUME WITH INTERMEDIATE THERMAL POWER THROUGH THE CONTINENTAL LITHOSPHERE AND DURING ITS ERUPTION ON THE SURFACE
The study is focused on thermochemical mantle plumes with intermediate thermal power (1.15 < Ka < 1.9). Previously we have shown that these plumes are diamondiferous. Based on the laboratory modeling data, the flow structure of a melt in a plume conduit is represented. A plume melts out and as...
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| Autors principals: | , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2020-06-01
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| Col·lecció: | Геодинамика и тектонофизика |
| Matèries: | |
| Accés en línia: | https://www.gt-crust.ru/jour/article/view/1040 |
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