Аннотация
This report presents the primary results of experiments at 5.5 GPa and 1600°C on the migration of molten iron through a solid silicate matrix consisting of olivine crystals with graphite-filled interstices. It was shown that the migration rate was quite high at the given P and T values (up to 2.5 mm/h). It was shown that carbon in its elemental forms might affect the migration capability of molten iron. This effect must be included in creating a correct model of the formation of the inner parts of the Earth, the terrestrial planets, and planetoids.
Язык оригинала | английский |
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Страницы (с-по) | 677-679 |
Число страниц | 3 |
Журнал | Doklady Earth Sciences |
Том | 463 |
Номер выпуска | 1 |
DOI | |
Состояние | Опубликовано - 4 июл 2015 |
Опубликовано для внешнего пользования | Да |