Source: http://journals.uran.ua/geofizicheskiy/article/view/111022
Timestamp: 2019-04-22 05:01:48+00:00

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The investigation of the PT-parameters of magma in the mantle of this and other oceans is conducted. They are about 25 km and 1150 °С, 55—60 km and 1200 °С, 95 km and 1300 °С, 145 km and 1500 °С, 210 km and 1700 °С. The results are consistent with the advection-polymorphic hypothesis of deep processes.
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