About ÐÒ conditions of magma chambers in the Earth's mantle
© Gordienko V.V., 2014
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 °Ñ, 55-60 km and 1200 °Ñ, 95 km and 1300 °Ñ, 145 km and 1500 °Ñ, 210 km and 1700 °Ñ. The results are consistent with
the advection-polymorphic hypothesis of deep processes.
Key words: mantle of the oceans and continents, deep processes, magma sources, PT-parameters
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