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Underground hydrosphere and geofluids of the Earth’s crust and upper mantle

The physicochemical state of the water at various temperature and pressure conditions of the Earth’s interior has been characterized. Two groups of geofluidic systems for water have been established: subcritical (T &lt; 374 ¸ 450 °Ñ) and supercritical (T &gt; 374 ¸ 450 °C), which together wi...

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Bibliographic Details
Main Author: Kudelsky, A.V.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2017
Subjects:
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/112337
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