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On geological hydrogen

On geological hydrogen

Formation of geological (abiogenous) hydrogen in the interior is connected with two groups of hypotheses: production of secondary hydrogen in the Earth’s crust and upper mantle as a result of its emission from water and some minerals as well as discharge of primary hydrogen from the core and lower m...

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Bibliographic Details
Main Author: Shestopalov, V.M.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2020
Subjects:
geological secondary and primary hydrogen
heat flow
geo-reactor
tritium degassing
deep faults
native metals
hydrogen deposits
геологический вторичный и первичный водород
тепловой поток
геореактор
дегазация трития
глубинные разломы
самородные металлы
месторождения водорода
геологічний вторинний і первинний водень
тепловий потік
дегазація тритію
глибинні розломи
самородні метали
родовища водню
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/222278
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https://journals.uran.ua/geofizicheskiy/article/view/222278

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