Hydrogen generation from mantle source rocks in Oman

Details Hydrogen generation from mantle source rocks in Oman Hydrogen generation from mantle source rocks in Oman

Dec 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983e%26psl..66..315n&link_type=abstract

Earth and Planetary Science Letters (ISSN 0012-821X), vol. 66, Dec. 1983, p. 315-320.

Mathematics

Logic

25

Earth Mantle, Geochemistry, Hydrogen, Oman, Outgassing, Chemical Composition, Earth Atmosphere, Hydrogeology

Scientific paper

Isotopic and chemical evidence is adduced for the H gas associated with Ca(2+)OH-rich alkaline groundwaters presently emanating from ultramafic rocks of the Oman ophiolite which indicates that H is formed by low - temperature redox reactions in a closed groundwater environment. This normally cryptic hydrospheric process is fortuitously revealed by the unusual hydrogeological conditions in Oman, where O is totally assimilated. It is suggested that H generation in mantlle source rocks at depth and in the early Archaean surface environment may be more widespread than has been previously supposed.

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