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• W2032290499 abstract "Hydrogen gas, associated with Ca2+ OH-rich alkaline groundwaters (pH = 10–12), is at present emanating from ultramafic rocks of the Oman ophiolite. Isotopic and chemical evidence indicates that hydrogen is formed by low-temperature redox reactions in a closed groundwater environment. This is normally a cryptic process in the hydrosphere but is fortuitously revealed by the unusual hydrogeological conditions in Oman where atmospheric oxygen is totally assimilated. It is suggested that hydrogen generation in mantle source rocks at depth and in the early Archaean surface environment may be more widespread than has hitherto been realised." @default.
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• W2032290499 date "1983-12-01" @default.
• W2032290499 modified "2023-10-16" @default.
• W2032290499 title "Hydrogen generation from mantle source rocks in Oman" @default.
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• W2032290499 doi "https://doi.org/10.1016/0012-821x(83)90144-9" @default.
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