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- W2078753512 abstract "The low-temperature alteration of siliceous volcanic glass by meteoric water involves considerable hydrogen exchange for Na+ or K+ ions. This can occur with little alteration of the other major- or trace-element composition of the glass. As much as 40% of the alkali sites can be occupied by H+ ion. Most water in these glasses is present as molecular water rather than as hydroxyl groups. This hydration is accompanied by oxygen isotope exchange resulting in an oxygen isotopic enrichment to over 20‰ (relative to SMOW) for this suite of samples. The high degree of alkali mobility during this alteration process affects the KAr age dating method. In these glasses, Ar appears to be less mobile than alkali ions, resulting in discrepant KAr ages for glass with significant hydration and oxygen isotopic exchange." @default.
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- W2078753512 date "1985-08-01" @default.
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- W2078753512 title "Low-temperature alteration of volcanic glass: Hydration, Na, K, 18O and Ar mobility" @default.
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- W2078753512 doi "https://doi.org/10.1016/0168-9622(85)90040-5" @default.
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