Thermodynamic constraints on hydrogen generation during serpentinization of ultramafic rocks
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference92 articles.
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4. Allen D. E., Berndt M. E. and Seyfried Jr. W. E. (1995) Iron component of brucite as an indicator of fH2 during serpentinization of olivine at 300°C and 500 bars. EOS Trans. AGU, 76, Fall Meeting Suppl., V32B-2 (abstr.).
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