(Table 5) Oxygen isotope data for clay minerals extracted from vesicles of the upper volcanic series of ODP Hole 104-642E
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Temperature calculated by assuming formation in equilibrium with water at 0 per mil and using the fractionation factor of glauconite (Savin and Epstein, 1970, doi:10.1016/0016-7037(70)90149-3) for celadonite, and of Mg-smectites (Escande, 1983) for saponite. The chemical analyses of samples are given in Tables 1 (doi:10.1594/PANGAEA.737383) and 2 (doi:10.1594/PANGAEA.737384).
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2025-11-10
