(Table 3) Stable isotopic analyses of vein carbonates of ODP Hole 136-843B
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Sediment depth is given in mbsf. Equilibration temperatures calculated assuming formation in equilibrium with water having d18O of normal seawater (O per mil) and d18O-depleted pore fluids (-2 per mil) using fractionation factors of O'Neil et al. (1969).
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2025-11-04
