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Oxygen and hydrogen isotope fractionation in serpentine–water and talc–water systems from 250 to 450 °C, 50 MPa

✍ Scribed by Peter J. Saccocia; Jeffrey S. Seewald; Wayne C. Shanks III

No coin nor oath required. For personal study only.

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Oxygen and hydrogen isotope fractionation in serpentine–water and talc–water systems from 250 to 450&#xa0;°C, 50&#xa0;MPa