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Figure F25. Plots of Fe₂O₃^T vs. Cr, Sc, V, and Y for basaltic rock samples, Hole U1382A. Data for aphyric and porphyritic basalts from corresponding depths in Hole 395A (Rhodes et al., 1979; Bougault et al., 1979) are also shown for comparison. Fe₂O₃^T = total iron as Fe₂O₃.

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