Figure F103. A–C. Compositions of different rock types recovered from Hole U1415J vs. TiO2. For comparison, a compilation of plutonic rocks sampled along the East Pacific Rise (EPR) at Hess Deep (Hékinian et al., 1993; Shipboard Scientific Party, 1993; Miller et al., 1996; Natland and Dick, 2009; Pedersen et al., 1996; Hanna, 2004; Kirchner and Gillis, 2012), Pito Deep (Perk et al., 2007), and other locations (Saunders et al., 1982) is shown. Plutonic rock sampled in Holes U1415E, U1415H, and U1415I are also shown for comparison. Cpx = clinopyroxene.
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