Figure 12 | Table of Contents

Figure 11. TiO₂ vs. Mg# for basement rocks recovered at all Leg 192 sites and ODP Sites 803 and 807. The fields for basaltic lava flows of the >2.7-km-thick Kwaimbaita Formation and the overlying ~750-m-thick Singgalo Formation on Malaita (Tejada et al., 1996, 2000) are shown for comparison. Data for Sites 803 and 807 are from Mahoney et al. (1993).