Figure F58. Cr vs. TiO2, showing the elevated Cr abundances of the samples from the lower part of the cored section at Hole 1184A (three samples with ~300 ppm Cr) compared to those from the upper part. Data for basalt units from Sites 803, 807 (Mahoney et al., 1993), 1183, 1185, 1186, and 1187, and data fields for the Kwaimbaita and Singgalo Formations on Malaita (Tejada et al., in press) are also shown.

Figure F58. Cr vs. TiO₂, showing the elevated Cr abundances of the samples from the lower part of the cored section at Hole 1184A (three samples with ~300 ppm Cr) compared to those from the upper part. Data for basalt units from Sites 803, 807 (Mahoney et al., 1993), 1183, 1185, 1186, and 1187, and data fields for the Kwaimbaita and Singgalo Formations on Malaita (Tejada et al., in press) are also shown.