Figure F56. Zr vs. TiO2, showing that five Site 1184 samples have compositions similar to the basalt of Units C-G at Site 807 (Mahoney et al., 1993), to the basalt flows of the Kwaimbaita Formation on Malaita (Tejada et al., in press), and to basalt units at Sites 1183, 1185 (lower group), and 1186. One sample is similar in composition to the basalt of Site 803, Unit A at Site 807, and the Singgalo Formation on Malaita.