Figure F44. Abundance of Ba, Sr, and Ti vs. Zr comparing data for lavas from Koko, Nintoku, and Suiko Seamounts. The five Nintoku samples offset to high Zr from the Ti vs. Zr trend are hawaiites (see "Physical Volcanology and Igneous Petrology" in the "Site 1205" chapter).

Figure F44. Abundance of Ba, Sr, and Ti vs. Zr comparing data for lavas from Koko, Nintoku, and Suiko Seamounts. The five Nintoku samples offset to high Zr from the Ti vs. Zr trend are hawaiites (see "Physical Volcanology and Igneous Petrology" in the "Site 1205" chapter).