
Figure F40.
Mantle peridotites from Conical, Torishima, and South Chamorro Seamounts plotted
in (A)CaO vs. Al2O3 and (B)
CaO vs. 100 x Mg2+/(Mg2+
+ Fe2+) diagrams after Ishiwatari (1985), showing different degrees
of melting. Fields for Conical and Torishima Seamount peridotites are from Ishii
et al. (1992), Parkinson and Pearce (1998), and I.P. Savov and W.B.F. Ryan (unpubl.
data).

