Whole rock geochemistry of Forearc Basalts from IODP Expedition 352
2019-11-19T14:07:52Z (GMT) by
These basalts represent the earliest response to subduction initiation in the Izu-Bonin arc system during the early Eocene. They are highly refractory and formed by high degrees of partial melting of a previously depleted source. Major elements normalized to 100% anhydrous.