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Diversity And Petrogenesis Of Rhyolites From An Intra-Oceanic Arc: Evidence From Iodp Site U1437, Izu Bonin Rear-Arc And Surrounding Area, Luan J. (Luan Jean) Heywood

WWU Graduate School Collection

Magmas from the Izu Bonin rear-arc show a geochemical signature (medium- to high-K and light rare-earth element [LREE] enriched) that resembles the average composition of the continental crust. I investigate that continent-like signature by examining a suite of rear-arc-derived mafic to felsic tephras from International Ocean Discovery Program (IODP) Site U1437, which was drilled as part of IODP Expedition 350. Volcaniclastic glasses from Site U1437 comprise a compositional series from basalt to rhyolite, aged 1.1-4.4 Ma.

Site U1437 tephras record the timespan when the Izu-Bonin arc began rifting and provide a well-dated record of changing magmatic compositions through the transition …