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- W2158445900 abstract "Abundant rhyolitehaseruptedfromthe Izu^Bonin^Marianavolca-nic arc (IBM arc) from its earliest stage (Eocene) to the present.Geochemically, three types of Quaternary rhyolites exist in the Izu^Bonin arcfront, and theyare closely related tovolcanotypeand crus-tal structure.The dominantly basaltic islands of the volcanic frontproduce small volumes of rhyolites that we call R1.The submarinecalderas of the volcanic front erupt mostly rhyolite that we call R2.Seamounts, knolls, and pillow ridges in thebackarcextensionalzoneare mostly basaltic but also contain rhyolites that we call R3.Thethickest total crust, and the thickest intermediate compositionmiddle crust, occurs below the dominantly basaltic volcanoes,whereas the intermediate composition middle crust tends to be thin-nerbeneaththesubmarinecalderas. R1rhyolitesmaybederivedfromQuaternary andesitic sources whereas R2 and R3 rhyolites may bederivedfromOligoceneones.ThehigherCaO/Al" @default.
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- W2158445900 date "2009-04-01" @default.
- W2158445900 modified "2023-09-27" @default.
- W2158445900 title "Silicic Magmas in the Izu–Bonin Oceanic Arc and Implications for Crustal Evolution" @default.
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- W2158445900 doi "https://doi.org/10.1093/petrology/egp017" @default.
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