Geochemical variations of the Quaternary Daisen adakites, Southwest Japan, controlled by magma production rate
Abstract
The late Cenozoic Southwest Japan arc was formed by hot subduction of the young Shikoku Basin slab, and Daisen Volcano has erupted exclusively adakitic products since ca.1.0 Ma under this subduction regime. Although previous studies have revealed that the adakites of this arc were generated by melting of the subducted basaltic crust and incorporation of slab sediments, this model cannot simply explain the observed geochemical variations of the...
Paper Details
Title
Geochemical variations of the Quaternary Daisen adakites, Southwest Japan, controlled by magma production rate
Published Date
Dec 1, 2019
Journal
Volume
350-351
Pages
105214 - 105214
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