Control of subduction rate on Tonga-Kermadec arc magmatism
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DOI: 10.1007/s00343-018-7026-8
Abstract: Dehydration/melting of oceanic crusts during returning to the mantle in subduction zones are related to origin of arc lavas. The factors that influence arc magmatism include compositions of the subducting slabs, mantle wedge and subduction… read more here.
Keywords: arc magmatism; subduction; rate; kermadec arc ... See more keywords