Chemical geodynamics of mafic magmatism above subduction zones

•Mafic magmatism above oceanic and continental subduction zones proceeds in two-stage processes.•Crustal signatures are transferred by liquid phases into the mantle source of mafic igneous rocks.•The fractionation of melt-mobile trace elements is significant at the slab-mantle interface.•Metasomatis...

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Bibliographic Details
Published inJournal of Asian earth sciences Vol. 194; p. 104185
Main Authors Zheng, Yong-Fei, Xu, Zheng, Chen, Long, Dai, Li-Qun, Zhao, Zi-Fu
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.06.2020
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