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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Published in | Journal of Asian earth sciences Vol. 194; p. 104185 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.06.2020
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Subjects | |
Online Access | Get full text |
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