Parental arc magma compositions dominantly controlled by mantle-wedge thermal structure
The processes that lead to the fourfold variation in arc-averaged compositions of mafic arc lavas remain controversial. Control by the mantle-wedge thermal structure is supported by chemical correlations with the thickness of the underlying arc crust, which affects the thermal state of the wedge. Co...
Main Authors: | , , , , |
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Format: | Journal article |
Language: | English |
Published: |
Springer Nature
2016
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