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...
| Κύριοι συγγραφείς: | , , , , |
|---|---|
| Μορφή: | Journal article |
| Γλώσσα: | English |
| Έκδοση: |
Springer Nature
2016
|