Arc magma compositions controlled by linked thermal and chemical gradients above the subducting slab
Global arc magmatism is sustained by a continuous fluid flux that is returned to the mantle in subduction zones. Despite considerable advances in simulations of melting processes, models of arc magmatism remain incompletely tested against erupted products. Here, we show that a suite of primitive vol...
| Glavni autori: | , , , |
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| Format: | Journal article |
| Jezik: | English |
| Izdano: |
John Wiley and Sons, Inc.
2013
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| Teme: |