Oceanic slab-top melting during subduction: implications for trace-element recycling and adakite petrogenesis
Arc volcanism and trace-element recycling are controlled by the devolatilization of oceanic crust during subduction. The type of fluid—either aqueous fluids or hydrous melts—released during subduction is controlled by the thermal structure of the subduction zone. Recent thermomechanical models and r...
| Main Authors: | , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Geological Society of America
2019
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