Nature and distribution of slab‐derived fluids and mantle sources beneath the Southeast Mariana forearc rift
Subduction zone magmas are produced by melting depleted mantle metasomatized by fluids released from the subducted slab. In most subduction zones, formation of backarc basin (BAB) and arc magmas depletes the mantle source toward the trench, resulting in more depleted mantle beneath the forearc. Slab...
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| Principais autores: | , , , , , , |
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| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Wiley
2013-10-01
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| Serier: | Geochemistry, Geophysics, Geosystems |
| Fag: | |
| Online adgang: | https://doi.org/10.1002/ggge.20244 |
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