The contribution of hydrothermally altered ocean crust to the mantle halogen and noble gas cycles
Recent studies suggest that seawater-derived noble gases and halogens are recycled into the deep mantle by the subduction of oceanic crust. To understand the processes controlling the availability of halogens and noble gases for subduction, we determined the noble gas elemental and isotopic ratios a...
| Main Authors: | , , , , , , |
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| Formato: | Journal article |
| Publicado em: |
Elsevier
2016
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