Noble gases recycled into the mantle through cold subduction zones
Subduction of hydrous and carbonated oceanic lithosphere replenishes the mantle volatile inventory. Substantial uncertainties exist on the magnitudes of the recycled volatile fluxes and it is unclear whether Earth surface reservoirs are undergoing net-loss or net-gain of H2O and CO2. Here, we use no...
| Main Authors: | , , , , , , |
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| Format: | Journal article |
| Published: |
Elsevier
2017
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