Halogen variations through the quenched margin of a MORB lava: Evidence for direct assimilation of seawater during eruption
Halogens and noble gases within submarine basaltic glasses are critical tracers of interactions between the surface volatile reservoirs and the mantle. However, as the halogens and noble gases are concentrated within seawater, sediments, and the oceanic crust this makes the original volatile signatu...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Published: |
Wiley
2017
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