Volatiles beneath mid-ocean ridges: Deep melting, channelised transport, focusing, and metasomatism
Deep-Earth volatile cycles couple the mantle with near-surface reservoirs. Volatiles are emitted by volcanism and, in particular, from mid-ocean ridges, which are the most prolific source of basaltic volcanism. Estimates of volatile extraction from the asthenosphere beneath ridges typically rely on...
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| Materialtyp: | Journal article |
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Elsevier
2017
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