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...
| Main Authors: | , , |
|---|---|
| 格式: | Journal article |
| 出版: |
Elsevier
2017
|