Water follows carbon: CO2 incites deep silicate melting and dehydration beneath mid-ocean ridges
Author:
Publisher
Geological Society of America
Subject
Geology
Reference23 articles.
1. The importance of water to oceanic mantle melting regimes
2. Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts
3. The effects of deep damp melting on mantle flow and melt generation beneath mid-ocean ridges
4. Mantle upwelling and melting beneath slow spreading centers: effects of variable rheology and melt productivity
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