Insights Into the Nature of Plume‐Ridge Interaction and Outflux of H 2 O From the Galápagos Spreading Center
Author:
Affiliation:
1. Deparment of Earth Sciences University of Cambridge Cambridge UK
2. School of Earth and Environmental Sciences Cardiff University Cardiff UK
Funder
Natural Environment Research Council
Royal Commission for the Exhibition of 1851
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009560
Reference123 articles.
1. The importance of water to oceanic mantle melting regimes
2. Effect of the Galápagos hotspot on seafloor volcanism along the Galápagos Spreading Center (90.9–97.6°W)
3. Geochemical variations at ridge-centered hotspots caused by variable melting of a veined mantle plume
4. Constructing the crust along the Galapagos Spreading Center 91.3°-95.5°W: Correlation of seismic layer 2A with axial magma lens and topographic characteristics
5. Melt migration in plume–ridge systems
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1. Determining the pressure-temperature-composition (P-T-X) conditions of magma storage;Reference Module in Earth Systems and Environmental Sciences;2024
2. Episodic intraplate magmatism fed by a long-lived melt channel of distal plume origin;Science Advances;2023-06-09
3. The Geochemical Evolution of Santa Cruz Island, Galápagos Archipelago;Frontiers in Earth Science;2022-09-13
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