Enhanced East Pacific Rise hydrothermal activity during the last two glacial terminations
Mid-ocean ridge magmatism is driven by seafloor spreading and decompression melting of the upper mantle. Melt production is apparently modulated by glacial-interglacial changes in sea level, raising the possibility that magmatic flux acts as a negative feedback on ice-sheet size. The timing of melt...
Published in: | Science |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Association for the Advancement of Science
2016
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Subjects: | |
Online Access: | https://doi.org/10.1126/science.aad4296 |