Elemental changes and alteration recorded by basaltic drill core samples recovered from in situ temperatures up to 345°C in the active, seawater-recharged Reykjanes geothermal system, Iceland
Hydrothermal activity results in element exchanges between seawater and oceanic crust that contribute to many aspects of ocean chemistry; therefore, improving knowledge of the associated chemical processes is of global significance. Hydrothermally altered basaltic drill core samples from the seawate...
| Main Authors: | , |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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eScholarship, University of California
2016
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| Online Access: | https://escholarship.org/uc/item/65b3p62g |