Geochemistry of abyssal peridotites from ODP Hole 209-1274A
Aqueous dihydrogen (H2,aq) is produced in copious amounts when seawater interacts with peridotite and H2O oxidizes ferrous iron in olivine to ferric iron in secondary magnetite and serpentine. Poorly understood in this process is the partitioning of iron and its oxidation state in serpentine, althou...
Main Authors: | , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2009
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.783396 https://doi.org/10.1594/PANGAEA.783396 |