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...

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Bibliographic Details
Main Authors: Klein, Frieder, Bach, Wolfgang, Jöns, Niels, McCollom, Thomas M, Moskowitz, Bruce, Berquo, Thelma
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2009
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.783396
https://doi.org/10.1594/PANGAEA.783396