Chemical composition of mineral phases of serpentinized and steatized peridotite from the Mid Atlantic Ridge (15°20'N Fracture Zone, ODP Leg209)

Serpentinization of abyssal peridotites is known to produce extremely reducing conditions as a result of dihydrogen (H2,aq) release upon oxidation of ferrous iron in primary phases to ferric iron in secondary minerals by H2O.We have compiled and evaluated thermodynamic data for Fe-Ni-Co-O-S phases a...

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Bibliographic Details
Main Authors: Klein, Frieder, Bach, Wolfgang
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2010
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.736007
https://doi.org/10.1594/PANGAEA.736007