Chemistry of minerals of ODP Hole 103-637A peridotites

The Galicia margin lies northwest of the Iberian Peninsula and is a passive ocean margin with thin sedimentary cover. Altered peridotite was recovered from ODP Site 637, on the north-trending ridge at the western edge of the margin, near the oceanic/continental crust boundary. The altered ultramafic...

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Bibliographic Details
Main Authors: Kimball, Karen L, Evans, Cynthia A
Format: Dataset
Language:English
Published: PANGAEA 1988
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.743572
https://doi.org/10.1594/PANGAEA.743572