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...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
1988
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.743572 https://doi.org/10.1594/PANGAEA.743572 |