Petrology of ultramafic rocks at DSDP Holes 82-556, 82-558, and 82-560

Strongly serpentinized peridotites occur at shallow crustal levels at DSDP Sites 556 (35-Ma-old crust), 558 (35-Maold crust), and 560 (12-Ma-old crust) in the North Atlantic. Primary peridotite silicate minerals are preserved only at Sites 556 and 558, but all three sites have primary spinel preserv...

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Bibliographic Details
Main Authors: Michael, Peter, Bonatti, Enrico
Format: Dataset
Language:English
Published: PANGAEA 1985
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.806240
https://doi.org/10.1594/PANGAEA.806240