Oxygen isotope evidence for the origin of pyroxenites in the Beni Bousera peridotite massif, North Morocco: derivation from subducted oceanic lithosphere
- 31 March 1991
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 102 (3-4) , 289-301
- https://doi.org/10.1016/0012-821x(91)90024-c
Abstract
No abstract availableKeywords
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