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- W2912019678 abstract "Dunites occurring in alkali basalts from oceanic volcanic islands cannot be strictly considered as residual rocks. Their olivines are enriched in iron and their spinels are enriched in iron and titanium, during magma-mantle interaction. Some picritic basalts (especially some oceanites) are not directly the cause of the resorption of mantle orthopyroxenes. The resorption begins during emplacement of earlier alkali basalts. The chemical and mineralogical compositions of oceanites result partly from the incorporation of a great amount of reequilibrated mantle-olivines." @default.
- W2912019678 created "2019-02-21" @default.
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- W2912019678 date "1985-01-01" @default.
- W2912019678 modified "2023-09-26" @default.
- W2912019678 title "Le concept de dunites résiduelles et la signification pétrologique de certains magmas picritiques. Réponse au commentaire de A. Nicolas , concernant la note Les dunites en enclaves dans les basaltes alcalins des îles océaniques : Approche pétrologique de E.T. Berger et M. Vannier" @default.
- W2912019678 doi "https://doi.org/10.3406/bulmi.1985.7890" @default.
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