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- W2510169726 abstract "Dunites occurring in alkali basalts from oceanic volcanic islands most often are considered as cognate cumulates. This interpretation may be in agreement with the observed paragenesis and the composition of phases (Ol., Sp., Cpx.). An alternative interpretation is here proposed based on microscopic observations as well as thermal history estimated from microprobe data. It is suggested that the studied dunites result from an interaction of mantle-rocks and a percolating magma. Stages of this interaction are : 1/ resorption of pyroxenes ; 2/ thermal reequilibrium of olivines and spinels ; 3/ chemical reequilibrium of olivines and spinels with magma ; 4/ late crystallization of little interstitial clinopyroxenes." @default.
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- W2510169726 date "1984-01-01" @default.
- W2510169726 modified "2023-09-26" @default.
- W2510169726 title "Les dunites en enclaves dans les basaltes alcalins des îles océaniques : approche pétrologique" @default.
- W2510169726 doi "https://doi.org/10.3406/bulmi.1984.7809" @default.
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