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- W2015413424 abstract "Chrome-spinels in the stratiform complex of Rhum, Scotland, have compositions that lie along two reaction trends, with the composition of a given crystal being determined by its local environment. Crystals in chrome-spinel rich seams between allivalite and peridotite, or disseminated in adcumulates of allivalite or peridotite, have compositions defining a reaction trend involving a marked change in the CrAl ratio and little variation in Fe3+ (Al-trend). Chrome-spinel crystals in cumulates that contain crystallized trapped liquid, define a reaction trend involving a marked change in Fe3+ (Fe-trend). Evidence is presented to show that the Al-trend results from reaction of cumulus chromite, cumulus olivine and either plagioclase or a liquid rich in the plagioclase component, whereas the Fe-trend results from reaction of only cumulus chromite and trapped liquid. Some of the implications of these findings are discussed." @default.
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- W2015413424 date "1975-06-01" @default.
- W2015413424 modified "2023-10-06" @default.
- W2015413424 title "Reaction trends shown by chrome-spinels of the Rhum layered intrusion" @default.
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- W2015413424 doi "https://doi.org/10.1016/0016-7037(75)90045-9" @default.
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