Origins of compositional heterogeneity in olivine-hosted melt inclusions from the Baffin Island picrites

The Baffin Island picrites are highly magnesian (< 22 wt% MgO) olivine tholeiites, erupted through felsic continental crust. Plots of most major and minor element oxides against MgO for the lavas define very tight trends consistent with modification of melts parental to the erupted suite by olivi...

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Bibliographic Details
Published in:Contributions to Mineralogy and Petrology
Main Authors: Yaxley, Gregory, Kamenetsky, Vadim S, Kaminska, M, Norman, Marc, Francis, Don
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer
Subjects:
Online Access:http://hdl.handle.net/1885/86478
https://doi.org/10.1007/s00410-004-0613-z
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