An insight into the first stages of the Ferrar magmatism: ultramafic cumulates from Harrow Peaks, northern Victoria Land, Antarctica

A group of ultramafic xenoliths hosted in Cenozoic hypabyssal rocks from Harrow Peaks (northern Victoria Land, Antarctica) show textural and geochemical features far removed from anything previously observed in mantle xenoliths of this region and elsewhere in Antarctica. They consist of spinel-beari...

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Bibliographic Details
Published in:Contributions to Mineralogy and Petrology
Main Authors: Pelorosso, Beatrice, Bonadiman, Costanza, Ntaflos, Theodoros, Gregoire, Michel, Gentili, Silvia, ZANETTI, Alberto, Coltorti, Massimo
Other Authors: Ntaflos, Theodoro, Zanetti, Alberto
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/11392/2404253
https://doi.org/10.1007/s00410-019-1579-1
https://link.springer.com/content/pdf/10.1007/s00410-019-1579-1.pdf