Ultramafic mantle xenoliths in the Late Cenozoic Volcanic rocks of the Antarctic Peninsula and Jones Mountains, West Antarctica

Abundant mantle-derived ultramafic xenoliths occur in Cenozoic (7.7-1.5 Ma) mafic alkaline volcanic rocks along the former active margin of West Antarctica, that extends from the northern Antarctic Peninsula to Jones Mountains. The xenoliths are restricted to post-subduction volcanic rocks that were...

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Bibliographic Details
Main Authors: Leat, Philip T., Ross, Aidan J., Gibson, Sally A.
Other Authors: Martin, A.P., van der Wal, W.
Format: Book Part
Language:unknown
Published: Geological Society of London 2022
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/528156/
https://www.lyellcollection.org/doi/10.1144/M56-2019-44