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...
Main Authors: | , , |
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Other Authors: | , |
Format: | Book Part |
Language: | unknown |
Published: |
Geological Society of London
2022
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/528156/ https://www.lyellcollection.org/doi/10.1144/M56-2019-44 |