Central volcanoes as sources for the Antarctic Peninsula Volcanic Group
From at least the Early Jurassic to the Miocene, eastward subduction of oceanic crust took place beneath the Antarctic Peninsula. Magmatism associated with the subduction generated a N-S linear belt of volcanic rocks known as the Antarctic Peninsula Volcanic Group (APVG), and which erosion has now e...
Published in: | Antarctic Science |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Cambridge University Press
1994
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/516553/ https://doi.org/10.1017/S0954102094000568 |