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...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Leat, Philip T., Scarrow, Jane H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1994
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102094000568
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102094000568