Recent extension driven by mantle upwelling beneath the Admiralty Mountains (East Antarctica)

Northern Victoria Land is located at the boundary between an extended, presumably hot, region (West Antarctic Rift System) and the thick, possibly cold, East Antarctic craton. The style and timing of Tertiary deformation along with relationships with the magmatic activity are still unclear, and cont...

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Bibliographic Details
Published in:Tectonics
Main Authors: Faccenna, C., Rossetti, F., Becker, T. W., Danesi, S., Morelli, A.
Other Authors: Faccenna, C.; Università Roma Tre, Rossetti, F.; Università Roma Tre, Becker, T. W.; University of Southern California, USA, Danesi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia, Morelli, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia, Università Roma Tre, University of Southern California, USA, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2008
Subjects:
Online Access:http://hdl.handle.net/2122/4257
https://doi.org/10.1029/2007TC002197