Age and provenance of the Beardmore Group, Antarctica: Constraints on Rodinia supercontinent breakup

New U-Pb ages for detrital and igneous zircons constrain the depositional age and sedimentary provenance of the Beardmore Group, a siliciclastic succession that records transformation of the East Antarctic margin during Rodinia breakup and subsequent Gondwana amalgamation. We divide rocks previously...

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Bibliographic Details
Published in:The Journal of Geology
Main Authors: Goodge, John W, Myrow, Paul M, Williams, Ian, Bowring, Samuel A
Format: Article in Journal/Newspaper
Language:unknown
Published: University of Chicago Press
Subjects:
Online Access:http://hdl.handle.net/1885/92336
https://doi.org/10.1086/340629