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...
Published in: | The Journal of Geology |
---|---|
Main Authors: | , , , |
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 |