Provenance of Neoproterozoic and lower Paleozoic siliciclastic rocks of the central Ross orogen, Antarctica: Detrital record of rift-, passive-, and active-margin sedimentation

Siliciclastic rocks in the Transantarctic Mountains record the tectonic transformation from a Neoproterozoic rift-margin setting to a passive-margin and ultimately to an active early Paleozoic orogenic setting along the paleo-Pacific margin of East Antarctica. New U-Pb detrital-zircon ages constrain...

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Bibliographic Details
Published in:Geological Society of America Bulletin
Main Authors: Goodge, John W, Williams, Ian, Myrow, Paul M
Format: Article in Journal/Newspaper
Language:unknown
Published: Association of Engineering Geologists
Subjects:
Online Access:http://hdl.handle.net/1885/86302
https://doi.org/10.1130/B25347.1