The geology and geochronology of the basement complex of the central Transantarctic Mountains

The central part of the Transantarctic Mountain chain consists of a basement complex of igneous and metamorphic rocks overlain nonconformably by sedimentary rocks of late Paleozoic age, including Permian tillites and coal measures. The basement complex is exceptionally well exposed in the Wisconsin...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Faure, Gunter, Murtaugh, J. G., Montigny, R. J. E.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1968
Subjects:
Online Access:http://dx.doi.org/10.1139/e68-051
http://www.nrcresearchpress.com/doi/pdf/10.1139/e68-051