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...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1968
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e68-051 http://www.nrcresearchpress.com/doi/pdf/10.1139/e68-051 |