U-Pb (zircon) geochronologic analyses for rocks of the Transantarctic Mountains (Table 4.3-1)
The Byrd Glacier discontinuity us a major boundary crossing the Ross Orogen, with crystalline rocks to the north and primarily sedimentary rocks to the south. Most models for the tectonic development of the Ross Orogen in the central Transantarctic Mountains consits of two-dimensional transects acro...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2007
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.611703 https://doi.org/10.1594/PANGAEA.611703 |