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...

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Bibliographic Details
Main Authors: Stump, Edmund, Gootee, Brian, Lauria, Mary-Lou
Format: Dataset
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.611703
https://doi.pangaea.de/10.1594/PANGAEA.611703