Early Paleozoic tectonism within the East Antarctic craton: The final suture between east and west Gondwana?

New U-Pb SHRIMP ages from East Antarctica point to the existence of a laterally continuous orogenic belt that bisects the East Antarctic craton. This orogenic belt juxtaposes Archean crust to the south and east against Neoproterozoic metamorphic rocks to

Bibliographic Details
Main Authors: Boger, Steven D., Wilson, Colin J, Fanning, Christopher
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America Inc 2015
Subjects:
Antarctic
East Antarctica
Antarc*
Antarctica
Online Access:http://hdl.handle.net/1885/94152
Description
Summary:New U-Pb SHRIMP ages from East Antarctica point to the existence of a laterally continuous orogenic belt that bisects the East Antarctic craton. This orogenic belt juxtaposes Archean crust to the south and east against Neoproterozoic metamorphic rocks to

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