On the Late Precambrian-Early Paleozoic Metavolcanic and Metasedimentary Rocks of the Queen Maud Mountains, Antarctica, and a Comparison With Rocks of Similar Age for Southern Africa

The non-intrusive portion of the late Precambrian-early Paleozoic basement complex in the Queen Maud Mountains, Antarctica, consists of graywacke-shale sequences of the Beardmore Group (Goldie, Duncan, and LaGorce Formations), rhyolite porphyries of the Wyatt Formation, and rhyolite porphyries, mino...

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Bibliographic Details
Main Author: Stump, Edmund
Format: Report
Language:English
Published: Institute of Polar Studies, The Ohio State University 1976
Subjects:
Ross Orogen
Metavolcanic rocks > Queen Maud Land
Antarctica
Metasedimentary rocks > Queen Maud Land
Damara Orogen
Byrd
Queen Maud Land
Fairweather
Beardmore
Wyatt
Goldie
Byrd Glacier
Pensacola Mountains
Antarc*
Online Access:http://hdl.handle.net/1811/54226

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