Publisher's Synopsis
Excerpt from British Antarctic Expedition 1907-9, Under the Command of Sir E. H. Shackleton, C. V. O; Reports on the Scientific Investigations, Vol. 1: Geology: Glaciology, Physiography, Stratigraphy, and Tectonic Geology of South Victoria Land
It would seem, therefore, that in East Antarctica the great Schild has formed a land surface, subsequent to the extensive lower Cambrian transgression, from Devonian times down to the present.
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