Tectonic elements of the continental margin of East Antarctica, 38–164ºE

Abstract The East Antarctic continental margin from 38–164ºE is divided into western and eastern provinces that developed during the separation of India from Australia–Antarctica (Early Cretaceous) and Australia from Antarctica (Late Cretaceous). In the overlap between these provinces the geology is...

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Bibliographic Details
Main Authors: P. E. O’brien, H. M. J. Stagg
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.551.7526
http://pubs.usgs.gov/of/2007/1047/srp/srp085/of2007-1047srp085.pdf