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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Language: | English |
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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 |