The Weddell Sea Formation: post−Late Pliocene terrestrial glacial deposits on Seymour Island, Antarctic Peninsula
ABSTRACT: A sequence of glacial deposits up to 4 m thick unconformably overlies the Eocene La Meseta Formation on the Seymour Island plateau (meseta) and forms a litho− stratigraphically distinct unit in the succession of the James Ross Basin, which is formally named here as the Weddell Sea Formatio...
Main Authors: | , , , |
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.626.7439 http://www.polar.pan.pl/ppr25/ppr25-189.pdf |