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James Ross Basin workshop

Published online by Cambridge University Press:  13 May 2004

Rodney M. Feldmann
Affiliation:
Department of Geology, Kent State University, Kent, Ohio 44242, USA
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The rocks of the James Ross Basin consist of a 6 km-thick, relatively complete sequence of Early Cretaceous-Eocene marine sediments, which are remarkably well exposed over Seymour, Vega, James Ross, and Snow Hill islands. Throughout most of the sequence, macrofossils and microfossils are extremely abundant and diverse.

Type
Short Note
Copyright
© Antarctic Science Ltd 1992