Hostname: page-component-78c5997874-j824f Total loading time: 0 Render date: 2024-11-18T14:14:20.988Z Has data issue: false hasContentIssue false
  • English
  • Français

Palynology of the James Ross Island area, Antarctic Peninsula

Published online by Cambridge University Press:  13 May 2004

A.M. Duane ,
D. Pirrie  and
J.B. Riding
A.M. Duane
Affiliation:
AUTHOR(S). 1992. Title. In DUANE, A.M., PIRRIE, D. & RIDING, J.B. eds, Palynology of the James Ross Island area, Antarctic Peninsula. Antarctic Science, 4, page numbers.
D. Pirrie
Affiliation:
AUTHOR(S). 1992. Title. In DUANE, A.M., PIRRIE, D. & RIDING, J.B. eds, Palynology of the James Ross Island area, Antarctic Peninsula. Antarctic Science, 4, page numbers.
J.B. Riding
Affiliation:
AUTHOR(S). 1992. Title. In DUANE, A.M., PIRRIE, D. & RIDING, J.B. eds, Palynology of the James Ross Island area, Antarctic Peninsula. Antarctic Science, 4, page numbers.
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

The James Ross Island area is recognized as one of the geological treasures of Antarctica. It exposes a section of 5–6 km of Cretaceous and Tertiary marine sedimentary strata with an important content of reworked Upper Jurassic rocks near the base. This succession is probably one of the most important Cretaceous sequences in the Southern Hemisphere.

Type
Special Issue
Information
Antarctic Science , Volume 4 , Issue 3 , September 1992 , pp. 258
Copyright
© Antarctic Science Ltd 1992