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Journal of the Geological Society; 2008; v. 165; issue.1; p. 19-29;
DOI: 10.1144/0016-76492007-002
© 2008 Geological Society of London

Original Article

First-order reconstructions of a Late Ordovician Saharan ice sheet

D.P. Le Heron1 & J. Craig2

1 Institüt für Geologie, Callinstraße 30, Leibniz Universität, Hannover, D-30167, Germany (e-mail: daniel.leheron{at}geowi.uni-hannover.de)
2 ENI E & P, 1 Via Emilia, San Donato Milanese, 20097 Milan, Italy

Synthesis of outcrop and subsurface sedimentological and geomorphological datasets across North Africa allows a tentative palaeo-glaciological model of the flow dynamics and recessional character of a 440 Ma old (Hirnantian) ice sheet to be proposed. A system of eight cross-shelf trough depocentres is identified from the Late Ordovician of the Sahara region. These are interpreted to have been carved and occupied by ice streams, providing evidence for widespread heterogeneous flow within the ice sheet. During retreat, two key geological features were produced: (1) laterally extensive, sinuous to linear piles of sediment dumped parallel to the ice margin; (2) large meltwater channels (tunnel valleys) cut near the grounding line.





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D. P. Le Heron and J. A. Dowdeswell
Calculating ice volumes and ice flux to constrain the dimensions of a 440 Ma North African ice sheet
Journal of the Geological Society, 2009; 166: 277 - 281.
[Abstract] [Full Text] [PDF]