Till—as a glacial “tectomict”, its internal architecture, and the development of a “typing” method for till differentiation-Reference-Cited by-同舟云学术

Till—as a glacial “tectomict”, its internal architecture, and the development of a “typing” method for till differentiation

Published:2006-04 Issue:1-2 Volume:75 Page:172-200
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

Menzies John,van der Meer Jaap.J.M.,Rose James

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference151 articles.

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2. Allen, J.R.L., 1982. Sedimentary Structures: Their Character and Physical Basis. 2 Volumes, pp. 611 and 679. Elsevier Science Publishing, Amsterdam.

3. Deforming-bed origin for southern Laurentide till sheets?;Alley;J. Glaciol.,1991

4. Continuity comes first; recent progress in understanding subglacial deformation;Alley;Geol. Soc. Spec. Publ.,2000

5. Continuous till deformation beneath ice sheets;Alley;Int. Assoc. Hydrol. Sci.,1987

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