Cryoturbations: A sediment structural analysis
- 1 October 1992
- journal article
- Published by Wiley in Permafrost and Periglacial Processes
- Vol. 3 (4) , 343-351
- https://doi.org/10.1002/ppp.3430030408
Abstract
Cryoturbations have always provoked discussions on their origin. However, the sedimentary structures which result from the deformations differ according to the mechanism involved. Diagnostic characterization by sedimentary structure is especially suited to distinguish between deformations caused by cryohydrostatic and cryostatic pressure on the one hand and by periglacial loading on the other.Keywords
This publication has 6 references indexed in Scilit:
- Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbationsPermafrost and Periglacial Processes, 1991
- Salt TectonicsScientific American, 1987
- Periglacial Involutions and Mass Displacement Structures, Banks Island, CanadaGeografiska Annaler: Series A, Physical Geography, 1986
- Deformation of laminated silt loam due to repeated freezing and thawing cyclesEarth Surface Processes and Landforms, 1985
- Weichselian Convolution Phenomena and processes in fine sediments.Boreas, 1982
- The origin of hummocks, western Arctic coast, CanadaCanadian Journal of Earth Sciences, 1980