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A comparative analyses of microstructures from Late Jurassic diamictic units, near Helmsdale, northeast Scotland and a Pleistocene diamicton from near Milton, southern Ontario, Canada – a differential diagnostic method of sediment typing using micromorphology

Published online by Cambridge University Press:  24 March 2014

J. Menzies*
Affiliation:
Depts. of Earth Sciences & Geography, Brock University, St. Catharines, Ontario, Canada L2S 3A1
C. Whiteman
Affiliation:
School of the Environment University of Brighton, Brighton, BN2 4GJ, England, U.K.
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Abstract

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Micromorphology is used to examine and compare a Late Jurassic diamictite from northeast Scotland with a Pleistocene diamict from southern Ontario, Canada in order to test if a statistical difference between diamicts can be recognized and used to separate differing types of diamicts/diamictites. The diamictites from Scotland have been ascribed to various depositional agencies occurring in several distinctly differing terrestrial and marine palaeoenvironments. In contrast, the Pleistocene diamicton is regarded as a subglacial till. Both diamicts appear remarkably similar visually and contain many corresponding features such as macrostructures, and exotic and fractured subangular to subrounded clasts. Micromorphology is used to re-examine these diamicts/diamictites at the microscopic level to detect if the palaeoenvironments within which they were deposited can be ascertained. In this paper a quantitative assessment of microstructures using micromorphology is developed. Comparative statistical analyses of these diamicts, using micromorphological features, reveals that the Jurassic diamictites are non-glacigenic, non-terrestrial and most likely deposited within a marine environment as a result of subaquatic debris mass movement, while, in contrast, the Pleistocene diamicts were most likely subglacial tectomicts deposited beneath the active base of the Laurentide Ice Sheet.

Type
Research Article
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2009

References

Abbink, O., Targarona, J., Brinkhuis, H. & Visscher, H., 2001. Late Jurassic to earliest Cretaceous palaeoclimatic evolution of the southern North Sea. Global and Planetary Change 30: 231256.Google Scholar
Allaby, A. & Allaby, M., (eds), 1999. The Dictionary of Earth Sciences, Oxford University Press (NY) USA: 512pp.Google Scholar
Allen, J.R.L., 1982. Sedimentary Structures: Their Character and Physical Basis. 2 Volumes. Elsevier Science Publishing (Amsterdam): 611 and 679pp.Google Scholar
Bailey, E.B., & Weir, J., 1932. Submarine faulting in Kimmeridgian times: East Sutherland. Transactions of the Royal Society of Edinburgh 47: 431467.Google Scholar
Bailey, E.B., Collet, L.W. & Field, R.M., 1928. Paleozoic submarine landslips near Quebec City. Journal of Geology 36: 577.Google Scholar
Bardou, E., Boivin, P. & Pfeifer, H.-R., 2007. Properties of debris flow deposits and source materials compared: implications for debris flow characterization. Sedimentology 54: 469–480.Google Scholar
Barnett, P.J., 1992. Quaternary. In: Thurston, P.C., Williams, H. R., Sutcliffe, R. H., Stott, G. M. (eds): Geology of Ontario, Ontario Geological Survey (Toronto): 10111090.Google Scholar
Bertran, P., 1993. Deformation-induced microstructures in soils affected by mass movements. Earth Surface Processes and Landforms 18: 645660.CrossRefGoogle Scholar
Bertran, P., & Texier, J.-P., 1999. Sedimentation Processes and Facies on a Semi-Vegetated, Talus, Lousteau, Southwestern France. Earth Surface Processes and Landforms 24: 177188.3.0.CO;2-R>CrossRefGoogle Scholar
Blake, J.F., 1902. On a remarkable inlier among the Jurassic rocks of Sutherland and its bearing on the origin of the breccia-beds. Quarterly Journal of the Geological Society of London 57: 290312.Google Scholar
Boës, X. & Fagel, N., 2005 Impregnation method for detecting annual laminations in sediment cores: an overview. Sedimentary Geology 179: 185194.Google Scholar
Boulton, G.S., & Zatsepin, S., 2006. Hydraulic impacts of glacier advance over a sediment bed. Journal of Glaciology 179: 497527.CrossRefGoogle Scholar
Camuti, K.P. & McGuire, P., 1999. Preparation of polished thin-sections from poorly consolidated regolith and sediment materials. Sedimentary Geology 128: 171178.Google Scholar
Carr, S.J., 2000. Micromorphological evidence supporting late Weichselian glaciation of the northern North Sea. Boreas 29: 315328.CrossRefGoogle Scholar
Crowell, J.C., 1961. Depositional structures from Jurassic boulder beds, east Sutherland. Transactions of the Edinburgh Geological Society 18, 202220.CrossRefGoogle Scholar
Crowell, J.C., 1999. Pre-Mesozoic ice ages; their bearing on understanding the climate system. Memoir - Geological Society of America 192: 106pp.Google Scholar
Evans, D.J.A., Phillips, E.R., Hiemstra, J.F. & Auton, C.A., 2006. Subglacial till: formation, sedimentary characteristics and classification. Earth Science Reviews 78: 115176.Google Scholar
Eyles, N, Eyles, C.H. & Menzies, J., submitted. Rapid generation of deformation till below a fast flowing Laurentide Ice Sheet lobe: Wildfield Till, Southern Ontario, Canada. Quaternary Science Reviews.Google Scholar
Flint, R.F., 1971. Glacial and Quaternary Geology, John Wiley & Sons (New York and London): 892pp.Google Scholar
Folk, R.L., 1954. The distinction between grain size and mineral composition in sedimentary rock nomenclature. Journal of Geology 62: 344359.Google Scholar
Friedman, G.M., 2003. Classification of Sediments and Sedimentary Rocks. In: Middleton, G.V. et al. (eds): Encyclopedia of Sediments and Sedimentary Rocks, Kluwer Academic Publishers (Dordrecht): 127136.Google Scholar
Hart, J.K., 2006. An investigation of subglacial processes at the microscale from Briksdalsbreen, Norway. Sedimentology 53: 125146.CrossRefGoogle Scholar
Hiemstra, J.F., & Van der Meer, J.J.M., 1997. Pore-water controlled grain fracturing as indicator for subglacial shearing in tills. Journal of Glaciology 43: 446454.Google Scholar
Hiemstra, J.K. & Rijsdijk, K.F., 2003. Observing artificially induced strain: implications for subglacial deformation. Journal of Quaternary Science 18: 373383.CrossRefGoogle Scholar
Hudson, J.D. & Trewin, N.H., 2002. Jurassic. In: Trewin, N.H. (ed.): The Geology of Scotland, The Geological Society of London (London): 323350.Google Scholar
Jenner, K.A., Piper, D.J.W., Campbell, D.C. & Mosher, D.C., 2007. Lithofacies and origin of late Quaternary mass transport deposits in submarine canyons, central Scotian Slope, Canada Sedimentology 54: 1938.Google Scholar
Judd, J.W., 1873. The secondary rocks of Scotland. Quarterly Journal of the Geological Society of London 29: 97195.Google Scholar
Karrow, P.F., 1987. Quaternary geology of the Hamilton-Cambridge area, southern Ontario. Ontario Geological Survey Report 255, Ontario Geological Survey, Toronto, Canada.Google Scholar
Karrow, P.F., 1989. Quaternary geology of the Great Lakes subregion. In: Fulton, R.J. (ed.): Quaternary Geology of Canada and Greenland. Geological Survey of Canada No. 1 also Geological Society of America, The Geology of North America v. K-1: 326350.Google Scholar
Kemp, R.A., 1985. Soil Micromorphology and the Quaternary. Quaternary Research Association Technical Guide No. 2: 80pp.Google Scholar
Kubiëna, W.L., 1938. Micropedology. Collegiate Press (Ames, Iowa): 243pp.Google Scholar
Lachniet, M.S., Larson, G.J., Lawson, D.E., Evenson, E.B. & Alley, R.B., 2001. Microstructures of sediment flow deposits and subglacial sediments. Boreas 30: 254262.Google Scholar
Larsen, N.K., Piotrowski, J.A., Christoffersen, P. & Menzies, J., 2006. Formation and deformation of basal till during a glacier surge; Elisebreen, Svalbard. Geomorphology 81: 217234.Google Scholar
Larsen, N.K., Piotrowski, J.A. & Menzies, J., 2007. Microstructural evidence of low-strain, time-transgressive subglacial deformation. Journal of Quaternary Science 22: 593608.Google Scholar
Lee, J.R. & Phillips, E.R., 2008. Progressive soft sediment deformation within a subglacial shear zone – a hybrid mosaic-pervasive deformation model for Middle Pleistocene glaciotectonised sediments from eastern England. Quaternary Science Reviews, 27: 13501362.Google Scholar
MacDonald, A.C.T. & Trewin, N.H., 1993. The Upper Jurassic of the Helmsdale area. In: Trewin, N.H. (ed.): Excursion guide to the geology of East Sutherland and Caithness. Scottish Academic Press (Edinburgh): 75114.Google Scholar
Maltman, A.J., 1988. The importance of shear zones in naturally deformed wet sediments. Tectonophysics 145: 163175.Google Scholar
Maltman, A.J. (ed), 1994. The geological deformation of sediments. Chapman & Hall (London): 362pp.Google Scholar
Matsuda, J.-i., 2000. Seismic deformation structures of the post-2300 a BP muddy sediments in Kawachi lowland plain, Osaka, Japan. Sedimentary Geology 135: 99116.Google Scholar
Menzies, J., 2000a. Micromorphological analyses of microfabrics and microstructures, indicative of deformation processes, in glacial sediments. In: Maltman, A.J., Hubbard, B. & Hambrey, M.J. (eds): Deformation of Glacial Materials (Geological Society, London): 245258.Google Scholar
Menzies, J., 2000b. Microstructures in diamictites of the lower Gowganda Formation (Huronian), near Elliot Lake, Ontario; evidence for deforming-bed conditions at the grounding line? Journal of Sedimentary Research 70: 210216.Google Scholar
Menzies, J. & Brand, U., 2007. The internal sediment architecture of a drumlin, Port Byron, New York State, USA. Quaternary Science Reviews 26: 322335.Google Scholar
Menzies, J. & Shilts, W.W., 1996. Subglacial Environments. In: Menzies, J. (ed): Past Glacial Environments – sediments, forms and techniques. Butterworth-Heinemann (Oxford): 15136.Google Scholar
Menzies, J. & Taylor, J.M., 2003. Seismically induced soft-sediment microstructures (seismites) from Meikleour, western Strathmore, Scotland. Boreas 32: 314327.Google Scholar
Menzies, J. & Zaniewski, K., 2003. Microstructures within a modern debris flow deposit derived from Quaternary glacial diamicton – a comparative micromorphological study. Sedimentary Geology 157: 131–48.Google Scholar
Menzies, J., Van der Meer, J.J.M. & Rose, J., 2006. Till – as a Glacial ‘Tectomict’, its internal architecture, and the development of a ‘typing’ method for till differentiation. Geomorphology 75: 172200.Google Scholar
Mulder, T. & Alexander, J., 2001. The physical character of subaqueous sedimentary density flows and their deposits. Sedimentology 48: 269299.CrossRefGoogle Scholar
Murchison, R.I., 1827. On the coal-field of Brora in Sutherlandshire. Transactions Geological Society of London 2: 293326.Google Scholar
Norton, W.H., 1917. A classification of breccias. Journal of Geology 25: 160.CrossRefGoogle Scholar
O'Brien, N.R. & Slatt, R.M., 1990. Argillaceous Rock Atlas. Springer-Verlag (New York): 141 ppGoogle Scholar
Pettijohn, F.J., 1975. Sedimentary Rocks. Harper Row (New York): 628 pp.Google Scholar
Phillips, E.R., 2006. Micromorphology of a debris flow deposit: evidence of basal shearing, hydrofracturing, liquefaction and rotational deformation during emplacement. Quaternary Science Reviews 25: 720738.CrossRefGoogle Scholar
Phillips, E.R. & Auton, C.A., 2000. Micromorphological evidence for polyphase deformation of glaciolacustrine sediments from Strathspey, Scotland. In: Maltman, A.J., Hubbard, B. & Hambrey, M.J., (eds): Geological Society of London (London): 279292.Google Scholar
Phillips, E.R. & Auton, C. A., 2007. Microtextural analysis of a glacially ‘deformed’ bedrock: implications for inheritance of preferred clast orientations in diamictons. J. Quaternary Science 23: 229240.Google Scholar
Phillips, E.R., Evans, D.J.A. & Auton, C.A., 2002. Polyphase deformation at an oscillating ice margin following the Loch Lomond Readvance, central Scotland, UK. Sedimentary Geology 149: 157182.Google Scholar
Pickering, K.T., 1984. The Upper Jurassic ‘Boulder Beds’ and related deposits: a fault-controlled submarine slope, NE Scotland. Journal of the Geological Society of London 141: 357374.Google Scholar
Price, G.D., 1999. The evidence and implications of polar ice during the Mesozoic. Earth Science Reviews 48: 183210.Google Scholar
Ramsay, A.C., 1865. The Glacial Theory of Lake Basins. Philosophical Magazine 29: 285.Google Scholar
Schermerhorn, L.J.G., 1966. Terminology of mixed coarse-fine sediments. Journal of Sedimentary Petrology 36: 831835.CrossRefGoogle Scholar
Schieber, J., 2003. Depositional fabric of mudstones. In: Middleton, G.V. et al. (eds): Encyclopedia of Sediments and Sedimentary Rocks, Kluwer Academic Publishers (Dordrecht): 203207.Google Scholar
Scott, B. & Price, S., 1988. Earthquake-induced structure in young sediments. Tectonophysics 147: 165170.Google Scholar
Stewart, I.S., Sauber, J. & Rose, J., 2000. Glacio-Seismotectonics: Ice Sheets, Crustal Deformation and Seismicity. Quaternary Science Reviews 19: 13671389.CrossRefGoogle Scholar
Stoops, G., 2003. Guidelines for analysis and description of soil and regolith thin sections. Soil Science Society of American (Madison, WI): 184 pp.Google Scholar
Thomason, J.F. & Iverson, N.R., 2006. Microfabric and microshear evolution in deformed till. Quaternary Science Reviews 25: 10271038.Google Scholar
Van der Meer, J.J.M., 1993. Microscopic evidence of subglacial deformation. Quaternary Science Reviews 12: 553587.Google Scholar
Van der Meer, J.J.M., 1996. Micromorphology. In: Menzies, J, (ed.), Past Glacial Environments – sediments, forms and techniques. Butterworth-Heinemann (Oxford): 335356.Google Scholar
Van der Meer, J.J.M., Menzies, J. & Rose, J., 2003. Subglacial till: the deforming glacier bed. Quaternary Science Reviews 22: 16591685.Google Scholar
Wignall, P.B.P. & Pickering, K.T., 1993. Palaeoecology and sedimentology across a Jurassic fault scarp, NE Scotland. Journal of the Geological Society of London 150: 323340.Google Scholar
Ziegler, P.A., 1990. Geological Atlas of Western and Central Europe (2nd ed.) Shell International Exploration and Production, the Hague.Google Scholar