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Late Precambrian resedimented conglomerates from Bellsund, Spitsbergen

Published online by Cambridge University Press:  01 May 2009

P. Waddams
P. Waddams
Affiliation:
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ
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Summary

Late Precambrian polymict conglomerates are described from Bellsund, western Spitsbergen, where they are intimately associated with authentic glacigenic sediments. They display normal, compound and reverse grading. Spectacular flame, injection and incipient rip-up structures are developed at the base of some beds. The conglomerates were initially deposited either as foreset debris beneath a wet-based glacier, or on the subaqueous part of a glaciomarine outwash delta, and were subsequently redeposited from mass gravity flows initiated by slumping on the unstable glacial detritus slope. An informal stratigraphic nomenclature is proposed for the Kapp Martin area to the north of Bellsund and the Kapp Lyell area to the south.

Type
Articles
Information
Geological Magazine , Volume 120 , Issue 2 , March 1983 , pp. 153 - 164
Copyright
Copyright © Cambridge University Press 1983

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References

REFERENCES

Anketell, J. M., Gegla, J. & Dzulynski, S. 1970. On the deformational structures in systems with reversed density gradients. Ann. Soc. Geol. Pologne 15, 3–29.Google Scholar
Birkenmajer, K. 1960. Relation of the Cambrian to the Precambrian in Hornsund, Vestspitsbergen. Int. geol. cong. Rept. 21st session, Norden, Part 8, 64–74.Google Scholar
Birkenmajer, K. 1972. Cross-bedding and stromatolites in the Precambrian Høferpynten Dolomite Formation of Sørkapp Land, Spitsbergen. Årbok Norsk Polarinst. 1970 (Oslo, 1972), pp. 128–45.Google Scholar
Birkenmajer, K. 1975. Caledonides of Svalbard and Plate Tectonics. Bull. geol. Soc. Denmark 24, 1–19.Google Scholar
Carey, S. W. & Ahmed, N. 1961. Glacial marine sedimentation. In Geology of the Arctic 2, (ed. Raasch, G. O.), pp. 865–94. Toronto: University of Toronto Press.CrossRefGoogle Scholar
Culver, S. J., Williams, H. R. & Bull, P. A. 1978. Infracambrian glaciogenic sediments from Sierra Leone. Nature, Phys. Sci., Lond. 274, 49–51.CrossRefGoogle Scholar
Davies, I. C. & Walker, R. G. 1974. Transport and deposition of resedimented conglomerates: The Cap Enragé Formation, Cambro-Ordovician, Gaspé, Quebec. J. sedim. Petrol. 44, 1200–16.Google Scholar
Dzulynski, S. & Walton, E. K. 1965. Sedimentary Features of Flysch and Greywacke. 274 pp. Amsterdam: Elsevier.Google Scholar
Edwards, M. B. 1976. Sedimentology of Late Precambrian Sveanor and Kapp Sparre Formations at Aldousbreen, Wahlenbergfjorden, Nordaustlandet. Årbok Norsk Polarinst. 1974 (Oslo, 1976), pp. 51–62.Google Scholar
Edwards, M. B. 1978. Glacial environments. In Sedimentary Environments and Facies (ed. Reading, H. G.), pp. 416–38. Oxford: Blackwell.Google Scholar
Elliott, R. E. 1965. A classification of subaqueous sedimentary structures based on rheological and kinematic parameters. Sedimentology 5, 193–209.CrossRefGoogle Scholar
Enos, P. 1969. Anatomy of a flysch. J. sedim. Petrol. 39, 680–723.Google Scholar
Fisher, R. V. & Mattinson, J. M. 1968. Wheeler Gorge turbidite-conglomerate series, California, inverse grading. J. sedim. Petrol. 38, 1013–23.Google Scholar
Flood, B., Gee, D. G., Hjelle, A., Siggerud, T. & Winsnes, T. S. 1969. The Geology of Nordaustlandet, northern and central parts. Skr. norsk Polarinst, Nr 146, 139 pp.Google Scholar
Gill, W. D. & Kuenen, Ph. H. 1957. Sand volcanoes on slumps in the Carboniferous of County Clare, Ireland. Q. Jl geol. Soc. Lond. 113, 441–60.CrossRefGoogle Scholar
Hambrey, M. J. 1982. Late Precambrian diamictites of north eastern Svalbard. Geol. Mag. 119, 527–51.CrossRefGoogle Scholar
Hambrey, M. J., Harland, W. B. & Waddams, P. 1981. Late Precambrian tillites of Svalbard. In The Earth's Pre-Pleistocene Glacial Record, (ed. Hambrey, M. J. & Harland, W. B.), pp. 592–601. Cambridge: Cambridge University Press.Google Scholar
Hambrey, M. J. & Waddams, P. 1981. Deformed stones of varied lithology in Late Precambrian tillites, western Spitsbergen. J. geol. Soc. Lond. 138, 445–53.CrossRefGoogle Scholar
Harland, W. B. 1978. The Caledonides of Svalbard. In IGCP Project 27: Caledonian Appalachian Orogen of the North Atlantic Region. Pap. geol. Surv. Can. 78–13.Google Scholar
Harland, W. B. 1979. A reconsideration of Late Precambrian stratigraphy of Southern Spitsbergen. Polarforschung 48, 44–61.Google Scholar
Heezen, B. C. & Hollister, C. D. 1964. Turbidity currents and glaciation. In Problems in Palaeoclimatology, (ed. Nairn, A. E. M.), pp. 119–49. London: lnterscience.Google Scholar
Hendry, H. E. 1973. Sedimentation of deep water conglomerates in Lower Ordovician rocks of Quebec - composite bedding produced by progressive liquefaction of sediment? J. sedim. petrol. 43, 125–36.CrossRefGoogle Scholar
Hjelle, A. 1962. Contribution to the geology of the Hecla Hoek Formation in Nordenskiøld Land, Vestspitsbergen. Åbok Norsk Polarinst. 1961 (Oslo, 1962), 83–95.Google Scholar
Hjelle, A. 1969. Stratigraphic correlation of Hecla Hoek successions of north and south of Bellsund. Åbok Norsk Polarinst. 1967 (Oslo, 1969), 46–51.Google Scholar
Kelling, G. & Walton, E. K. 1957. Load-cast structures: their relationship to upper-surface structures and their mode of formation. Geol. Mag. 94, 481–90.CrossRefGoogle Scholar
Krasil'shchikov, A. A. 1967. Tillite-like rocks of North East Land. In Materials on the Stratigraphy of Spitsbergen, (ed. Sokolov, V. N.), pp. 36–62. Leningrad: Institute for Geology of the Arctic, (NII GA). (In Russian).Google Scholar
Kuenen, Ph. H. & Menard, H. W. Turbidity currents graded and non-graded deposits. J. sedim. Petrol. 22, 83–96.Google Scholar
Kulling, O. 1934. Scientific results of the Swedish-Norwegian Arctic Expedition in the summer of 1931. Vol. II, Part XI: The ‘Hecla Hoek Formation’ round Hinlopenstredet. Geogr. Annlr Stockh. 16, 161–254.Google Scholar
Middleton, G. V. 1970. Experimental studies related to problems of flysch sedimentation. In Flysch Sedimentology in North America, (ed. J., Lajoie), pp. 253–72. Spec. Pap. geol. Assoc. Can. 7.Google Scholar
Middleton, G. V. & Hampton, M. A. 1973. Sediment gravity flows: mechanics of flow and deposition. In Turbidites and Deep-water Sedimentation (ed. Middleton, G. V. and Bouma, A. H.). Shortcourse Lecture Notes Soc. econ. Paleont. Miner. Los Angeles.Google Scholar
Middleton, G. V. & Hampton, M. A. 1976. Subaqueous sediment transport and deposition by sediment gravity flows. In Marine Sediment Transport and Environmental Management, (ed. Stanley, D. J. and Swift, D. J. P.), pp. 197–218. New York: John Wiley.Google Scholar
Nystuen, J. P. 1976. Facies and sedimentation of the Late Precambrian Moelv Tillite in the eastern part of the sparagmite region, Southern Norway. Norg. geol. Unders. 329.Google Scholar
Orvin, A. K. Outline of the Geological History of Spitsbergen. Skr. Svalb og Ishavet Nr 78.Google Scholar
Pettijohn, F. J. & Potter, P. E. Atlas and Glossary of Primary Sedimentary Structures. New York: Springer.CrossRefGoogle Scholar
Pickton, C. A. G. & Harland, W. B. 1978. Cambridge Spitsbergen Expedition, 1978. Polar Record 19, 377–8.CrossRefGoogle Scholar
Reading, H. G. & Walker, R. G. 1966. Sedimentation of Eocambrian tillites and associated sediments in Finnmark, Northern Norway. Palaeogeogr. Palaeoclim. Palaeoecol. 2, 177–212.CrossRefGoogle Scholar
Sanders, J. E. 1965. Primary sedimentary structures formed by turbidity currents and their hydrodynamic interpretation. Spec. Publs. Soc. econ. Palaeont. Miner. 12.Google Scholar
Selley, R. C. 1978. Ancient Sedimentary Environments. London: Chapman and Hall.Google Scholar
Selley, R. C., Shearman, D. J. & Watson, J. 1963. Some underwater disturbances in the Torridonian of Skye and Raasay. Geol. Mag. 100, 224–43.CrossRefGoogle Scholar
Sullwold, H. 1959. Nomenclature of load deformation in turbidites. Bull. geol. Soc. Am. 70, 1247–8.CrossRefGoogle Scholar
Sutton, J. & Watson, J. 1960. Sedimentary structures in the Epidotic Grits of Skye. Geol. Mag. 97, 106–22.CrossRefGoogle Scholar
Walker, R. G. 1975. Generalized facies models for resedimented conglomerates of turbidite association. Bull. geol. Soc. Am. 86, 737–48.2.0.CO;2>CrossRefGoogle Scholar
Walker, R. G. 1977. Deposition of upper Mesozoic resedimented conglomerates and associated turbidites in southwestern Oregon. Bull. geol. Soc. Am. 88, 273–85.2.0.CO;2>CrossRefGoogle Scholar
Walton, E. K. 1956. Limitations of graded bedding and alternate criteria of upward sequence in the rocks of the Southern Uplands. Trans. Edinb. geol. Soc. 16, 267–71.CrossRefGoogle Scholar
Wilson, C. B. & Harland, W. B. 1964. The Polarisbreen Series and other evidences of late Pre-Cambrian Ice Ages in Spitsbergen. Geol. Mag. 101, 198–219.CrossRefGoogle Scholar