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The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen

Published online by Cambridge University Press:  01 May 2009

D. L. Dineley
D. L. Dineley
Affiliation:
Geology Department, University of Bristol.
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Abstract

The Lower Old Red Sandstone deposits of Ekmanfjorden belong mainly to the Lykta Division, but pale sandstones with Giganthaspis representingthe Kapp Kjeldsen Division also occur in the core of what is probably a N.-S. striking anticline. The lower beds of the Lykta Division are soft, dull and silty and not very fossiliferous; above them are some 1,100 feet of sandstones and conglomeratic beds alternatingwith shales or marls. Locally abundant vertebrate remains include the guide fossil Doryaspis. Various sedimentary structures suggest rapid deposition on a broad shallow delta front.

Type
Articles
Information
Geological Magazine , Volume 97 , Issue 1 , February 1960 , pp. 18 - 32
Copyright
Copyright © Cambridge University Press 1960

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References

REFERENCES

Bates, D. E. B., and Schwarzacher, W., 1958. The Geology of the Land between Ekmanfjorden and Dicksonfjorden in Central Vestspits-bergen. Geol. Mag., xcv, 219–33.CrossRefGoogle Scholar
Dineley, D. L., 1956. Some Devonian Fish Remains from North Central Vestspitsbergen. Geol. Mag., xciii, 255–60.Google Scholar
Folk, R. L., 1959. Practical petrographic classification of limestones. Bull. Assoc. Amer. Petrol. Geol., 43, 1–38.Google Scholar
Føyn, S., and Heintz, A., 1943. The Downtonian and Devonian Vertebrates of Spitsbergen. VIII—The English-Norwegian-Swedish Expedition 1939: Geological Results. Norges Svalbard-og Ishavs-Undersøk., Skr. 85.Google Scholar
Holtedahl, O., 1926. Notes on the Geology of North-western Spitsbergen. Result. Norske Spitsbergeneneksped., B.1, Nr. 8.Google Scholar
Keunen, Ph. H., 1948. Slumping in the Carboniferous rocks of Pembroke-shire. Quart. Journ. Geol. Soc. Lond., civ, 365–79.CrossRefGoogle Scholar
Quirke, T. T., 1930. Spring pits, sedimentation phenomena. Journ. Geol., xxxviii, 88–91.CrossRefGoogle Scholar
Shrock, L. L., 1948. Sequence in Layered Rocks. New York, 507 pp.Google Scholar
Thomas, G., 1957. In discussion on Gill, W. D., and phKeunen, H., 1957 Sand Volcanoes on Slumps in the Carboniferous of County Clare, Ireland. Quart. Journ. Geol. Soc. Lond., cxiii, 441–57.Google Scholar
Wängsjö, G., 1952. The Downtonian and Devonian Vertebrates of Spitsbergen. IX—Morphologic and systematic studies of the Spitsbergen Cephalaspids. Norsk Polarinst. Skr. 97.Google Scholar
White, E. I., 1950. The Vertebrate Faunas of the Lower Old Red Sandstone of the Welsh Border. II. Pteraspis leathensis White A Dittonian Zone Fossil. Bull. Brit. Mus., Geol., 1, Nr. 3.Google Scholar
White, E. I., 1956. Preliminary note on the range of Pteraspids in Western Europe. Bull. Inst. roy. Sci. nat. Belg., xxxii, 1–10.Google Scholar