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The Geology of the Snøfjella and Dovrefjella in Vestspitsbergen

Published online by Cambridge University Press:  01 May 2009

John Preston
John Preston
Affiliation:
Department of Geology, The Queen's University, Belfast.
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Abstract

The area yields marbles, schists, and quartzites, probably of Hecla Hoek age, a series similar in lithology to those in the Kongsfjorden region. Their structure and metamorphic condition fit in with the general picture of Caledonian trend and of increasing orogenic activity westwards. Later faulting along the western edge of a graben has broken this ground up into independent blocks as witnessed by the disposition of the Devonian conglomerates. The youngest rocks are a southerly outlier of the plateau basalts best seen around Woodfjorden, remnants of at least two flows are preserved, both of olivine basalt rich in olivine phenocrysts and carrying inclusions of a more alkaline rock type.

Type
Articles
Information
Geological Magazine , Volume 96 , Issue 1 , February 1959 , pp. 45 - 57
Copyright
Copyright © Cambridge University Press 1959

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References

V. REFERENCES

Backlund, H., 1911. Uber einige Olivinknollen aus der Lava von Wood-Bay Spitzbergen. Skr. VidenskSelsk. Krist., 1. Mat-Nat. Kl. No. 16.Google Scholar
Føyn, S., and Heintz, A., 1943. The Downtonian and Devonian Vertebrates of Spitsbergen. Skr. Svalb. og Ishavet, No. 85.Google Scholar
Hallimond, A. F., 1950. Universal stage methods. Mining Mag., lxxxiii, 12–22.Google Scholar
Harland, W. B., and Wilson, C. B., 1956. The Hecla Hoek succession in Ny Friesland, Spitsbergen. Geol. Mag., xciii, 265–286.CrossRefGoogle Scholar
Hoel, A., and Holtedahl, O., 1911. Les nappes de laves, les volcans et les sources thermales dans les environs de la Baie Wood au Spitsberg. Skr. VidenskSelsk. Krist., 1. Mat-Nat. Kl. No. 8.Google Scholar
Hoel, A., and Holtedahl, O., 1914. Nouvelles observations sur le district volcanique du Spitsberg du nord. Skr. VidensSelsk. Krist., 1. Mat-Nat. Kl. No. 9.Google Scholar
Holtedahl, O., 1914. New Features in the Geology of Northwestern Spitsbergen. Amer. Journ. Sci., Ser. 4, xxxvii, 415–424.CrossRefGoogle Scholar
Holtedahl, O., 1926. Notes on the geology of north-western Spitsbergen. Skr. Svalb. og Ishavet, No. 8.Google Scholar
Isachsen, G., 1916. Travaux Topographiques de l'Expedition Isachsen 1909‐1910. Expedition Isachsen, Resultats Scientifiques, ii, 1–61. Kristiania, 1916.Google Scholar
Orvin, A. K., 1934. Geology of the Kings Bay region, Spitsbergen, with special reference to the coal deposits. Skr. Svalb. og Ishavet, No. 57, 1–195.Google Scholar
Orvin, A. K., 1940. Outline of the geological history of Spitsbergen. Skr. Svalb. og Ishavet, No. 78, 1–57.Google Scholar
Tyrrell, G. W., 1924. The geology of Prince Charles Foreland, Spitsbergen. Trans. Roy. Soc. Edinb., liii, 443–478.Google Scholar