Hostname: page-component-cd9895bd7-jn8rn Total loading time: 0 Render date: 2024-12-23T16:26:47.286Z Has data issue: false hasContentIssue false
  • English
  • Français

The Late Pre-Cambrian Stratigraphic Sequence in the Scandinavian Mountain Chain

Published online by Cambridge University Press:  01 May 2009

I. Hernes
I. Hernes
Affiliation:
Geological Institute, University of Bergen, Norway.
Get access Rights & Permissions [Opens in a new window]

Abstract

A late Pre-Cambrian eugeosynclinal stratigraphic sequence in the western part of the Scandinavian mountain chain is established. In the Möre region the succession is about 11 km thick. The wellknown late Pre-Cambrian miogeosynclinal sequence in the eastern part of the chain corresponds to the upper part of the eugeosynclinal sequence.

Type
Articles
Information
Geological Magazine , Volume 104 , Issue 6 , December 1967 , pp. 557 - 563
Copyright
Copyright © Cambridge University Press 1967

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Englund, J.-O., 1966. Studies on the Latest Precambrian and Eocambrian Rocks in Norway. No. 2. Sparagmittgruppens bergarter ved Fåvang, Gudbrandsdalen. Norg. geol. Unders., 238, 55–103.Google Scholar
Geis, H.-P., 1965. Eisen-Titanlagerstatten bei Raudsand, Westnorwegen. Norg. geol. Unders., 234, 15–52.Google Scholar
Gjelsvik, T., 1953. Det nordvestlige gneis-område i det sydlige Norge, aldersforhold og tektonisk-stratigrafisk stilling. Norg. geol. Unders., 184, 71–94.Google Scholar
Harland, W. B., Wallis, R. H., and Gayer, R. A., 1966. A Revision of the Lower Hecla Hoek Succession in Central North Spitsbergen and Correlation Elsewhere. Geol. Mag., 103, 70–97.CrossRefGoogle Scholar
Hernes, I., 1964. Anzeichen einer frühkaledonischen Metamorphose. Neues Jb. Miner. Mh., 110–116.Google Scholar
Hernes, I., 1965. Die kaledonische Schichtenfolge in Mittelnorwegen. Neues Jb. Geol. Paläont. Mh., 69–84.Google Scholar
Hernes, I., 1966 a. Age of the Anorthosites in the Norwegian Caledonian Chain. Nature, Lond., 209, p.191.CrossRefGoogle Scholar
Hernes, I., 1966 b. Zur Deutung der skandinavischen Kaledoniden. Neues Jb. Geol. Paläont. Mh., 449–471.Google Scholar
Hernes, I., (In press.) Zur Geschichte der skandinavischen Gebirgskette. Neues Jb. Geol. Paläont. Mh.Google Scholar
Holtedahl, O., 1938. Geological Observations in the Opdal-Sunndal-Trollheimen District. Norsk geol. Tidsskr., 18, 29–53.Google Scholar
Kolderup, C. F., and Kolderup, N.-H., 1940. Geology of the Bergen Arc System. Bergens Mus. Skr., 20, 1–137.Google Scholar
Oftedahl, C, 1964. Studies in the Trondheim region, Central Norwegian Caledonides. The nature of the basement contact. Norg. geol. Unders., 227, 5–12.Google Scholar
O'Hara, M. J., and Mercy, E. L. P., 1963. Petrology and Petrogenesis of some Garnetiferous Peridotites. Trans. R. Soc. Edinb., 65, 251–314.Google Scholar
Reusch, H. H., 1882. Silurfossiler og pressede konglomerater i Bergensskifrene. Univ. program. Kristiania (Oslo).Google Scholar
Rosenqvist, I. T., 1941. The Lønset anticline in the Opdal area. Norsk geol. Tidsskr., 21, 25–48.Google Scholar
Stille, H., 1946. Die assyntische Ära und der vor-, mit- und nachassyntische Magmatismus. Z. D. geol. Ges., 98, 152–165.Google Scholar
Stille, H., 1958. Die assyntische Tektonik im geologischen Erdbild. Beih. geol. Jb., 22, 1–255.Google Scholar
Strand, T., 1951. The Sel and Vågå map areas. Norg. geol. Unders., 178, 1–118.Google Scholar
Vogt, T., 1924. Forholdet mellem sparagmitsystemet og det marine underkambrium ved Mjösen. Norsk geol. Tidsskr., 7, 281–384.Google Scholar