Chronology of Caledonian tectonothermal activity within the Gaissa and Laksefjord Nappe Complexes (Lower Allochthon), Finnmark, Norway: Evidence from K—Ar and 40Ar/39Ar ages-Reference-Cited by-同舟云学术

Chronology of Caledonian tectonothermal activity within the Gaissa and Laksefjord Nappe Complexes (Lower Allochthon), Finnmark, Norway: Evidence from K—Ar and 40Ar/39Ar ages

Published:1989 Issue: Volume: Page:9-26
ISSN:
Container-title:The Caledonide Geology of Scandinavia
language:
Short-container-title:

Author:

Dallmeyer R. D.,Reuter A.,Clauer N.,Liewig N.

Publisher

Springer Netherlands

Link

http://link.springer.com/content/pdf/10.1007/978-94-009-2549-6_2.pdf

Reference53 articles.

1. U.S. Geological Survey Open-File Report;EC Alexander Jr.,1978

2. Andersen, T. B. (1981). The structure of the Mageroy Nappe, Finnmark, North Norway. Norges Geol. Unders. 363, 1–23.

3. Andersen, T. B., Austrheim, H., Sturt, B. A., Pedersen, S. and Kjaersrud, K. (1982). Rb-Sr whole-rock ages from Mageroy, north Norwegian Caledonides. Norsk Geol. Tidsskr. 62, 79–85.

4. Bevins, R. E., Robinson, D., Gayer, R. A. and Allman, S. (1986). Low-grade metamorphism and its relationship to thrust tectonics in the Caledonides of Finnmark, North Norway. Norges Geol. Unders. Bull. 404, 31–42.

5. Bonhomme, M., Thuizat, R., Pinault, Y., Clauer, N., Wendling, A. and Winkler, R. (1975). Méthode de datation potassium-argon. Appareillage et technique; Note technique de l’Institut de Géologie, Univ. L. Pasteur, Strasbourg, vol. 3.

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