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A Structural Study of the Southern End of the French Jura

Published online by Cambridge University Press:  01 May 2009

Maurits Lindström
Maurits Lindström
Affiliation:
Department of Geology, University of Lund, Sweden.
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Abstract

In the Chambéry region, Jura folds with a north-north-west trend meet the boundary of the Subalpine zone, which strikes north-north-east. The two fold trends were probably not formed at exactly the same time. Minor folding, thrusting on steep planes, wrench-faulting, formation of sub-horizontal stylolites, and opening of filled joints all took place during a succession of tectonic events with maximum compression at about east-west, after the aforementioned fold-trends had been formed. The evidence considered in this study seems incompatible with hypotheses of deformation by gravitational gliding.

Type
Articles
Information
Geological Magazine , Volume 99 , Issue 3 , June 1962 , pp. 193 - 207
Copyright
Copyright © Cambridge University Press 1962

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References

REFERENCES

Gidon, P., 1951 a. Feuille de Chambéry au 80.000e. Carte Géol. Fr. Bull., 48 (1950), 147–161.Google Scholar
Gidon, P., 1951 b. Structure géologique du groupe “Mont de Joigny, Mont Granier” en Grande-Chartreuse septentrionale (Savoie). Comptes Rendus Acad. Sci. Fr., 233, 809–811.Google Scholar
Gidon, P., 1952. Les chaines jurassiennes du Mont Tournier et du Mont du Chat. Carte Géol. Fr. Bull., 49 (1951), 163–177.Google Scholar
Gidon, P., 1954. Le front subalpin septentrional. Lab. Géol. Univ. Grenoble Trav., 32, 49–56.Google Scholar
Kelling, G., 1961. The stratigraphy and structure of the Ordovician rocks of the Rhinns of Galloway. Quart. J. geol. Soc. Lond., 117, 37–75.Google Scholar
Lindström., M., 1960. Methods of differentiating tectonic regimes. Internat. Geol. Congr. Proc., 18, 347–352.Google Scholar
Pfannenstiel, M., 1958. Faltung unter Gesteinsverlust, dargestellt and Beispielen aus dem Kettenjura. Zeitschr. Deutsch. Geol. Gesellsch., 110, 9.Google Scholar
Prokopovich, N., 1952. The origin of stylolites. J. sediment. Petrol., 22, 212–220.Google Scholar
Rigby, J. K., 1953. Some transverse stylolites. J. sediment. Petrol., 23, 265–271.CrossRefGoogle Scholar
Sander, B., 1948. Einführung in die Gefügekunde der geologischen Körper. I. Allgemeine Gefügekunde und Arbeiten im Bereich Handstück bis Profil. Vienna.CrossRefGoogle Scholar
Williams, A., 1958. Oblique-slip faults and rotated stress systems. Geol. Mag., 95, 207–218.CrossRefGoogle Scholar
Williams, A., 1959. A structural history of the Girvan district, S. W. Ayrshire. Trans. roy. Soc., Edinb., 63, 629–667.Google Scholar