A Structural Study of the Southern End of the French Jura
- 1 June 1962
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 99 (3), 193-207
- https://doi.org/10.1017/s0016756800058246
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.Keywords
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