La faille de Merens dans les Pyrenees ariegeoises
- 1 January 1958
- journal article
- Published by EDP Sciences in BSGF - Earth Sciences Bulletin
- Vol. S6-VIII (7) , 793-796
- https://doi.org/10.2113/gssgfbull.s6-viii.7.793
Abstract
The southern border fault (Merens fault) of the Aston massif in the Pyrenees of Ariege, France, corresponds to a southward thrusting of this massif over a zone of sedimentary formations attributed to the Canaveilles series (probably Cambrian). On the south, these sediments are in fault contact with the Hospitalet gneiss massif (Pinet fault); farther east, toward Merens, they form the cover of the Hospitalet massif.Keywords
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