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Attributes

Fernschub
Fernschub
poussée à distance
spinta a distanza
Grossmassstäbliche Abscherung des Sedimentkeils im Alpenvorland.
Large-scale decoupling of the frontal-Alpine sedimentary wedge.
2023-07-03T12:51:06.3233630Z
67017
https://www.termdat.bk.admin.ch/entry/67017
ENSI, Sedimentologische und stratigraphische Aspekte des ‘Braunen Doggers‘, 2017-01, S. 16, Abs. 4.3.1 ([Internet, 2023-06-05](https://www.ensi.ch/de/wp-content/uploads/sites/2/2017/03/ENSI_33-462_Brauner-Dogger_Final.pdf))
V. Rime et al., Tectonics of the Neuchâtel Jura Mountains, in: Swiss Journal of Geosciences, 112/2019, p. 563 ([Internet, 2023-06-05](https://sjg.springeropen.com/articles/10.1007/s00015-019-00349-y))
swisstopo, Atlas géologique de la Suisse, 1143 Le Locle, 2020, p. 114 ([Internet, 2023-06-05](https://prod-swishop-s3.s3.eu-central-1.amazonaws.com/product-documents/GA25-ERL-172.pdf))
QWiki, Geologia del massiccio del Giura ([Internet, 2023-06-05](https://it.frwiki.wiki/wiki/G%C3%A9ologie_du_massif_du_Jura))
Le principe d’une poussée à distance («Fernschub») a été retenu pour la construction des coupes géologiques. Ce modèle implique que les contraintes nécessaires pour déformer les strates sédimentaires entre le Bassin molassique et le front du Jura plissé au niveau de Besançon sont transmises à travers l’ensemble du prisme critique [...].
Nel complesso, i dati sismici hanno confermato il modello della "spinta a distanza" per la formazione del Giura.
This deformation is explained by the “Fernschub” theory (...) linking emplacement of the External Crystalline Massifs to the initiation of the main décollement.
EXP: Ursache für die Jurafaltung
swisstopo, Landesgeologie, 2007
swisstopo, Landesgeologie, 2007
CNRS, P. Jordan, Evidence for large-scale decoupling, 1992, p. 2
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