1986
DOI: 10.1016/0191-8141(86)90057-x
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Change of direction of overthrust shear in the Helvetic nappes of western Switzerland

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Cited by 46 publications
(22 citation statements)
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“…5 and 8. Dietrich and Durney, 1986;McClay, 1992). However, in the case of the Dokos and Mandritsa areas, a late-stage passive reorientation of the thrust transport direction towards an extension-related transport direction is fairly obvious in the hanging wall of extensional system, assisted by the displacement on the detachments and associated steep faults (Figs.…”
Section: Deformational Historymentioning
confidence: 96%
“…5 and 8. Dietrich and Durney, 1986;McClay, 1992). However, in the case of the Dokos and Mandritsa areas, a late-stage passive reorientation of the thrust transport direction towards an extension-related transport direction is fairly obvious in the hanging wall of extensional system, assisted by the displacement on the detachments and associated steep faults (Figs.…”
Section: Deformational Historymentioning
confidence: 96%
“…The Alpine realm suffered important N-S contraction in response to Adria-Europe collision in late Eoceneearly Oligocene times (Lacassin 1989;Schmid & Kissling 2000;Dèzes et al 2004). Early Alpine northward to NW-ward thrusting and folding is documented in many places throughout the Alps: in the Helvetic zone (Dietrich & Durney 1986;Ramsay 1989;Wildi & Huggenberger 1993), in the Internal Zones (Caby 1973;Maury & Ricou 1983;Merle & Brun 1984;Merle et al 1989;Platt et al 1989b;Schmid et al 1996;Ceriani & Schmid 2004) and in the Austro-Alpine realm (Froitzheim et al 1994). N-directed thrusting is also known in the Pelvoux realm (Barbier 1956;Desthieux & Vernet 1968;Bartoli et al 1974;Gidon 1979;Gillcrist 1988;Barféty & Gidon 1990;Pêcher et al 1992;Ford 1996;Sue et al 1998;Gidon 1999) but it has been generally confused with Pyrenean-Provence events.…”
Section: Multistage Shortening: a Proposed Tectonic And Geodynamic Scmentioning
confidence: 99%
“…1). Earlier studies provide substantial constraints on the stratigraphy, geometry, and deformation history of the Morcles nappe and its eastern pendant, the Doldenhorn nappe, at a regional scale (badoux 1972;ramsay 1981;ramsay et al 1983;Dietrich & Durney 1986;burkhard & Kerrich 1988;coward & Dietrich 1989;Dietrich & casey 1989;ramsay 1989;Escher et al 1993;Pfiffner 1993;crespo-blanc et al 1995;Kirschner et al 1995;Kirschner et al 1996;burkhard & Goy-Eggenberger 2001;bucher et al 2003;Herwegh & Pfiffner 2005). Detailed studies of the microstructures of deformed marbles from a range of locations along the nappe also exist (schmid et al 1981;Dietrich 1986;Ebert et al 2007a) (Figs.…”
Section: Introductionmentioning
confidence: 99%