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• W1894402334 startingPage "n/a" @default.
• W1894402334 abstract "[1] This study investigates spatial and temporal interactions of thin- and thick-skinned tectonics in a classical foreland setting located at the front of the Jura fold-and-thrust belt in eastern France. The working area coincides with the intracontinental Rhine-Bresse Transfer Zone and represents the most external front of the deformed Alpine foreland. The investigation combines analyses of largely unpublished and newly available subsurface information with our own structural data, including an exhaustive paleostress analysis and geomorphologic observations. Results are provided in the form of a new tectonic map and a series of regional cross sections through the study area. The Besancon Zone, forming the most external part of the thin-skinned fold-and-thrust belt, encroached onto the Eo-Oligocene Rhine-Bresse Transfer Fault System until early Pliocene times. Thrust propagation was largely controlled by the Late Paleozoic to Paleogene preexisting fault pattern that characterizes the Rhine-Bresse Transfer Zone. Thick-skinned deformation, dominant throughout the Avant-Monts Zone located farther to the west, was associated with compressional to transpressional reactivation of such faults. Overprinting and crosscutting criteria of fault slip data allow distinguishing between systematically fanning maximum horizontal stress axes that define the front of the thin-skinned Jura fold-and-thrust belt and consistently NW–SE directed maximum horizontal stress axes that characterize deformation of the autochthonous cover of the foreland, which is affected by thick-skinned tectonics. Tectonic and geomorphic analyses indicate that thick-skinned tectonics started at a very late stage of foreland deformation (post-early Pliocene). Geomorphic observations imply that deformation between Mesozoic cover and basement is locally still decoupled. However, overprinting relationships and recent seismicity suggest that present-day tectonic activity is thick skinned, which probably reflects ongoing tectonic underplating in the Alpine foreland." @default.
• W1894402334 created "2016-06-24" @default.
• W1894402334 creator A5005989808 @default.
• W1894402334 creator A5014988254 @default.
• W1894402334 creator A5019006329 @default.
• W1894402334 date "2008-10-01" @default.
• W1894402334 modified "2023-10-14" @default.
• W1894402334 title "Interactions between thin- and thick-skinned tectonics at the northwestern front of the Jura fold-and-thrust belt (eastern France)" @default.
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• W1894402334 cites W1964915507 @default.
• W1894402334 cites W1966659122 @default.
• W1894402334 cites W1973187189 @default.
• W1894402334 cites W1973194039 @default.
• W1894402334 cites W1975630028 @default.
• W1894402334 cites W1984033259 @default.
• W1894402334 cites W1985315668 @default.
• W1894402334 cites W1992265640 @default.
• W1894402334 cites W1992472420 @default.
• W1894402334 cites W1995026670 @default.
• W1894402334 cites W1996080599 @default.
• W1894402334 cites W1996828347 @default.
• W1894402334 cites W1997099580 @default.
• W1894402334 cites W1998908091 @default.
• W1894402334 cites W2001226697 @default.
• W1894402334 cites W2003020875 @default.
• W1894402334 cites W2008877113 @default.
• W1894402334 cites W2009079992 @default.
• W1894402334 cites W2011112180 @default.
• W1894402334 cites W2011352448 @default.
• W1894402334 cites W2021632917 @default.
• W1894402334 cites W2031094001 @default.
• W1894402334 cites W2032804613 @default.
• W1894402334 cites W2037900360 @default.
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• W1894402334 cites W2048255596 @default.
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• W1894402334 cites W2055142290 @default.
• W1894402334 cites W2057013620 @default.
• W1894402334 cites W2057913422 @default.
• W1894402334 cites W2058345335 @default.
• W1894402334 cites W2058769256 @default.
• W1894402334 cites W2065190360 @default.
• W1894402334 cites W2073117466 @default.
• W1894402334 cites W2075686130 @default.
• W1894402334 cites W2078444532 @default.
• W1894402334 cites W2078764266 @default.
• W1894402334 cites W2079263965 @default.
• W1894402334 cites W2083678379 @default.
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• W1894402334 cites W2114370832 @default.
• W1894402334 cites W2117323364 @default.
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• W1894402334 cites W2127335932 @default.
• W1894402334 cites W2129493594 @default.
• W1894402334 cites W2135990801 @default.
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• W1894402334 doi "https://doi.org/10.1029/2008tc002282" @default.
• W1894402334 hasPublicationYear "2008" @default.
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