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- W2058780871 abstract "The present study aims to investigate how the tectonic compression due to Africa–Eurasia convergence is transmitted up to Central Europe via a thermo-mechanical model, in which a high-resolution rheological analysis is performed in the surroundings of the Alpine domain and the predicted heterogeneous lithosphere strength is accounted for to reproduce the surface strain pattern. Our rheological analysis reveals a strongly heterogeneous lithosphere strength that is characterised by steep strength gradients across the Periadriatic Lineament and the occurrence of non-competent crustal layers located below the Northern Alps, where the upper crust controls the total lithosphere strength. When the predicted lithosphere strength is included within a spherical thin sheet model to investigate the propagation of the tectonic compression due to Africa–Eurasia convergence toward Central Europe, our analysis supports the hypothesis that the N–S compressive stress dominates the gravitational body forces in the Southern Alps up to the Periadriatic Lineament. This lineament defines an abrupt transition from the strong mantle belonging to the Adriatic lithosphere to the softer mantle below the Eastern Alps, which is mechanically decoupled from the relatively stronger upper crust, thus preventing stress transmission toward the surface. Thus, in the Eastern Alps, the transmitted S–N compression would remain lower than the E–W extensional stress induced at crustal levels by the body gravitational forces associated with thick crustal layers." @default.
- W2058780871 created "2016-06-24" @default.
- W2058780871 creator A5009555783 @default.
- W2058780871 creator A5027409893 @default.
- W2058780871 date "2014-09-01" @default.
- W2058780871 modified "2023-09-30" @default.
- W2058780871 title "3D mechanical structure of the lithosphere below the Alps and the role of gravitational body forces in the regional present-day stress field" @default.
- W2058780871 cites W1536356084 @default.
- W2058780871 cites W1560528922 @default.
- W2058780871 cites W1597733412 @default.
- W2058780871 cites W1633951790 @default.
- W2058780871 cites W1825505754 @default.
- W2058780871 cites W1838841355 @default.
- W2058780871 cites W1965105111 @default.
- W2058780871 cites W1968051836 @default.
- W2058780871 cites W1969599221 @default.
- W2058780871 cites W1969684613 @default.
- W2058780871 cites W1971828111 @default.
- W2058780871 cites W1972023992 @default.
- W2058780871 cites W1975991751 @default.
- W2058780871 cites W1976796651 @default.
- W2058780871 cites W1977946147 @default.
- W2058780871 cites W1982208033 @default.
- W2058780871 cites W1982800365 @default.
- W2058780871 cites W1986738852 @default.
- W2058780871 cites W1987388713 @default.
- W2058780871 cites W1989447145 @default.
- W2058780871 cites W1992096365 @default.
- W2058780871 cites W1992933809 @default.
- W2058780871 cites W1999675312 @default.
- W2058780871 cites W1999720315 @default.
- W2058780871 cites W1999778350 @default.
- W2058780871 cites W2000033909 @default.
- W2058780871 cites W2002247122 @default.
- W2058780871 cites W2003121585 @default.
- W2058780871 cites W2006766138 @default.
- W2058780871 cites W2009558532 @default.
- W2058780871 cites W2010269787 @default.
- W2058780871 cites W2010497141 @default.
- W2058780871 cites W2010806432 @default.
- W2058780871 cites W2014395164 @default.
- W2058780871 cites W2014896099 @default.
- W2058780871 cites W2015351629 @default.
- W2058780871 cites W2015419721 @default.
- W2058780871 cites W2018314772 @default.
- W2058780871 cites W2020491401 @default.
- W2058780871 cites W2022857521 @default.
- W2058780871 cites W2023648341 @default.
- W2058780871 cites W2026814260 @default.
- W2058780871 cites W2028375840 @default.
- W2058780871 cites W2032964793 @default.
- W2058780871 cites W2035413994 @default.
- W2058780871 cites W2037881181 @default.
- W2058780871 cites W2037992388 @default.
- W2058780871 cites W2040356201 @default.
- W2058780871 cites W2041696552 @default.
- W2058780871 cites W2044345773 @default.
- W2058780871 cites W2044752290 @default.
- W2058780871 cites W2048742589 @default.
- W2058780871 cites W2049950848 @default.
- W2058780871 cites W2053830600 @default.
- W2058780871 cites W2054802878 @default.
- W2058780871 cites W2061189564 @default.
- W2058780871 cites W2061360284 @default.
- W2058780871 cites W2061656081 @default.
- W2058780871 cites W2062000567 @default.
- W2058780871 cites W2062421980 @default.
- W2058780871 cites W2064559765 @default.
- W2058780871 cites W2065146837 @default.
- W2058780871 cites W2067454886 @default.
- W2058780871 cites W2069591775 @default.
- W2058780871 cites W2078815957 @default.
- W2058780871 cites W2083665727 @default.
- W2058780871 cites W2084364546 @default.
- W2058780871 cites W2084796812 @default.
- W2058780871 cites W2086835258 @default.
- W2058780871 cites W2088585909 @default.
- W2058780871 cites W2094249051 @default.
- W2058780871 cites W2107855077 @default.
- W2058780871 cites W2107901522 @default.
- W2058780871 cites W2112633201 @default.
- W2058780871 cites W2117804105 @default.
- W2058780871 cites W2121038255 @default.
- W2058780871 cites W2121440949 @default.
- W2058780871 cites W2125238892 @default.
- W2058780871 cites W2128721289 @default.
- W2058780871 cites W2138416791 @default.
- W2058780871 cites W2143829803 @default.
- W2058780871 cites W2155090707 @default.
- W2058780871 cites W2156701839 @default.
- W2058780871 cites W2166465211 @default.
- W2058780871 cites W2949229931 @default.
- W2058780871 cites W3043177896 @default.
- W2058780871 doi "https://doi.org/10.1016/j.tecto.2014.04.038" @default.
- W2058780871 hasPublicationYear "2014" @default.
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