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Tertiary tectono-metamorphic evolution of the European margin during Alpine collison: example of the Leventina Nappe (Central Alps, Switzerland)

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Academic year: 2021

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Figure

table 1 correlates structures and deformation phases of the Leventina Nappe with those of the simano Nappe in the hang-ing wall to the east and the west accordhang-ing to the relative age of deformation, as well as the metamorphic conditions deduced by
Fig. 3. Field pictures and microphotographs of structural features observed in the Leventina Gneisses
table 1. correlation of Mesoscopic structural elements in the subpenninic Domain of the central Alps of switzerland (Leventina Nappe and simano Nappe) and inferred ages after becker (1993), Gebauer (1996), Hurford et al
Fig. 4. Map of s2 foliations in the study area. 257 field measurements of s2 were averaged through inverse distance weighted spatial averaging with the program spheristat for Windows (Pangaea scientific, brookville, Ontario)
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