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• W2029130717 abstract "In the Leventina valley of southern Switzerland a mylonite zone marks the boundary between Leventina and Simano nappe. Quartz textures and deformation microstructures are used to obtain information about the deformation conditions and kinematics in the mylonite zone. The c-axis patterns give evidence for a non-coaxial finite strain with a high scatter of the constructed shear directions. During texture formation the temperature conditions were in the range of 400–630°C. Structural elements observed in the Leventina-Simano nappe boundary area are integrated into the well-established regional deformation history of the Lepontine dome. On the basis of the kinematics and metamorphic conditions, the last non-brittle increment of the progressive deformation that caused the crystallographic preferred orientation in the quartz tectonites is assigned to the late second to third regional deformation phase. Under brittle to brittle-plastic conditions the mylonite zone was reactivated with a top-to-the-WNW shearing direction. This reactivation is possibly kinematically connected to other major orogen-parallel oriented extensional structures formed in the Miocene, like the Simplon and the Brenner shear zone and fault. Apatite fission track ages (~3.7–10 Ma) across the nappe boundary are similar to the regional data range, but show a negative age-altitude trend. The fission track data combined with structural and kinematic data indicate that there was no considerable amount of vertical displacement along the Leventina- Simano nappe boundary during or after Mid-Miocene. For the negative age-elevation relationship, interplay between exhumation and landscape evolution is suggested." @default.
• W2029130717 created "2016-06-24" @default.
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• W2029130717 date "2004-08-01" @default.
• W2029130717 modified "2023-10-14" @default.
• W2029130717 title "Deformation at the Leventina-Simano nappe boundary, Central Alps, Switzerland" @default.
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• W2029130717 doi "https://doi.org/10.1007/s00015-004-1121-4" @default.
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