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  3. Late stages of continent-continent collision: Timing, kinematic evolution, and exhumation of the Northern rim (Aar Massif) of the Alps

Late stages of continent-continent collision: Timing, kinematic evolution, and exhumation of the Northern rim (Aar Massif) of the Alps

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DOI
10.7892/boris.138324
Publisher DOI
10.1016/j.earscirev.2019.102959
Abstract
The Alpine front’s External Crystalline Massifs represent exhumation of mid-crustal basement during late-stage continent-continent-collision. We unravel the geodynamic evolution of the Northalpine front (Aar Massif) by combining structural and low-T thermochronometric data. A crustal-scale tectonic restoration (Neogene-present) and estimation of associated changes in exhumation rates become possible. The European continental margin experienced multiple switches from horizontal- to vertical- and again to horizontal-dominated tectonics. Early thrust-related inversion of rift basins is followed by a switch to rapid vertical exhumation, with deformation along steep reverse/normal faults. This vertical tectonics related to a positive buoyancy force of the European crust induced by lower crustal delamination of the Aar Massif during an orogenic rollback process of the European lithosphere (~22-20 Ma). Differential rock uplift rates of up to 1.3-1.6 km/Myr resulted, which decreased northwards to 0.1 km/Myr. Reducing buoyancy forces (isostatic compensation) led to a horizontal tectonic style again. Persisting compressional forces induced an orogen-scale strain partitioning with dextral transpressive faults in the south and simultaneous crustal-scale northwest-directed thrusting in the north. ‘En-bloc’ exhumation of the entire Aar Massif in the thrusts’ hanging wall occurred between 13-5 Ma and 5-0 Ma at rates of 0.5-0.9 km/Myr and 0.6-0.8 km/Myr, respectively. It is this late-stage thrusting in combination with surface erosion, which shaped today’s prominent Northalpine front. Switches between horizontal and vertical tectonics might generally be relevant for late continent-continent-collision stages. Here buoyancy forces of non-thinned continental crust entering the subduction zone cause a strong vertical tectonic deformation style instead of classical thrust tectonics.
Date Issued
2020
Publication Type
Article
Subject(s)
500 Science > 550 Earth sciences & geology
Language(s)
en
Author(s)
Herwegh, Marco  
Institut für Geologie  
Berger, Alfons  
Institut für Geologie  
Glotzbach, C.
Wangenheim, C.
Mock, Samuel  
Institut für Geologie  
Wehrens, Philip Chaim  
Institut für Geologie  
Baumberger, Roland  
Institut für Geologie  
Egli, Daniel  
Institut für Geologie  
Kissling, E.
Additional Credits
Institut für Geologie  
Journal
Earth-science reviews
Publisher
Elsevier
ISSN
0012-8252
Access(Rights)
open.access
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