Initiation and development of the Pennine Basal Thrust (Swiss Alps): A structural and geochronological study of an exhumed megathrust

Abstract The Pennine Basal Thrust (PBT) is an exhumed megathrust developed during continental collision from late Eocene to Miocene. To trace its evolution, five samples, with indications for up to three microstructurally diachronous white-mica generations, were investigated by laser in-situ and step-heating 40 Ar– 39 Ar dating. Three deformation-related crystallization ages can be distinguished: (1) D 1 , characterized in the PBT hanging wall by an S 1 foliation defined by white mica + chloritoid, began at or before ∼38.0 Ma; (2) D 2 formed a pervasive S 2 cleavage and synchronous white-mica rich veins dated at ∼27 Ma; (3) D 3 produced an S 3 crenulation cleavage and chlorite + white-mica veins dated at ∼23 Ma. Older ages of ∼96 Ma (footwall) and ∼115 Ma (hanging wall) are interpreted as minimum ages for the detrital component. Finally, discrete faulting produced fault gouge, with an illite K–Ar age of ∼19 Ma. A simplified back-restored reconstruction provides a tectonic context for the dated structures. In this framework, D 1 occurred during middle to late Eocene tectonic accretion. After late Eocene initiation of continental collision, D 2 reflects Oligocene top-to-NW shearing, with both in- and out-of-sequence thrusting. D 3 then developed from 23 to 19 Ma during the progressive deactivation of the PBT.