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Secondary ionization mass spectrometry (SIMS) U-Pb dating of zircons from the Å reskutan Nappe in the central part of the Seve Nappe Complex of western central Jämtland provides new constraints on the timing of granulite-amphibolite-facies metamorphism and tectonic stacking of the nappe during the Caledonian orogeny. Peak-temperature metamorphism in garnet migmatites is constrained to c. 442 + 4 Ma, very similar to the ages of leucogranites at 442 + 3 and 441 + 4 Ma. Within a migmatitic amphibolite, felsic segregations crystallized at 436 + 2 Ma. Pegmatites, cross-cutting the dominant Caledonian foliation in the Nappe, yield 428 + 4 and 430 + 3 Ma ages. The detrital zircon cores in the migmatites and leucogranites provide evidence of Late Palaeoproterozoic, Mesoproterozoic to Early Neoproterozoic source terranes for the metasedimentary rocks. The formation of the ductile and hot Seve migmatites, with their inverted metamorphism and thinning towards the hinterland, can be explained by an extrusion model in which the allochthon stayed ductile for a period of at least 10 million years during cooling from peaktemperature metamorphism early in the Silurian.In our model, Baltica-Laurentia collision occurred in the Late Ordovician-earliest Silurian, with emplacement of the nappes far on to the Baltoscandian platform during the Silurian and early Devonian, Scandian Orogeny lasting until c. 390 Ma.