COMPLEX TECTONICS OF THE GONDWANA-LAURUSSIA PLATE BOUNDARY ZONE – INTERFERENCE OF RELATIVE PLATE MOTION AND LATERAL ESCAPING LITHOSPHERIC BLOCKS (Invited Presentation)
Early Devonian collision of the Armorican Spur with Laurussia initiated the Acadian / Early Variscan orogeny in Western Europe coeval with transpressional tectonics in the Northern Appalachians. Late Devonian plate tectonic reorganization caused NW directed lateral escape of a lithospheric block in Brittany coeval with ongoing NE directed subduction-accretion tectonics in Central Europe. Subsequent W-directed collision of decoupled huge E-Peri-Gondwana lithospheric block with already accreted crust of the western shelf resulted in pervasive transpressional tectonics of the W-European Variscides and resulted in the Late Variscan Ibero-Armorican Arc.
Latest Carboniferous detachment of the Gondwana plate south of Europe terminates the Variscan orogeny. Ongoing collision of Gondwana and Laurussia occurred exclusively at the plate boundary segment of Western Gondwana and North America, finally shaping the fold and thrust belts of the Southern Appalachians and the Ouachita-Sonora-Marathon belt.
References: Kroner and Romer, 2013, Gondwana Research, 24; Kroner et al., 2016, Tectonophysics, 681; Stephan et al., 2018, Geological Magazine; Willner et al., 2018, Tectonophysics