Abstract
Research on high-resolution tomography, three-dimensional anisotropy modelled from shear-wave splitting and P-residual analysis, as well as receiver function interpretation, are in progress with the aim to image the crust and uppermost mantle velocities in the Bohemian Massif. Structure of the deep lithosphere and location of boundaries of mantle domains will be compared with tectonics of the crust and limits of terranes derived by geologic and palaeomagnetic methods.
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