This project investigates the crust and upper mantle along a north-south oriented, about 350 km long profile from around the town of Ringkøbing in western Jutland to south of Hamburg in northwestern Germany, with a focus on teleseismic receiver functions and seismic tomography. A number of tectonic processes have affected the crust and uppermost mantle beneath southern Scandinavia and northern Germany: Precambrian crustal accretion in southern Baltica, Caledonian collision between Baltica and Avalonia along the Tornquist Suture Zone (TSZ), followed by Variscan collision and formation of the North German and the Norwegian-Danish basins, and more recent magmatic activity to the south. This study is particularly focused on the closure of the Tornquist Sea and the Caledonian collision between Baltica and Avalonia. A total of 29 stations, provided by GFZ and the University of Aarhus, were deployed between autumn 2010 and summer 2012, of which 25 form the main profile, and 4 are positioned in an off-line location. Waveform data are available from the GEOFON data centre, under network code ZW, and are available under CC-BY 4.0 license according to GIPP-rules.
* Description is taken from seismic metadata, and may not match the preferred title for citations.
Hejrani, B.; Balling, N.; Jacobsen, B. H.; Tilmann, F. (2015). Upper-mantle P- and S-wave velocities across the Northern Tornquist Zone from traveltime tomography. Geophysical Journal International, 203, 1, p. 437-458. doi:10.1093/gji/ggv291
Kind, R.; Sodoudi, F.; Yuan, X.; Shomali, H.; Roberts, R.; Gee, D.; Eken, T.; Bianchi, M.; Tilmann, F.; Balling, N.; Jacobsen, B. H.; Kumar, P.; Geissler, W.H. (2013). Scandinavia: A former Tibet?. Geochemistry Geophysics Geosystems (G3), 14, 10, p. 4479-4487. doi:10.1002/ggge.20251