By Derek Blundell, Roy Freeman, Stephan Mueller

A Continent printed provides the findings of the ecu Geotraverse (EGT)--a targeted learn of the tectonic evolution of the continent of Europe and the 1st complete move component of the continental lithosphere. The venture produced maps and geologic profiles, alongside a 250 kilometer broad swath stretching 4600 kilometers from Scandinavia to the Mediterranean, which shape a 3 dimensional photo of the constitution, homes, and composition of the continental lithosphere of Europe in an atlas structure. the various info that contain the maps also are awarded on an compact disc (ROM). The dialogue quantity, the maps, and a ebook containing gravity, electrical, and magnetic box facts represent the whole boxed set. The paperback dialogue quantity can also be on hand individually.

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Teissyre Tornquist Zone 2000 FW EUROPE'S LITHOSPHERE - SEISMIC STRUCTURE 41 about halfway between shotpoints FC and FB it traverses the Gothian granites. Still further south the Teisseyre Tornquist zone is crossed north of shotpoint FW which is located on the Caledonian orogen of eastern Germany. Detailed two-dimensional interpretations of the crustal P-wave data giving similar results were presented by Guggisberg (1986), Lund (1990), Stangl (1990) and Guggisberg et al. (1991) for the complete profile, while Clowes et al.

A spacing of about 300 km for the explosions was chosen so that the structure of the crust could be determined sufficiently well in order to ascertain its influence on those seismic phases which penetrated the upper mantle. All seismic wideangle reflection and refraction data were compiled by Hauser et al. (1990). The main profile (F in Figure 3-1) lies between the North Cape in Norway, with the most northerly shotpoints FI and FH offshore in the Barents Sea, and southern Sweden, with the southernmost shotpoints FB off the coast and FW onshore in eastern Germany to bridge the Baltic Sea.

ANSORGE, D. BLUNDELL AND ST. 1 SEISMIC METHODS FOR EXPLORING THE CRUST AND UPPER MANTLE OF EUROPE Methods for exploring the Earth's interior which follow the passage of seismic waves through the ground are adapted according to the scale on which the Earth is viewed. The resolution of the seismic method utilised governs the clarity of the image of the Earth's structure and the extent of information on physical properties. In general, the deeper the investigation, the lower the resolution and the more blurred is the image.

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