By Derek Blundell, Roy Freeman, Stephan Mueller
A Continent printed provides the findings of the ecu Geotraverse (EGT)--a particular examine of the tectonic evolution of the continent of Europe and the 1st finished go component to 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 photograph of the constitution, houses, and composition of the continental lithosphere of Europe in an atlas structure. a few of the facts that contain the maps also are provided on an compact disc (ROM). The dialogue quantity, the maps, and a book containing gravity, electrical, and magnetic box facts represent the whole boxed set. The paperback dialogue quantity can also be to be had individually.
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Extra info for A Continent Revealed: The European Geotraverse
9 Ga when Proterozoic Europe was situated next to North America, and when the two continents shared a continuous active margin. After the Cadomian orogeny, deep rifted sedimentary basins developed across those parts of Proterozoic Europe which by then had become a part of Gondwana. During the Late Ordovician, they experienced, like neighbouring regions of Gondwana, a major glaciation, the 'Saharan' glaciation. Meanwhile, a wide ocean, the so-called Tornquist Sea', was opening between the ice-covered relics and the northward drifting and anticlockwise rotating Baltica, Figure 2-2.
The northern and oldest leg of the triple junction, the Laurentia-Baltica suture, is more difficult to trace because not only has there been large-scale post-collisional shortening, but also later strike-slip movements, and finally crustal extension and rifting, have been superimposed. 8 THE ENGLISH-NORTH GERMAN-POLISH CALEDONIDES The English-North German-Polish Caledonides stretched from southern Ireland, Wales and England across the central and southern part of the North Sea to northern France, Belgium, Holland, Northern Germany and Poland (Figure 2-4).
This part, therefore, is of more noble and ancient origin. None the less, the crustal structure of the Polish Teisseyre Tornquist zone (Guterch et al. 1986) and that of the Sorgenfrei Tornquist zone due south of Scania (BABEL Working Group 1991) appear to show a great many similarities. 13 FINAL BREAKUP OF PANGEA: THE TETHYAN EVOLUTION With the entire assemblage of Gondwana and Laurussia locked together into the single continent of Pangaea, its massive continental entity extended, in Early Jurassic times, virtually from one pole to the other, giving the world a very different configuration of continent and ocean from the present.