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PORTAIL D'INFORMATION GÉOGRAPHIQUE

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  • Orogenetic geosynclinal and magmatic cycles are controlled by worldwide lateral motions. To the end of herzynian cycle are in the area of Werdau-Hainichen trough and permocarboniferous basins in the northwestern part of CSSR eight or ten changes
  • of tectonic course. In times of dilation and while changes of tectonic direction intruded Hercynian magmatic bodies. (HL).
  • to shields, the type of the shelf crust exists, as illustrated by Central and Western Europe. The geosynclinal, tectogenetic and magmatic development conditioned by the drift in this shelf crust region is described in outline. The geotectonic events