
WITHIN THE
CENTRAL EUROPEAN PERMOCARBONIFEROUS INTERMONTANE BASINS
AND THEIR BASEMENT –
LUSATIA –
(VENTS)
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During the Late
Carboniferous - Early Permian, the northern margin of the Bohemian Massif was
characterized by the formation of tectonically controlled basins and by strong
volcanic activity. Volcanic and subvolcanic products of the predominantly calc-alkaline
magmatism are intercalated within intermontane basins, like the
The VENTS program which
will have a duration of 6 years involves project leaders from three Polish
universities (
First Assessment Field Work Shop in Bolków, June 2006
Second Assessment Field Work Shop in Turnov, June 2007
Third Assessment Field Work Shop in Freiberg, May 2008
Fourth Assessment Field Work Shop west of Kraków, Poland, May 2009
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