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The complex tectonic history of Central Europe (Fig. 1a) reflects the break-up of a Neoproterozoic supercontinet(s) (Rodinia/Pannotia) to form the fragment Baltica and the subsequent growth of continental Europe beginning with the Caledonian orogeny. Caledonian and younger Variscan orogenesis involved accretion of Laurentian and Gondwanan terranes to the riftet margin of Baltica. (East European craton,...
Prawidłowe odwzorowanie rozmieszczenia oraz zachowania się szczelin w utworach łupkowych, przy wiernym opisie własności geomechanicznego ośrodka geologicznego, wymaga wykonania analiz i interpretacji na danych sejsmicznych z uwzględnieniem anizotropii. Azymutalne i wieloskładnikowe pomiary pionowego profilowania sejsmicznego PPS 3C są najbardziej użytecznym narzędziem, spośród stosowanych metod sejsmicznych,...
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