Geological section through the lower Paleozoic strata of the Polish part of the Baltic region

• Autorzy: Pokorski J.
• Języki publikacji: EN

Abstrakty

EN

The present-day structural pattern of the Baltic Depression developed due to superimposition of three main deformation phases: syn-Caledonian (after the Silurian), syn-Variscan (at the end of Carboniferous and beginning of Permian) and syn-Alpine (latest Mesozoic or earliest Cenozoic). The major restructuring of the area occurred as a result of syn-Variscan deformation that took place in latest Carboniferous and earliest Permian times. Most of the faults developed or became reactivated probably at that time. Syn-Alpine deformation manifested itself relatively weakly, mainly by reactivation of some pre-existing faults.

Słowa kluczowe

EN

Lower Paleozoic; Baltic Region; East European Craton; West European Platform; faults and fault zones; structural elements

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2010
• Tom: Vol. 54, No 2
• Strony: 123--130
• Opis fizyczny: Bibliogr. 17 poz., wykr.

Twórcy

autor

Pokorski J.

• Polish Geological Institute - National Research Institute, Rakowiecka 4, PL-00-975 Warszawa, Poland,

Bibliografia

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