Dajki klastyczne i brekcje sejsmotektoniczne w utworach permu basenu Nachodu (Sudety Środkowe)

• Autorzy: Wojewoda J. , Burliga S.

Warianty tytułu

EN

Clastic dikes and seismotectonic breccia in Permian deposits of the Nachod Basin (Middle Sudetes)

• Języki publikacji: PL

Abstrakty

EN

Clastic dikes have been evidenced in Permian conglomerates occurring near Kudowa Zdrój in the Nachod Basin, the Sudetes, NE Bohemian Massif. The lithology of the dikes is the same as that of the polimictic conglomerate hosting them; they only differ in textural characteristics. The spatial orientation of the dikes points out to their genetic relationship with a nearby fault that, in a map view, separates Permian and Cretaceous formations. The dikes must have intruded after tectonic rotation of conglomerate beds on the fault to a position similar to the present one and they represent record of post-diagenetic seismotectonic events.

Słowa kluczowe

PL

dajki klasycystyczne; brekcje sejsmotektoniczne; perm; basen Nachodu; Sudety

EN

clastic dikes; seismotectonic breccia; Permian; Nachod Basin; Sudetes

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Przegląd Geologiczny
• Rocznik: 2008
• Tom: Vol. 56, nr 9
• Strony: 857--862
• Opis fizyczny: bibliogr. 35 poz., rys.

Twórcy

autor

Wojewoda J.

autor

Burliga S.

• Instytut Nauk Geologicznych, Uniwersytet Wrocławski, pl. Maksa Borna 9, 50-204 Wrocław,

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