Sedimentation and tectonics of the Upper Proterozoic-Lower Cambrian deposits of the Southern Małopolska Massif (SE Poland)

Moryc, W; Łydka, K.

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Tytuł artykułu

Sedimentation and tectonics of the Upper Proterozoic-Lower Cambrian deposits of the Southern Małopolska Massif (SE Poland)

Autorzy

Moryc W , Łydka K.

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Abstrakty

In the latest Precambrian and Early Cambrian, turbidity currents and cohesive flows transported pebbles, sand and mud into a deep water in south-east Poland, this sediment probably being sourced from Gondwana. Abundant detrital albite grains suggest volcanism during sedimentation. Pebbles in conglomerate interbeds are polymict and include rock fragments showing greenschist facies regional metamorphism in the source area. The Precambrian surface in the marginal part of the Carpathians lies at 2000-5000 m b.s.l., whereas farther south, around Kuźmina it reaches 7000 m. Still farther south (Krosno-Sanok-Baligród) geophysical evidence suggests it lies at about 17-20 km depth.

Słowa kluczowe

Carpathian Foreland Tarnów-Przemyśl area Precambrian sedimentation lithology basement tectonics clastic rock

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2000

Tom

Vol. 44, Nr 1

Strony

47--58

Opis fizyczny

fot., tab., wykr., bibliogr. 72 poz.

Twórcy

autor

Moryc W

Geological Office "Geonafta", Lubicz 25, PL-31-503 Kraków, Poland

autor

Łydka K.

Institute of Geochemistry, Mineralogy and Petrography, Uniiversity of Warsaw, Żwirki i Wigury 93,P L-02-089,Warszawa, Poland

Bibliografia

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