Stratigraphy and facies development of the upper Tithonian-lower Berriasian Niżniów Formation along the Dnister River (Western Ukraine)

• Autorzy: Gutowski J. , Popadyuk I. V. , Olszewska B.
• Języki publikacji: EN

Abstrakty

EN

The deposits of the Niżniów Formation, exposed around Niżniów, mainly on the banks of Dnister River, accumulated in the most proximal, marginal position of the latest Jurassic-earliest Cretaceous epicontinental basin on the SW margin of the East European Platform. The Niżniów Formation directly onlaps a Palaeozoic substrate and consists of transgressive cliff-derived conglomerates, and sandstones and marls which pass laterally into shallow marine carbonates: mainly biomicrites, oncomicrites, and pelmicrites with an abundant benthic fauna dominated by nerineid gastropods. The thickness of the formation in the area studied ranges from 0 to more than 20 metres and was controlled bymorphology of the pre-transgression substrate (mainly built of Devonian clastic rocks), synsedimentary fault tectonics and pre-mid-Albian erosion. The age of the Niżniów Formation can be determined, on the evidence of benthic foraminifers encountered in thin sections, as most probably late Tithonian-early Berriasian.

Słowa kluczowe

EN

Tithonian-Berriasian Ukraine; transgression; stratigraphy; facies development

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2005
• Tom: Vol. 49, No. 1
• Strony: 45--52
• Opis fizyczny: Bibliogr. 20 poz., rys.

Twórcy

autor

Gutowski J.

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

autor

Popadyuk I. V.

• Ukrainian State Geological Research Institute, Lviv Branch, Mickiewicz Square 8, U-79601 Lviv, Ukraine

autor

Olszewska B.

• Polish Geological Institute, Carpathian Branch, Skrzatów 1, PL-31-560 Kraków, Poland

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