Foraminiferal biostratigraphy of the Miocene deposits from the Busko (Młyny) PIG-1 and Kazimierza Wielka (Donosy) PIG-1 boreholes (northern part of the Carpathian Foredeep)
Journal Title: Biuletyn Państwowego Instytutu Geologicznego - Year 2015, Vol 461, Issue 461
Abstract
Micropaleontological study of Miocene deposits from the Busko (Młyny) PIG-1 and Kazimierza Wielka (Donosy) PIG-1 boreholes, located in the northern part of the Carpathian Foredeep, has allowed taxonomic and biostratigraphic characteristics of foraminiferal assemblages. The samples were taken from clay and clay-marly interbeds in sub-evaporitic, evaporitic and supra-evaporitc complexes. In the Busko (Młyny) PIG-1 borehole, five foraminiferal assemblages have been defined (Z.b.I–Z.s.V), corresponding with the following foraminiferal zones: [i]Orbulina suturalis[/i]/ [i]Praeorbulina[/i] – Z.b.I (Moravian substage of the Early Badenian), [i]Neobulimina longa[/i] – Z.b.II; [i]Velapertina indigena[/i] – Z.b.III, [i]Hanzawaia crassiseptata[/i] – Z.b.IV (Kosovian substage of the Late Badenian) and [i]Anomalinoides dividens [/i]– Z.b.V (Volhynian substage of the Early Sarmatian). In the Kazimierza Wielka (Donosy) PIG-1 borehole, two foraminiferal assemblages have been identified (Z.b.I and Z.s.II), correlated with following foraminiferal zones [i]Velapertina indigena[/i] – Z.b.I (Kosovian substage of the Late Badenian) and [i]Varidentella sarmatica[/i] – Z.s.II (Volhynian substage of the Early Sarmatian). The third assemblage (Z.s.III), because of poor preservation of foraminifers has been attributed to the Sarmatian stage in general. Lateral replacement of planktonic and benthonic foraminiferal assemblages confirms a significant facies variability of the Late Badenian deposits that accumulated in the northern margin of marine basin in the Carpathian Foredeep.
Authors and Affiliations
Jolanta PARUCH-KULCZYCKA
Keywords
Related Articles
- EP ID EP63567
- DOI -
- Views 45
- Downloads 0
VARIANT SELECTION OF WETLAND AREAS RESTORATION IN THE KAMPINOS NATIONAL PARK BASED ON HYDRODYNAMIC MODELLING RESEARCH
Modelling research was conducted in the hydrogeological valley unit, where the Kampinos National Park (KNP) is situated. The aim of the calculations was to provide a prognosis for the evaluation of proposed restoration v...
DYNAMIC OF THE HYDRAULIC HEADS IN THE YEARS 1961–1981 IN THE OSTROWO–GOPŁO CANAL
The aim of the project was to define relations between the dynamics of groundwater levels and rainfall in the system Ostrowo–Goplo Canal. The point of departure for this study was groundwater levels data and the sum of a...
ZAWARTOŚĆ RTĘCI W GLEBACH ORAZ OSADACH RZECZNYCH I STRUMIENIOWYCH W REGIONIE ŚLĄSKO-KRAKOWSKIM
W artykule przedstawiono ocenę zawartości i zróżnicowanie przestrzenne występowania rtęci w glebach oraz osadach rzecznych i strumieniowych regionu śląsko-krakowskiego, ze szczególnym uwzględnieniem otoczenia hałd i zakł...
THE DISCHARGE ANALYSIS BASED ON LIMNIMETRIC MONITORING: SPRING POD WYSOKIM DZIAŁEM, PIENINY KLIPPEN BELT
The paper describes the results of 9-year stationary monitoring of the spring Pod Wysokim Działem, located in the Pieniny Mts. The monitoring of water level with application of automatic limnimeters and periodically meas...
Główne przezroczyste minerały ciężkie w osadach czwartorzędowych Polski
W pracy zaprezentowano skład przezroczystych minerałów ciężkich znajdujących się w czwartorzędowych osadach spoistych (gliny zwałowe, mułki, lessy) oraz osadach sypkich (fluwioglacjalnych, rzecznych, wydmowych). Podano p...