engleski

Processes controlling eocene mid-latitude larger foraminifera accumulations : modelling of the stratigraphic architecture of a fore-arc basin (Podhale basin, Poland)

A model for the stratigraphic architecture of the Eocene strata of the Podhale basin has been developed. Generally, the sedimentation of the basin was controlled by eustatic sea-level changes and fore-arc spreading in a convergente regime related to the infratatric subduction. Our sequence stratigraphic data correlated well with the corresponding implications from a recently published composite oxygen isotope record for the Cenozoic.

eocene; Central Western Carpathians; Podhale basin; fore-arc basin; sequence stratigraphy; larger foraminifers

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