Abstract
The results of stratigraphic and sedimentological investigating Paleocene-Eocene deposits of Metova Formation (Vezhan or «Marmarosh Klippen» nappe, Inner Ukrainian Carpathians) are represented. For these deposits were supplemented the biostratigraphic data, the fi rst time where distinguished zone Acarinina rotundimarginata. According to our micropaleontological and sedimentological analyses the bathymetry of the Paleocene-Eocene sedimentary basin evolved from the deep-water conditions below foraminiferal lysocline up to bathyal envirounments above lysocline.
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Schedule a callMore From: Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine
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