HEAVY MINERALS IN THE KEY LATE PLEISTOCENE LOESS-PALAEOSOL SECTION AT KOLODIIV (EAST CARPATHIAN FORELAND, UKRAINE)

dc.contributor.authorRacinowski R.
dc.date.accessioned2026-08-10T12:18:45Z
dc.date.issued2007
dc.description.abstractSuccessions of loess and other deposits in the Kolodiiv profile, formed during the Eemian Interglacial and Vistulian Glacial (OIS 5-2), are characterized using the results of heavy mineral analysis. Weathered local carbonate rocks and fluvial deposits (Wartanian Glacial, OIS 6) are used for comparison. It was found that the content of minerals derived from weathered and redeposited Carpathian Flysch increases from bottom to top of the profile. The entire loess succession accumulated under similar lithodynamic conditions and the palaeosols are of similar character.
dc.identifierhttps://elibrary.ru/item.asp?id=28027973
dc.identifier.citationGeological Quarterly, 2007, 51, 2, 185-188
dc.identifier.issn1641-7291
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/53952
dc.subjectHEAVY MINERALS
dc.subjectLATE PLEISTOCENE
dc.subjectLOESS
dc.subjectPALAEOSOLS
dc.subjectUKRAINE
dc.subjectPleistocene
dc.subject.ageCenozoic::Quaternary::Pleistocene
dc.subject.ageКайнозой::Четвертичная::Плейстоцен
dc.titleHEAVY MINERALS IN THE KEY LATE PLEISTOCENE LOESS-PALAEOSOL SECTION AT KOLODIIV (EAST CARPATHIAN FORELAND, UKRAINE)
dc.typeСтатья

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