@ARTICLE{Bogutskiy_Andriy_Conditions_2000,
 author={Bogutskiy, Andriy and Łanczont, Maria and Racinowski, Roman},
 volume={Vol. 17},
 journal={Studia Quaternaria},
 pages={3-17},
 howpublished={online},
 year={2000},
 publisher={Committee for Quaternary Research PAS},
 publisher={Institute of Geological Sciences PAS},
 abstract={Large exposure near the brick-field in Halie represents one of the most complete loess sequences in the Ukrainian Carpathian F orcland, which i I lustrates a progress of events covering a considerable part of the Middle Pleistocene and the whole Upper Pleistocene. The most important of these arc: the Luck soil corresponding to the soil from the Zbójno lnicrglacial in Polish profiles and Dornnitz Interglacial (1~0 stage 9) in West European profiles, bottom part of the Upper Pleistocene (Dnieper= Odranian = Saalian I) loesses, which arc extremely thick and stratigraphically divided into units of lower rank. and well developed soil complexes - Korshov and Horok hov. Investigations of the Korshov soil arc a basis to discuss at least two stages/phases ofpedogcncsis development during the last but one interglacial (Lublinian = Trcenian: 1~0 stage 7). The Horokhov paleosol is connected with the Ecmian Interglacial. The Dubno and Rovno soils occur within the poorly developed Vistulian loesses: the Rovno soil is a cultural layer.},
 type={Article},
 title={Conditions and course of sedimentation of the Middle and Upper Pleistocene loesses in the Halie profile(NWUkraine)},
 URL={http://www.czasopisma.pan.pl/Content/121925/PDF-MASTER/3_STUDIA_VOL_17_2000_Bogutskiy_Conditions.pdf},
 keywords={loesses, Upper Pleistocene, paleogeograpahy, Ukrainian Carpathian Foreland},
}