. "Exoscopy of Moravian eolian sediments" . "Z(AV0Z3013912)" . "1214-1119" . . . . . . "Loess and related eolian sediment samples from selected localities in southern and central Moravia were studied using exoscopy combined with the study of heavy minerals, toward determining the provenance of their source rocks. The loess sediments from selected localities were divided into four sub-groups based on the characteristics of their heavy mineral fractions. Material of the first sub-group was deflated solely from the weathering horizons of nearby magmatic or metamorphic rocks to the west. The material of the other loess sub-areas was predominantly deflated from sedimentary rocks to the west, southwest, and northwest of their present sites. The sediments with a predominant fine-grained fraction contain exceedingly minimum quartz grains lacking distinctive transport evidence. Nonetheless, it has been possible to use other methods in determining their source rocks." . "CZ - \u010Cesk\u00E1 republika" . "Exoscopy of Moravian eolian sediments" . . "3" . . "[3CCBEAAD8BF0]" . "RIV/67985831:_____/04:00103920" . "79" . "Exoscopy of Moravian eolian sediments"@en . . "Exoscopy of Moravian eolian sediments"@en . "exoscopy; heavy minerals; loess"@en . "Exoskopie eolick\u00FDch sediment\u016F na Morav\u011B"@cs . . "Bulletin of Geosciences" . . "6"^^ . "Exoskopie eolick\u00FDch sediment\u016F na Morav\u011B"@cs . . "177;182" . "563620" . . "Lis\u00E1, Lenka" . "RIV/67985831:_____/04:00103920!RIV/2005/AV0/A09005/N" . "1"^^ . "Loess and related eolian sediment samples from selected localities in southern and central Moravia were studied using exoscopy combined with the study of heavy minerals, toward determining the provenance of their source rocks. The loess sediments from selected localities were divided into four sub-groups based on the characteristics of their heavy mineral fractions. Material of the first sub-group was deflated solely from the weathering horizons of nearby magmatic or metamorphic rocks to the west. The material of the other loess sub-areas was predominantly deflated from sedimentary rocks to the west, southwest, and northwest of their present sites. The sediments with a predominant fine-grained fraction contain exceedingly minimum quartz grains lacking distinctive transport evidence. Nonetheless, it has been possible to use other methods in determining their source rocks."@en . . . "Vzorky spra\u0161\u00ED a spra\u0161\u00EDm podobn\u00FDch sediment\u016F st\u0159edn\u00ED a ji\u017En\u00ED Moravy byly studov\u00E1ny z hlediska metody exoskopie kombinovan\u00E9 s metodou studia t\u011B\u017Ek\u00FDch miner\u00E1l\u016F. V\u00FDsledkem studia bylo ur\u010Den\u00ED provenien\u010Dn\u00ED oblasti dan\u00FDch sediment\u016F. Spra\u0161ov\u00E9 sedimenty z vybran\u00FDch lokalit byly pomoc\u00ED asociac\u00ED t\u011B\u017Ek\u00FDch miner\u00E1l\u016F rozd\u011Bleny do \u010Dty\u0159ech hlavn\u00EDch skupin. Materi\u00E1l prvn\u00ED skupiny poch\u00E1z\u00ED ze zv\u011Btralin z\u00E1padn\u011B le\u017E\u00EDc\u00EDch magmatick\u00FDch a metamorfovan\u00FDch hornin. Materi\u00E1l ostatn\u00EDch skupin poch\u00E1z\u00ED p\u0159ev\u00E1\u017En\u011B z severn\u011B, severoz\u00E1padn\u011B \u010Di severov\u00FDchodn\u011B le\u017E\u00EDc\u00EDch sediment\u00E1rn\u00EDch hornin. Prachov\u00E1 frakce obsahuje minimum zrn kde by byly zaznamen\u00E1ny mikrostruktury charakterizuj\u00EDc\u00ED ten ur\u010Dit\u00FD druh transportu, proto pro determinaci jejich zdrojov\u00FDch hornin musela b\u00FDt pou\u017Eita dal\u0161\u00ED metodika."@cs . "1"^^ .