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Description
  • 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.
  • 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 spraší a spraším podobných sedimentů střední a jižní Moravy byly studovány z hlediska metody exoskopie kombinované s metodou studia těžkých minerálů. Výsledkem studia bylo určení provenienční oblasti daných sedimentů. Sprašové sedimenty z vybraných lokalit byly pomocí asociací těžkých minerálů rozděleny do čtyřech hlavních skupin. Materiál první skupiny pochází ze zvětralin západně ležících magmatických a metamorfovaných hornin. Materiál ostatních skupin pochází převážně z severně, severozápadně či severovýchodně ležících sedimentárních hornin. Prachová frakce obsahuje minimum zrn kde by byly zaznamenány mikrostruktury charakterizující ten určitý druh transportu, proto pro determinaci jejich zdrojových hornin musela být použita další metodika. (cs)
Title
  • Exoscopy of Moravian eolian sediments
  • Exoscopy of Moravian eolian sediments (en)
  • Exoskopie eolických sedimentů na Moravě (cs)
skos:prefLabel
  • Exoscopy of Moravian eolian sediments
  • Exoscopy of Moravian eolian sediments (en)
  • Exoskopie eolických sedimentů na Moravě (cs)
skos:notation
  • RIV/67985831:_____/04:00103920!RIV/2005/AV0/A09005/N
http://linked.open.../vavai/riv/strany
  • 177;182
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(AV0Z3013912)
http://linked.open...iv/cisloPeriodika
  • 3
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 563620
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/04:00103920
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • exoscopy; heavy minerals; loess (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [3CCBEAAD8BF0]
http://linked.open...i/riv/nazevZdroje
  • Bulletin of Geosciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 79
http://linked.open...iv/tvurceVysledku
  • Lisá, Lenka
http://linked.open...n/vavai/riv/zamer
issn
  • 1214-1119
number of pages
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