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rdf:type
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Description
| - Moravické souvrství sestává z pestrá asociace různých turbitidních facií, které lze interpretovat jako výplně hlubokomořských kanálů střídající se s usazeninami hlubokomořských vějířů. Jedna z asociací se vyznačuje střídáním laminitů a hrubších složek (facie D a C) střídajících se s ještě hrubozrnnějšími sedimenty - písky a konglomeráty (facie B a C). Společenstva fosilních stop této asociace sestávají z ichnodruhu Dictyodora liebeana, občas doprovázeného ichnodruhy Chondrites isp. a Phycospon incertum. Druhá asociace bližší klasickému flyši hlubokomořských vějířů obsahuje ichnofosilie Diplocraterion isp., Rhizocoralium isp., Dictyodora liebeana, Cosmorhaphe isp. a Paleodictyon isp (cs)
- The Moravice Formation provides a facies association of extremely diverse turbidites interpreted as channel-fill cycles alternating with overbank sediments deposited in inner- to middle-fan environments. One aassociation is comprised of thick succesions of laminite and beds of facies D and C, alternating with sandstone lenses that range in thickness from several tens to about one hundred meters, and are composed of facies C and B. The second facies association was deposited as sandstone lobe and lobe-fringe sediments in outer-fan environment. The ichnoassemblages of the first facies association are dominated by Dictyodora liebeana, which is accompanied by Chondrites isp. and Phycospon incertum,. The second facies association occurs at the margins of greywacke lenses and contains Diplocraterion isp., Rhizocoralium isp., Dictyodora liebeana, Cosmorhaphe isp. and Paleodictyon isp.
- The Moravice Formation provides a facies association of extremely diverse turbidites interpreted as channel-fill cycles alternating with overbank sediments deposited in inner- to middle-fan environments. One aassociation is comprised of thick succesions of laminite and beds of facies D and C, alternating with sandstone lenses that range in thickness from several tens to about one hundred meters, and are composed of facies C and B. The second facies association was deposited as sandstone lobe and lobe-fringe sediments in outer-fan environment. The ichnoassemblages of the first facies association are dominated by Dictyodora liebeana, which is accompanied by Chondrites isp. and Phycospon incertum,. The second facies association occurs at the margins of greywacke lenses and contains Diplocraterion isp., Rhizocoralium isp., Dictyodora liebeana, Cosmorhaphe isp. and Paleodictyon isp. (en)
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Title
| - Trace fossils of the Moravice Formation from the southern Nízký Jeseník Mts. (Lower Carboniferous, Culm facies; Moravia, Czech Republic)
- Ichnofosilie moravického souvrství z jižní části Nízkého Jeseníku (spodní karbon, kulmská facie; Morava) (cs)
- Trace fossils of the Moravice Formation from the southern Nízký Jeseník Mts. (Lower Carboniferous, Culm facies; Moravia, Czech Republic) (en)
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skos:prefLabel
| - Trace fossils of the Moravice Formation from the southern Nízký Jeseník Mts. (Lower Carboniferous, Culm facies; Moravia, Czech Republic)
- Ichnofosilie moravického souvrství z jižní části Nízkého Jeseníku (spodní karbon, kulmská facie; Morava) (cs)
- Trace fossils of the Moravice Formation from the southern Nízký Jeseník Mts. (Lower Carboniferous, Culm facies; Moravia, Czech Republic) (en)
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skos:notation
| - RIV/67985831:_____/04:00103968!RIV/2005/GA0/A09005/N
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http://linked.open.../vavai/riv/strany
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/67985831:_____/04:00103968
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - ichnofossils;Lower Carboniferous;Culm facies (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Mikuláš, Radek
- Bábek, O.
- Lehotský, T.
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issn
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number of pages
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