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Statements

Subject Item
n2:RIV%2F61989592%3A15310%2F05%3A00010009%21RIV10-MSM-15310___
rdf:type
skos:Concept n15:Vysledek
dcterms:description
In its early history the polygenetic depression of the Upper Moravia Graben (UMG) evolved in two separated phases: The Karpathian to Badenian phase and Badenian to Pliocene phase. During the former phase, The Olomouc-Prostějov basin was formed, which was directly related to marine sedimentation in the Carpathian foredeep. During the latter phase a strongly segmented depositional area developed in the UMG, comprising fluvial and lacustrine sedimentation which persisted in the area up to the Quaternary. Both the depressions evolved in direct response to the Styrian movements of the allochtonous unit of the Outer Western Carpathians over the eastern margin of the Bohemian Massif. In its early history the polygenetic depression of the Upper Moravia Graben (UMG) evolved in two separated phases: The Karpathian to Badenian phase and Badenian to Pliocene phase. During the former phase, The Olomouc-Prostějov basin was formed, which was directly related to marine sedimentation in the Carpathian foredeep. During the latter phase a strongly segmented depositional area developed in the UMG, comprising fluvial and lacustrine sedimentation which persisted in the area up to the Quaternary. Both the depressions evolved in direct response to the Styrian movements of the allochtonous unit of the Outer Western Carpathians over the eastern margin of the Bohemian Massif. In its early history the polygenetic depression of the Upper Moravia Graben (UMG) evolved in two separated phases: The Karpathian to Badenian phase and Badenian to Pliocene phase. During the former phase, The Olomouc-Prostějov basin was formed, which was directly related to marine sedimentation in the Carpathian foredeep. During the latter phase a strongly segmented depositional area developed in the UMG, comprising fluvial and lacustrine sedimentation which persisted in the area up to the Quaternary. Both the depressions evolved in direct response to the Styrian movements of the allochtonous unit of the Outer Western Carpathians over the eastern margin of the Bohemian Massif.
dcterms:title
Poznámky ke geologickému vývoji severozápadní části Hornomoravského úvalu Poznámky ke geologickému vývoji severozápadní části Hornomoravského úvalu Remarks to the geological development of the north-western of the Upper Moravia Graben
skos:prefLabel
Poznámky ke geologickému vývoji severozápadní části Hornomoravského úvalu Poznámky ke geologickému vývoji severozápadní části Hornomoravského úvalu Remarks to the geological development of the north-western of the Upper Moravia Graben
skos:notation
RIV/61989592:15310/05:00010009!RIV10-MSM-15310___
n3:aktivita
n17:S
n3:aktivity
S
n3:cisloPeriodika
1
n3:dodaniDat
n11:2010
n3:domaciTvurceVysledku
n9:5173620
n3:druhVysledku
n4:J
n3:duvernostUdaju
n8:S
n3:entitaPredkladatele
n13:predkladatel
n3:idSjednocenehoVysledku
537494
n3:idVysledku
RIV/61989592:15310/05:00010009
n3:jazykVysledku
n16:cze
n3:klicovaSlova
Upper Moravia Graben; Lower Badenian; Pliocene; Styrian movements
n3:klicoveSlovo
n10:Pliocene n10:Styrian%20movements n10:Upper%20Moravia%20Graben n10:Lower%20Badenian
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[CD08CF80FC2D]
n3:nazevZdroje
Geologické výzkumy na Moravě a ve Slezsku
n3:obor
n12:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
1
n3:rokUplatneniVysledku
n11:2005
n3:svazekPeriodika
12
n3:tvurceVysledku
Zapletal, Jan
s:issn
1212-6209
s:numberOfPages
3
n14:organizacniJednotka
15310