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Statements

Subject Item
n2:RIV%2F00216224%3A14330%2F05%3A00013385%21RIV10-MSM-14330___
rdf:type
n11:Vysledek skos:Concept
dcterms:description
The Prague Synform (Teplá-Barrandian region, Bohemian Massif) represents remains of Ordovician to middle Devonian sedimentary units folded into a large synclinorium. The Tachlovice Fault (Svoboda & Prantl 1948) is one of major longitudinal faults in the Prague Synform located in the NW limb of the synform. This fault at least fourty kilometers in length strikes in WSWENE direction and dips in 45 SE and could be traced from the surroundings of Beroun through Prague to Běchovice. The stratigraphic separation diagram for the Tachlovice Fault was constructed using detailed geological maps (1: 25 000). Based on the interpretation of SSD, we obtained an exact argument for the flat-and-ramp geometry of the Tachlovice Fault. The opposite sense of tectonic transport along this fault top-to-the SE (%22normal%22 faulting) was documented by small-scale structures (small ramps, S-C structures etc.). The Prague Synform (Teplá-Barrandian region, Bohemian Massif) represents remains of Ordovician to middle Devonian sedimentary units folded into a large synclinorium. The Tachlovice Fault (Svoboda & Prantl 1948) is one of major longitudinal faults in the Prague Synform located in the NW limb of the synform. This fault at least fourty kilometers in length strikes in WSWENE direction and dips in 45 SE and could be traced from the surroundings of Beroun through Prague to Běchovice. The stratigraphic separation diagram for the Tachlovice Fault was constructed using detailed geological maps (1: 25 000). Based on the interpretation of SSD, we obtained an exact argument for the flat-and-ramp geometry of the Tachlovice Fault. The opposite sense of tectonic transport along this fault top-to-the SE (%22normal%22 faulting) was documented by small-scale structures (small ramps, S-C structures etc.).
dcterms:title
The Tachlovice Fault - a well-documented thrust in the Barrandian The Tachlovice Fault - a well-documented thrust in the Barrandian
skos:prefLabel
The Tachlovice Fault - a well-documented thrust in the Barrandian The Tachlovice Fault - a well-documented thrust in the Barrandian
skos:notation
RIV/00216224:14330/05:00013385!RIV10-MSM-14330___
n3:aktivita
n5:P n5:Z
n3:aktivity
P(IAA3013406), Z(MSM0021622412)
n3:cisloPeriodika
1
n3:dodaniDat
n10:2010
n3:domaciTvurceVysledku
n4:3032744 n4:5789567 n4:9765476
n3:druhVysledku
n18:J
n3:duvernostUdaju
n16:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
545948
n3:idVysledku
RIV/00216224:14330/05:00013385
n3:jazykVysledku
n8:eng
n3:klicovaSlova
Prague Synform; Barrandian; Bohemian Massif; Tachlovice Fault; thrust; stratigraphic separation diagram
n3:klicoveSlovo
n6:stratigraphic%20separation%20diagram n6:Tachlovice%20Fault n6:thrust n6:Barrandian n6:Prague%20Synform n6:Bohemian%20Massif
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[7DCEE83BBDC0]
n3:nazevZdroje
Geolines
n3:obor
n7:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
3
n3:projekt
n19:IAA3013406
n3:rokUplatneniVysledku
n10:2005
n3:svazekPeriodika
Vol. 19
n3:tvurceVysledku
Ferbar, Petr Janečka, Jiří Melichar, Rostislav
n3:zamer
n15:MSM0021622412
s:issn
1210-9606
s:numberOfPages
2
n17:organizacniJednotka
14330