About: Tectonic setting of the Ohře/Eger Graben between the central part of the České středohoří Mts. and the Most Basin, a regional study

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About: Tectonic setting of the Ohře/Eger Graben between the central part of the České středohoří Mts. and the Most Basin, a regional study Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	The paper is focused on tectonic setting in the SW part of the České středohoří Mts.(a section of the Ohře/Eger Graben/Rift. The SE marginal graben fault zone is traced in detail. The fault zone is as a horst, with the graben fill being structured into rhomboidal blocks. The fault movements are classified into those older than 36 Ma, younger than 24 Ma and younger than 16 Ma. The faults are compared with the earlier-defined paleostress fields. Fault reversals were detected on several faults. The role of crystalline basement ridges during the graben formation was identified. Two areas with distinct tectonic and geological development were defined within the Graben. The Saxothuringian Teplá-Barrandian terrane boundary was found to be less important for graben formation during the Cenozoic. This disagrees with simplified riftogenic model of the Ohře/Eger Graben. The ”Litoměřice Deep-seated Fault“, representing a first-order terrane boundary, could not be confirmed in the post-Paleozoic rocks. The paper is focused on tectonic setting in the SW part of the České středohoří Mts.(a section of the Ohře/Eger Graben/Rift. The SE marginal graben fault zone is traced in detail. The fault zone is as a horst, with the graben fill being structured into rhomboidal blocks. The fault movements are classified into those older than 36 Ma, younger than 24 Ma and younger than 16 Ma. The faults are compared with the earlier-defined paleostress fields. Fault reversals were detected on several faults. The role of crystalline basement ridges during the graben formation was identified. Two areas with distinct tectonic and geological development were defined within the Graben. The Saxothuringian Teplá-Barrandian terrane boundary was found to be less important for graben formation during the Cenozoic. This disagrees with simplified riftogenic model of the Ohře/Eger Graben. The ”Litoměřice Deep-seated Fault“, representing a first-order terrane boundary, could not be confirmed in the post-Paleozoic rocks. (en)
Title	Tectonic setting of the Ohře/Eger Graben between the central part of the České středohoří Mts. and the Most Basin, a regional study Tectonic setting of the Ohře/Eger Graben between the central part of the České středohoří Mts. and the Most Basin, a regional study (en)
skos:prefLabel	Tectonic setting of the Ohře/Eger Graben between the central part of the České středohoří Mts. and the Most Basin, a regional study Tectonic setting of the Ohře/Eger Graben between the central part of the České středohoří Mts. and the Most Basin, a regional study (en)
skos:notation	RIV/00025798:_____/10:00000340!RIV11-GA0-00025798
http://linked.open...avai/riv/aktivita	I P Z
http://linked.open...avai/riv/aktivity	I, P(GA205/07/0691), P(IAA300460602), Z(AV0Z30130516), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika	3
http://linked.open...vai/riv/dodaniDat	2011
http://linked.open...aciTvurceVysledku	Valečka, Jaroslav
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Česká geologická služba
http://linked.open...dnocenehoVysledku	292121
http://linked.open...ai/riv/idVysledku	RIV/00025798:_____/10:00000340
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	surface-detected faults, timing of tectonic activity, Ohře/EgerGraben/Rift, Bohemian Cretaceous Basin, České středohoří Volcanic Complex,Most Basin, Cenozoic (en)
http://linked.open.../riv/klicoveSlovo	Ohře/EgerGraben/Rift surface-detected faults timing of tectonic activity Bohemian Cretaceous Basin Cenozoic České středohoří Volcanic Complex Most Basin
http://linked.open...odStatuVydavatele	CZ - Česká republika
http://linked.open...ontrolniKodProRIV	[562B8CBE3B92]
http://linked.open...i/riv/nazevZdroje	Journal of Geosciences
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	1 (xsd:int)
http://linked.open...cetTvurcuVysledku	2 (xsd:int)
http://linked.open...vavai/riv/projekt	Geothermal resources, their limits and a sustainable development: Benešov-Ústí aquifer system Upper-crustal model of the Ohře Rift and its vicinity.
http://linked.open...UplatneniVysledku	2010
http://linked.open...v/svazekPeriodika	55
http://linked.open...iv/tvurceVysledku	Valečka, Jaroslav Cajz, Vladimír
http://linked.open...ain/vavai/riv/wos	000286342100005
http://linked.open...n/vavai/riv/zamer	Zemský systém v průsečíku geologických procesů, vývoje života, klimatických a antropogenních vlivů Geosciences for the Society of the 21st Century: from regional research to geological hazards and global changes.
issn	1802-6222
number of pages	15 (xsd:int)
is http://linked.open...avai/riv/vysledek of	Tectonic setting of the Ohře/Eger Graben between the central part of the České středohoří Mts. and the Most Basin, a regional study

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