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| rdf:type
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| Description
| - Silurian effusive basalts and volcaniclastics compose the Svatý Jan volcanic center, which is located in the northwestern limb of the Prague synform, where three major volcanic phases have been recognized. The opening mode, which controlled both dikes, corresponds to a dextral transtensional regime, as deduced from the AMS K1 axis. They may have been opened during several magmatic stages related to different injections during late Wenlock to mid-Ludlow times. During the Late Devonian the nappes emplacement that pre-dates this direction was probably associated with the sinistral closure of the Rheic Ocean, in agreement with post-Givetian folding and faulting, which deformed the synform infi ll and closed the Barrandian marine sedimentary cycle.
- Silurian effusive basalts and volcaniclastics compose the Svatý Jan volcanic center, which is located in the northwestern limb of the Prague synform, where three major volcanic phases have been recognized. The opening mode, which controlled both dikes, corresponds to a dextral transtensional regime, as deduced from the AMS K1 axis. They may have been opened during several magmatic stages related to different injections during late Wenlock to mid-Ludlow times. During the Late Devonian the nappes emplacement that pre-dates this direction was probably associated with the sinistral closure of the Rheic Ocean, in agreement with post-Givetian folding and faulting, which deformed the synform infi ll and closed the Barrandian marine sedimentary cycle. (en)
- Výzkumné práce zahrnovaly bazalty a vulkanoklastické horniny v blízkosti centra Svatý Jan, který je lokalizován na severozápadě Pražské pánve. Na základě studia magnetických vlastností (anizotropie, magnetické susceptibility, magnetomineralogických a paleomagnetických parametrů) byl zjištěn systém otevření jednotlivých lávových proudů, které odpovídají svrchnímu Wenloku až střednímu Ludlowu. Současně byly potvrzeny předpoklady, že ve svrchním devonu se již uzavíral Rheický oceán a tím byl ukončen sedimentární cyklus Barrandienu. (cs)
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| Title
| - Structural evolution of the Prague synform (Czech Republic) during Silurian times: An AMS, rock magnetism, and palomagnetic study of the Svatý Jan pod Skalou dikes. Consequences for the nappes emplacement
- Strukturní vývoj Pražské pánve (Česká republika) během siluru: anizotropie magnetické susceptibility, magnetomineralogie a paleomagnetické studie žil ve Svatém Janu pod Skalou. Důsledky pro příkrovovou stavbu (cs)
- Structural evolution of the Prague synform (Czech Republic) during Silurian times: An AMS, rock magnetism, and palomagnetic study of the Svatý Jan pod Skalou dikes. Consequences for the nappes emplacement (en)
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| skos:prefLabel
| - Structural evolution of the Prague synform (Czech Republic) during Silurian times: An AMS, rock magnetism, and palomagnetic study of the Svatý Jan pod Skalou dikes. Consequences for the nappes emplacement
- Strukturní vývoj Pražské pánve (Česká republika) během siluru: anizotropie magnetické susceptibility, magnetomineralogie a paleomagnetické studie žil ve Svatém Janu pod Skalou. Důsledky pro příkrovovou stavbu (cs)
- Structural evolution of the Prague synform (Czech Republic) during Silurian times: An AMS, rock magnetism, and palomagnetic study of the Svatý Jan pod Skalou dikes. Consequences for the nappes emplacement (en)
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| skos:notation
| - RIV/67985831:_____/07:00090675!RIV08-AV0-67985831
|
| 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
| - P(IAA3013406), Z(AV0Z30130516)
|
| 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
| |
| http://linked.open...ai/riv/idVysledku
| - RIV/67985831:_____/07:00090675
|
| http://linked.open...riv/jazykVysledku
| |
| http://linked.open.../riv/klicovaSlova
| - magnetic properies; dikes; Variscan orogen; stress; rheic; AMS; magnetization; Variscan orogen (en)
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| http://linked.open.../riv/klicoveSlovo
| |
| http://linked.open...ontrolniKodProRIV
| |
| http://linked.open...i/riv/mistoVydani
| |
| http://linked.open...vEdiceCisloSvazku
| - Special papers- Geological Society of America, 423
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| http://linked.open...i/riv/nazevZdroje
| - Evolution of the Rheic Ocean : from Avalonian-Cadomian active margin to Alleghenian-Variscan collision
|
| http://linked.open...in/vavai/riv/obor
| |
| http://linked.open...ichTvurcuVysledku
| |
| http://linked.open...cetTvurcuVysledku
| |
| http://linked.open...vavai/riv/projekt
| |
| http://linked.open...UplatneniVysledku
| |
| http://linked.open...iv/tvurceVysledku
| - Pruner, Petr
- Štorch, Petr
- Chadima, Martin
- Aifa, T.
|
| http://linked.open...n/vavai/riv/zamer
| |
| number of pages
| |
| http://purl.org/ne...btex#hasPublisher
| |
| https://schema.org/isbn
| |
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