| Attributes | Values |
|---|
| rdf:type
| |
| Description
| - Paleomagnetické studie na detailně ovzorkovaném 27m mocném jursko-křídovém hraničním profilu na ostrově Nordvik (záliv Anabar, moře Laptěvů) umožnily poprvé provést korelace jednotlivých magnetozón s chronami M20n-M17r v boreální oblasti. Uvnitř zóny kladné polarity odpovídající chroně M20n, byl zjištěn krátký úsek záporné polarity pravděpodobně odpovídající Kysuca subzoně (M20n.1r). Další krátký úsek záporné polarity, stanovený uvnitř další kladné zóny M19n koreluje se subzonou Brodno (M19n. 1r). Stejná posloupnost kladně a záporně polarizovaných magnetozón byla dříve zjištěna v hraničním souvrství jura-křída v tethydní oblasti v Bosso Valley (Itálie), v Brodnu (Slovensko) a v Puerto Eskaňo (Španělsko). Bylo zjištěno, že hranice jura-křída odpovídá souvrství s výskytem druhu Craspedites taimyrensis ve svrchním Volgianu. (cs)
- As a result of detailed sampling and paleomagnetic study of the 27-m-thick section of Jurassic-Cretaceous boundary beds in the Nordvik Peninsula (Anabar Bay, Lapte Sea), a succession of M- zones correlative with chrons M20n-M17r is established for the first time in the Boreal deposits. Inside the normal polarity zone corresponding to Chron M20n, a thin interval of reversed polarity, presumably an equivalent of the Kysuca Subzone (M20n.1r),is discovered. The other thin interval of reversed polarity established within the next normalpolarity zone (M19n) is correlated with the Brodno subzone (M19n.1r). The same succession of normal and reversed polarity zones has been discovered recently in the Jurassic-Cretaceous boundary beds of the Tethyan sections: in the Bosso Valley (Italy), at the Brodno (Slovak Republic) and Puerto Escańo (Spain) sites. Correlation of successions established lead us to conclusion, that the Jurassic-Cretaceous boundary corresponds in the Panboreal Superrealm*** *
- As a result of detailed sampling and paleomagnetic study of the 27-m-thick section of Jurassic-Cretaceous boundary beds in the Nordvik Peninsula (Anabar Bay, Lapte Sea), a succession of M- zones correlative with chrons M20n-M17r is established for the first time in the Boreal deposits. Inside the normal polarity zone corresponding to Chron M20n, a thin interval of reversed polarity, presumably an equivalent of the Kysuca Subzone (M20n.1r),is discovered. The other thin interval of reversed polarity established within the next normalpolarity zone (M19n) is correlated with the Brodno subzone (M19n.1r). The same succession of normal and reversed polarity zones has been discovered recently in the Jurassic-Cretaceous boundary beds of the Tethyan sections: in the Bosso Valley (Italy), at the Brodno (Slovak Republic) and Puerto Escańo (Spain) sites. Correlation of successions established lead us to conclusion, that the Jurassic-Cretaceous boundary corresponds in the Panboreal Superrealm*** * (en)
|
| Title
| - Boreal- Tethyan Correlation of the Jurassic – Cretaceous Boundary Interval by Magneto- and Biostratigraphy
- Korelace mezi boreální a tethydní oblastí jursko-křídového hraničního profilu na základě magnetostratigrafie a biostratigrafie (cs)
- Boreal- Tethyan Correlation of the Jurassic – Cretaceous Boundary Interval by Magneto- and Biostratigraphy (en)
|
| skos:prefLabel
| - Boreal- Tethyan Correlation of the Jurassic – Cretaceous Boundary Interval by Magneto- and Biostratigraphy
- Korelace mezi boreální a tethydní oblastí jursko-křídového hraničního profilu na základě magnetostratigrafie a biostratigrafie (cs)
- Boreal- Tethyan Correlation of the Jurassic – Cretaceous Boundary Interval by Magneto- and Biostratigraphy (en)
|
| skos:notation
| - RIV/67985831:_____/07:00086856!RIV08-AV0-67985831
|
| http://linked.open.../vavai/riv/strany
| |
| http://linked.open...avai/riv/aktivita
| |
| http://linked.open...avai/riv/aktivity
| - P(GA205/06/0842), P(GA205/07/1365), Z(AV0Z30130516), Z(MSM0021620855)
|
| http://linked.open...iv/cisloPeriodika
| |
| http://linked.open...vai/riv/dodaniDat
| |
| http://linked.open...aciTvurceVysledku
| |
| http://linked.open.../riv/druhVysledku
| |
| http://linked.open...iv/duvernostUdaju
| |
| http://linked.open...titaPredkladatele
| |
| http://linked.open...dnocenehoVysledku
| |
| http://linked.open...ai/riv/idVysledku
| - RIV/67985831:_____/07:00086856
|
| http://linked.open...riv/jazykVysledku
| |
| http://linked.open.../riv/klicovaSlova
| - Jurassic- Cretaceous boundary; Boreal and Tethyan deposits; magnetostratigraphy; biostratigraphy; Northern Siberia (en)
|
| http://linked.open.../riv/klicoveSlovo
| |
| http://linked.open...odStatuVydavatele
| |
| http://linked.open...ontrolniKodProRIV
| |
| http://linked.open...i/riv/nazevZdroje
| - Stratigraphy and Geological Correlation
|
| 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...v/svazekPeriodika
| |
| http://linked.open...iv/tvurceVysledku
| - Košťák, M.
- Mazuch, M.
- Pruner, Petr
- Zakharov, V. A.
- Chadima, Martin
- Šlechta, Stanislav
- Houša, Václav
- Rogov, M. A.
|
| http://linked.open...n/vavai/riv/zamer
| |
| issn
| |
| number of pages
| |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)