| Attributes | Values |
|---|
| rdf:type
| |
| Description
| - Vrt Menin byl vrtán 20 km k jihovýchodu z Brna. Spodnikambrická Acritarcha byla zjištěna v hloubce 475 - 477,5 m. Sedimenty pod touto metráží jsou přiřazovány také ke kambriu. Zhledicka petrologie jsou studovanné horniny monotonní. V CL mikroskopu byly pozorovány tři druhy křemene, zonální K- živec a plagioklasy. Minerální kompozice sedimentárních hornin ukazuje na to, že horniny byly dotovány muskovit-biotitickou žulou. Ze sedimentologického hlediska byly studované vzorky pravděpodobně pod silným vlivem říčního prostředí. Stopy po lezení organismů pomohly identifikovat mořské prostředí v těchto klastikách. (cs)
- Měnín borehole is situated 20 km to the south-east from Brno. The Lower Cambrian mikrofossils of Acritarcha genus have been found at the depth of 475 - 477,5 m. The sediments below the layer with Acritarcha presence are considered to be Cambrian of age. Petrological character of studied sediments is monotonous. Three types of quartz, zoned K-feldspar, plagioclase were observed in CL microscope. The mineral composition of the sediments and internal fabric of individual minerals indicates that the muscovite-biotite bearing granites could be seen as potential source rock. Studied deposits were highly probably deposited under strong influence of fluvial environment (braid river).Trace fossils helped in tracing the marine influences in deposition. The deposition environment was in the studied case affected by the marine action in its marginal or distal areas (interdistributary area, braid delta ?), probably during reduced fluvial input or channel shifting. Shallow marine condition can be assumed.
- Měnín borehole is situated 20 km to the south-east from Brno. The Lower Cambrian mikrofossils of Acritarcha genus have been found at the depth of 475 - 477,5 m. The sediments below the layer with Acritarcha presence are considered to be Cambrian of age. Petrological character of studied sediments is monotonous. Three types of quartz, zoned K-feldspar, plagioclase were observed in CL microscope. The mineral composition of the sediments and internal fabric of individual minerals indicates that the muscovite-biotite bearing granites could be seen as potential source rock. Studied deposits were highly probably deposited under strong influence of fluvial environment (braid river).Trace fossils helped in tracing the marine influences in deposition. The deposition environment was in the studied case affected by the marine action in its marginal or distal areas (interdistributary area, braid delta ?), probably during reduced fluvial input or channel shifting. Shallow marine condition can be assumed. (en)
|
| Title
| - Litologický a sedimentologický vývoj kambriských sedimentů ve vrtu Měnin-1 (cs)
- Lithological and sedimentological Evolution of Cambrian in the Měnín ? 1 borehole
- Lithological and sedimentological Evolution of Cambrian in the Měnín ? 1 borehole (en)
|
| skos:prefLabel
| - Litologický a sedimentologický vývoj kambriských sedimentů ve vrtu Měnin-1 (cs)
- Lithological and sedimentological Evolution of Cambrian in the Měnín ? 1 borehole
- Lithological and sedimentological Evolution of Cambrian in the Měnín ? 1 borehole (en)
|
| skos:notation
| - RIV/00025798:_____/02:00000325!RIV07-MZP-00025798
|
| http://linked.open.../vavai/riv/strany
| |
| http://linked.open...avai/riv/aktivita
| |
| http://linked.open...avai/riv/aktivity
| |
| 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/00025798:_____/02:00000325
|
| http://linked.open...riv/jazykVysledku
| |
| http://linked.open.../riv/klicovaSlova
| - Southern Moravia,Cambrian age, sedimentology, petrology (en)
|
| http://linked.open.../riv/klicoveSlovo
| |
| http://linked.open...odStatuVydavatele
| |
| http://linked.open...ontrolniKodProRIV
| |
| http://linked.open...i/riv/nazevZdroje
| |
| http://linked.open...in/vavai/riv/obor
| |
| http://linked.open...ichTvurcuVysledku
| |
| http://linked.open...cetTvurcuVysledku
| |
| http://linked.open...UplatneniVysledku
| |
| http://linked.open...v/svazekPeriodika
| |
| http://linked.open...iv/tvurceVysledku
| - Leichmann, Jaromír
- Mikuláš, Radek
- Nehyba, Slavomír
- Gilíková, Helena
|
| 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)