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Statements

Subject Item
n2:RIV%2F62156489%3A43410%2F10%3A00165128%21RIV11-MSM-43410___
rdf:type
n7:Vysledek skos:Concept
dcterms:description
The Silezian Beskids (309 -- 1257 m a.s.l.) are border elevation from West Carpathian Range in Central Europe (49,677N; 18,941E). In south-western range in the Czech Republic we sampled rocks on the nine characteristic places. These places were selected according to the exploration of the forest site heterogeneity (SAMEC et al. 2010) (tab. 1). The dating of the investigated rock samples was based on literature survey only (BUDAY et al. 1967; SKUPIEN 2005; STRÁNÍK, ŠVÁBENICOVÁ 2004; GRADSTEIN, OGG 1996; GIBBARD, KOLFSCHOTEN 2004) (tab. 2). We sampled sedimentary rocks dated from Upper Jurassic, Lower and Upper Ctretaceous to Oligocene and Quarter. The chemical analyses of the samples were made by the induced coupled plasma mass spectrometry (ICP-MS) concentrated to biogene plant nutrition-important macroelements (Ca, Mg, K, Na, P, Fe, Al) as well as to rare Earth elements (REE) (tab. 3). An principal component analysis (PCA) was used for comparison of analytical results at aspects of similarities in ma The Silezian Beskids (309 -- 1257 m a.s.l.) are border elevation from West Carpathian Range in Central Europe (49,677N; 18,941E). In south-western range in the Czech Republic we sampled rocks on the nine characteristic places. These places were selected according to the exploration of the forest site heterogeneity (SAMEC et al. 2010) (tab. 1). The dating of the investigated rock samples was based on literature survey only (BUDAY et al. 1967; SKUPIEN 2005; STRÁNÍK, ŠVÁBENICOVÁ 2004; GRADSTEIN, OGG 1996; GIBBARD, KOLFSCHOTEN 2004) (tab. 2). We sampled sedimentary rocks dated from Upper Jurassic, Lower and Upper Ctretaceous to Oligocene and Quarter. The chemical analyses of the samples were made by the induced coupled plasma mass spectrometry (ICP-MS) concentrated to biogene plant nutrition-important macroelements (Ca, Mg, K, Na, P, Fe, Al) as well as to rare Earth elements (REE) (tab. 3). An principal component analysis (PCA) was used for comparison of analytical results at aspects of similarities in ma
dcterms:title
Exploration of element contents in the selected rocks of the Silezian Beskids (Czech Republic) Exploration of element contents in the selected rocks of the Silezian Beskids (Czech Republic)
skos:prefLabel
Exploration of element contents in the selected rocks of the Silezian Beskids (Czech Republic) Exploration of element contents in the selected rocks of the Silezian Beskids (Czech Republic)
skos:notation
RIV/62156489:43410/10:00165128!RIV11-MSM-43410___
n3:aktivita
n6:Z
n3:aktivity
Z(MSM6215648902)
n3:cisloPeriodika
2
n3:dodaniDat
n10:2011
n3:domaciTvurceVysledku
n8:6581242 n8:4733029
n3:druhVysledku
n15:J
n3:duvernostUdaju
n13:S
n3:entitaPredkladatele
n17:predkladatel
n3:idSjednocenehoVysledku
258471
n3:idVysledku
RIV/62156489:43410/10:00165128
n3:jazykVysledku
n16:eng
n3:klicovaSlova
soils; Beskids; source rocks; chemical contents; Czech Republic
n3:klicoveSlovo
n4:soils n4:Beskids n4:source%20rocks n4:Czech%20Republic n4:chemical%20contents
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[118702EB5061]
n3:nazevZdroje
Acta Musei Beskidensis : Acta Mus. Beskid
n3:obor
n9:DB
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n10:2010
n3:svazekPeriodika
2010
n3:tvurceVysledku
Kynický, Jindřich Samec, Pavel Cheng, Xu
n3:zamer
n14:MSM6215648902
s:issn
1803-960X
s:numberOfPages
6
n18:organizacniJednotka
43410