Pregled bibliografske jedinice broj: 41006
Geochemical comparison of stream and overbank sediments : a case study from Žumberak region, Croatia
Geochemical comparison of stream and overbank sediments : a case study from Žumberak region, Croatia // Geologia Croatica, 54 (2001), 1; 119-130 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 41006 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Geochemical comparison of stream and overbank sediments : a case study from Žumberak region, Croatia
Autori
Peh, Zoran ; Miko, Slobodan
Izvornik
Geologia Croatica (1330-030X) 54
(2001), 1;
119-130
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
geochemical mapping; drainage basin approach; stream sediment; overbank sediment; discriminant analysis; Žumberak; Croatia
Sažetak
A geochemical survey of the Žumberak region was carried out within the scope of the research project labelled Basic geochemical map of Croatia carbonate terrains. The purpose of this research was to narrow the focus of investigation to an appropriate sample medium that is area-related, with greater prospects of reflecting the surface lithology as well as traces of possible mineralization and pollution. Discriminant analysis was chosen as a simple strategy to sequester one of the two types of sample material stream sediment or overbank sediment - as more informative on the basis of their geochemical composition. Geochemical comparison between the low- to medium-order stream and overbank sediments was thus grounded on the presupposed statistical contradistinction between the locality-paired sample correlates. Results of discrimination prefer the overbank material mainly on account of its higher natural geochemical variability vis-a-vis otherwise common geochemical semblance. Investigations also demonstrated that in the relatively non-contaminated area it may not be easy to verify the supposed purity-contamination reciprocity between the investigated media since the recent and prehistoric materials were not contrasted as regards their non-lithogene components.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
Citiraj ovu publikaciju:
Časopis indeksira:
- Scopus