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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F03%3A00000493%21RIV07-MZP-00025798
rdf:type
skos:Concept n19:Vysledek
dcterms:description
PGEs enrichments have been recently found in Zn-, Cu-, and Ni-rich black shales in a number of geological settings. These facies are generally associated with the development of continental rift structures, both without significant volcanic activity (examples in Canada, China, Finland and Poland) and with volcanic activity (Czech Republic and Namibia). In these PGE-metal-rich black shales the fractionation of the PGE in the black shales reflects the fractionation of the PGE in the associated volcanic rocks. It was further concluded that, in metal-rich black shales in which distributions of Ni and Cu have been altered by various processes, the Ni/Cu versus Pd/Ir and Cu/Ir versus Ni/Pd ratios plots are applicable for determination of the source of PGEs only after careful evaluation of Ni and Cu enrichments. PGEs enrichments have been recently found in Zn-, Cu-, and Ni-rich black shales in a number of geological settings. These facies are generally associated with the development of continental rift structures, both without significant volcanic activity (examples in Canada, China, Finland and Poland) and with volcanic activity (Czech Republic and Namibia). In these PGE-metal-rich black shales the fractionation of the PGE in the black shales reflects the fractionation of the PGE in the associated volcanic rocks. It was further concluded that, in metal-rich black shales in which distributions of Ni and Cu have been altered by various processes, the Ni/Cu versus Pd/Ir and Cu/Ir versus Ni/Pd ratios plots are applicable for determination of the source of PGEs only after careful evaluation of Ni and Cu enrichments. Aplikace Ni/Cu versus Pd/Ir aCu/Ir versus Ni/Pd diagramů pro určení zdrojů obohacení Pt-kovy v Zn-, Cu- a Ni- bohatých černých břidlicích.
dcterms:title
Can we use mantle normalization and metal rations for identification of PGE sources in metal-rich black shales? Can we use mantle normalization and metal rations for identification of PGE sources in metal-rich black shales? Can we use mantle normalization and metal rations for identification of PGE sources in metal-rich black shales?
skos:prefLabel
Can we use mantle normalization and metal rations for identification of PGE sources in metal-rich black shales? Can we use mantle normalization and metal rations for identification of PGE sources in metal-rich black shales? Can we use mantle normalization and metal rations for identification of PGE sources in metal-rich black shales?
skos:notation
RIV/00025798:_____/03:00000493!RIV07-MZP-00025798
n4:strany
849-852
n4:aktivita
n20:Z
n4:aktivity
Z(MZP:N03/98:00)
n4:dodaniDat
n18:2007
n4:domaciTvurceVysledku
n14:1142488 n14:7303203
n4:druhVysledku
n9:D
n4:duvernostUdaju
n17:S
n4:entitaPredkladatele
n16:predkladatel
n4:idSjednocenehoVysledku
600315
n4:idVysledku
RIV/00025798:_____/03:00000493
n4:jazykVysledku
n8:eng
n4:klicovaSlova
metal-rich black shale, mantle normalization, metal ratios, source of PGE
n4:klicoveSlovo
n7:mantle%20normalization n7:metal%20ratios n7:metal-rich%20black%20shale n7:source%20of%20PGE
n4:kontrolniKodProRIV
[1A133130F897]
n4:mistoKonaniAkce
Athens
n4:mistoVydani
Rotterdam
n4:nazevZdroje
Mineral Exploration and Sustainable Development
n4:obor
n11:DB
n4:pocetDomacichTvurcuVysledku
3
n4:pocetTvurcuVysledku
3
n4:rokUplatneniVysledku
n18:2003
n4:tvurceVysledku
Vymazalová, Anna Barnes, S.-J. Pašava, Jan
n4:typAkce
n12:CST
n4:zahajeniAkce
2003-08-24+02:00
n4:zamer
n13:MZP%3AN03%2F98%3A00
s:numberOfPages
4
n15:hasPublisher
Millpress
n6:isbn
90-77017-77-1