About: Anomalous PGE in Fe-Cu-As ores from the Tisová Besshi-type deposit (Bohemian Massif)     Goto   Sponge   NotDistinct   Permalink

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  • Anomalous concentrations of Pt (33 - 4740 ppb, avg. 1225 ppb) accompanied by low Pd values (2.6 - 3.7 ppb), have been detected in ore samples from the Tisová Cu deposit, considered to be of Besshi-type deposit. Pd/Ir and Pd/Pt ratios are close to those in tholeitic basalts. Mantle normalized Ni-PGE-Cu patterns in ore samples from Tisová show significant Pt and Rh enrichment when compared to Besshi deposit (Japan) and other VHMS deposits of the Iberian Pyrite Belt (e.g. Neves Corvo and Rio Tinto). The studied ore samples are characterized by the presence of pyrite, pyrrhotite, chalcopyrite, arsenopyrite, sphalerite, native Bi, jamesonite, cobaltite, willyamite, and Fe-oxides (limonite). Mineralogical and subsequent LA-ICP-MS study have not resulted in the identification of principal PGE phases. Likely, Pt occurs as Pt-Fe oxide but the presence of other PGE discrete PGM on the boundary of sulfide grains cannot be excluded.
  • Anomalous concentrations of Pt (33 - 4740 ppb, avg. 1225 ppb) accompanied by low Pd values (2.6 - 3.7 ppb), have been detected in ore samples from the Tisová Cu deposit, considered to be of Besshi-type deposit. Pd/Ir and Pd/Pt ratios are close to those in tholeitic basalts. Mantle normalized Ni-PGE-Cu patterns in ore samples from Tisová show significant Pt and Rh enrichment when compared to Besshi deposit (Japan) and other VHMS deposits of the Iberian Pyrite Belt (e.g. Neves Corvo and Rio Tinto). The studied ore samples are characterized by the presence of pyrite, pyrrhotite, chalcopyrite, arsenopyrite, sphalerite, native Bi, jamesonite, cobaltite, willyamite, and Fe-oxides (limonite). Mineralogical and subsequent LA-ICP-MS study have not resulted in the identification of principal PGE phases. Likely, Pt occurs as Pt-Fe oxide but the presence of other PGE discrete PGM on the boundary of sulfide grains cannot be excluded. (en)
Title
  • Anomalous PGE in Fe-Cu-As ores from the Tisová Besshi-type deposit (Bohemian Massif)
  • Anomalous PGE in Fe-Cu-As ores from the Tisová Besshi-type deposit (Bohemian Massif) (en)
skos:prefLabel
  • Anomalous PGE in Fe-Cu-As ores from the Tisová Besshi-type deposit (Bohemian Massif)
  • Anomalous PGE in Fe-Cu-As ores from the Tisová Besshi-type deposit (Bohemian Massif) (en)
skos:notation
  • RIV/00025798:_____/11:00000452!RIV12-MZP-00025798
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, Z(MZP0002579801)
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
  • 186347
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/11:00000452
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • anomalous PGE, Tisová, Besshi type deposit, Bohemian Massif (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [4019DC4EAB99]
http://linked.open...v/mistoKonaniAkce
  • Antofagasta, Chile
http://linked.open...i/riv/mistoVydani
  • Antofagasta
http://linked.open...i/riv/nazevZdroje
  • Let's talk ore deposits.Proceedings of the 11th SGA Biennial Meeting, Antofagasta, Chile, 26-29 September 2011
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Malec, Jan
  • Pašava, Jan
  • Rojík, Petr
  • Vymazalová, Anna
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
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  • Ediciones Universidad Catolica del Norte
https://schema.org/isbn
  • 978-956-287-329-1
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