About: Potassian hastingsite and potassichastingsite from garnet - hedenbergite skarn at Vlastějovice, Czech Republic     Goto   Sponge   NotDistinct   Permalink

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  • Potassichastingsite (3.05 wt. % K2O) occurs along as large phenocrysts in metasomatic rims of pegmatite dykes penetrating Ca-Fe skarn at Vlastějovice, in the Moldanubian Zone, Bohemian Massif, Czech Republic. The skarn is characterized by the high f (O2) assemblage of grossularite – andradite garnets, Fe3+- enriched hedenbergite, magnetite, and epidote. Amphibole is characterized by Fe3+ > VIAl (Fe3+ 0.80 to 1.07 apfu, VIAl 0.30 to 0.38 apfu), high XFe (0.83 to 0.72) and low X-site vacancies (0.09 to 0.22). Due to high K content (up to 0.62 apfu) it corresponds to potassichastingsite or potassian hastingsite. The OH content ranges from 1.60 to 1.82 apfu, fluorine from 0.17 to 0.33 apfu, but chlorine only from 0.03 to 0.06 apfu. Thus this amphibole belongs to most K-rich chlorine-poor hastingsites reported: (K0.62Na0.28)0.87 (Ca1.95 Na0.05)2.00 (Fe2+2.79Mg0.92Mn0.03 Fe3+0.80Ti0.05 Al0.38)4.96 (Si5.98Al2.02)8.00 O22.05 (OH1.71F0.18Cl0.06)1.95.
  • Potassichastingsite (3.05 wt. % K2O) occurs along as large phenocrysts in metasomatic rims of pegmatite dykes penetrating Ca-Fe skarn at Vlastějovice, in the Moldanubian Zone, Bohemian Massif, Czech Republic. The skarn is characterized by the high f (O2) assemblage of grossularite – andradite garnets, Fe3+- enriched hedenbergite, magnetite, and epidote. Amphibole is characterized by Fe3+ > VIAl (Fe3+ 0.80 to 1.07 apfu, VIAl 0.30 to 0.38 apfu), high XFe (0.83 to 0.72) and low X-site vacancies (0.09 to 0.22). Due to high K content (up to 0.62 apfu) it corresponds to potassichastingsite or potassian hastingsite. The OH content ranges from 1.60 to 1.82 apfu, fluorine from 0.17 to 0.33 apfu, but chlorine only from 0.03 to 0.06 apfu. Thus this amphibole belongs to most K-rich chlorine-poor hastingsites reported: (K0.62Na0.28)0.87 (Ca1.95 Na0.05)2.00 (Fe2+2.79Mg0.92Mn0.03 Fe3+0.80Ti0.05 Al0.38)4.96 (Si5.98Al2.02)8.00 O22.05 (OH1.71F0.18Cl0.06)1.95. (en)
  • Draselný hastingsit s obsahem až 3.05 hm. % K2O se vyskytuje jako velké fenokrystaly v lemech pegmatitových žil, které pronikají Ca-Fe skarn ve Vlastějovicích (Moldanubikum). (cs)
Title
  • Potassian hastingsite and potassichastingsite from garnet - hedenbergite skarn at Vlastějovice, Czech Republic
  • Potassian hastingsite and potassichastingsite from garnet - hedenbergite skarn at Vlastějovice, Czech Republic (en)
  • Draslíkem bohatý a draselný hastingsit z granát - hedenbergitového skarnu ve Vladtějovicích, Česká republika (cs)
skos:prefLabel
  • Potassian hastingsite and potassichastingsite from garnet - hedenbergite skarn at Vlastějovice, Czech Republic
  • Potassian hastingsite and potassichastingsite from garnet - hedenbergite skarn at Vlastějovice, Czech Republic (en)
  • Draslíkem bohatý a draselný hastingsit z granát - hedenbergitového skarnu ve Vladtějovicích, Česká republika (cs)
skos:notation
  • RIV/00025798:_____/07:00000335!RIV08-MZP-00025798
http://linked.open.../vavai/riv/strany
  • 161-168
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  • Z(MZP0002579801)
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  • 2
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  • 442880
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  • RIV/00025798:_____/07:00000335
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  • potassichastingsite,skarn,Vlastějovice,Bohemian massif,Czech Republic (en)
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  • DE - Spolková republika Německo
http://linked.open...ontrolniKodProRIV
  • [A6A9E8BF3832]
http://linked.open...i/riv/nazevZdroje
  • Neues Jahrbuch für Mineralogie. Abhandlungen
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  • 184
http://linked.open...iv/tvurceVysledku
  • Žáček, Vladimír
http://linked.open...n/vavai/riv/zamer
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  • 0077-7757
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