About: Hyperpotassic granulites from the Blanský les Massif (Moldanubian Zone, Bohemian Massif) revisited     Goto   Sponge   NotDistinct   Permalink

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Description
  • In the Blanský les granulite Massif built mainly by felsic calc-alkaline HP?HT Grt + Ky granulite, occur rare small bodies of hyperpotassic (K2O < 7 %, up to c. 14 %, K2O/Na2O = 3.1?9.2 wt. %) granulite with Grt or Px. Characteristic are high concentrations of Cs, Rb, Ba and U at variable enrichments in Zr and Hf; contents some HFSE (Ti, Nb and Ta) are extremely low. The Sr?Nd isotopic ratios document the derivation from mature crustal sources (Eps337 -5.5; 87Sr/86Sr337 = 0.7109-0.7279). Ap saturation temperatures are high, close to the previously estimated conditions of (re)crystallization for both calc-alkaline and hyperpotassic granulites. The hyperpotassic granulites are interpreted as Viséan igneous rocks. The parental magma could have originated by low degrees of HP?HT, non-eutectic partial melting. The low-scale melt was most likely expelled close to the HP?HT metamorphic peak or at early stages of decompression from common Moldanubian calc-alkaline granulites.
  • In the Blanský les granulite Massif built mainly by felsic calc-alkaline HP?HT Grt + Ky granulite, occur rare small bodies of hyperpotassic (K2O < 7 %, up to c. 14 %, K2O/Na2O = 3.1?9.2 wt. %) granulite with Grt or Px. Characteristic are high concentrations of Cs, Rb, Ba and U at variable enrichments in Zr and Hf; contents some HFSE (Ti, Nb and Ta) are extremely low. The Sr?Nd isotopic ratios document the derivation from mature crustal sources (Eps337 -5.5; 87Sr/86Sr337 = 0.7109-0.7279). Ap saturation temperatures are high, close to the previously estimated conditions of (re)crystallization for both calc-alkaline and hyperpotassic granulites. The hyperpotassic granulites are interpreted as Viséan igneous rocks. The parental magma could have originated by low degrees of HP?HT, non-eutectic partial melting. The low-scale melt was most likely expelled close to the HP?HT metamorphic peak or at early stages of decompression from common Moldanubian calc-alkaline granulites. (en)
Title
  • Hyperpotassic granulites from the Blanský les Massif (Moldanubian Zone, Bohemian Massif) revisited
  • Hyperpotassic granulites from the Blanský les Massif (Moldanubian Zone, Bohemian Massif) revisited (en)
skos:prefLabel
  • Hyperpotassic granulites from the Blanský les Massif (Moldanubian Zone, Bohemian Massif) revisited
  • Hyperpotassic granulites from the Blanský les Massif (Moldanubian Zone, Bohemian Massif) revisited (en)
skos:notation
  • RIV/00216208:11310/07:10001176!RIV10-MZP-11310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/03/0040), S, Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika
  • 1-2
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
  • 425181
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11310/07:10001176
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • granulites; alkali feldspar syenites; high-pressure melting; geochemistry; Moldanubian Zone; Bohemian Massif (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [2621E8B4F0B6]
http://linked.open...i/riv/nazevZdroje
  • Journal of Geosciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 52
http://linked.open...iv/tvurceVysledku
  • Erban, Vojtěch
  • Janoušek, Vojtěch
  • Míková, Jitka
  • Finger, Fritz
  • Krenn, Erwin
http://linked.open...n/vavai/riv/zamer
issn
  • 1802-6222
number of pages
http://localhost/t...ganizacniJednotka
  • 11310
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