About: Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone     Goto   Sponge   NotDistinct   Permalink

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  • Three main Variscan tectono-metamorphic units with distinct metamorphic evolution are present at the eastern boundary of the Bohemian Massif: Moldanubian Zone (MZ), Svratka Unit (SU) and Polička Unit (PU). All these metamorphic complexes contain calc-silicate rocks, which occur as bodies, layers or nodules within gneisses, mica schists, marbles, amphibolites or skarns. Two groups of calc-silicate rocks are distinguished according to the presence/absence of garnet. The appearance of garnet is the result of continuous reactions among Fe-Ca-Al minerals. The dominant garnet-producing reaction calcite + quartz + clinozoisite = garnet + H2O + 5CO2 depends on the P–T conditions, XCO2 in the coexisting metamorphic fluids and bulk rock chemistry.
  • Three main Variscan tectono-metamorphic units with distinct metamorphic evolution are present at the eastern boundary of the Bohemian Massif: Moldanubian Zone (MZ), Svratka Unit (SU) and Polička Unit (PU). All these metamorphic complexes contain calc-silicate rocks, which occur as bodies, layers or nodules within gneisses, mica schists, marbles, amphibolites or skarns. Two groups of calc-silicate rocks are distinguished according to the presence/absence of garnet. The appearance of garnet is the result of continuous reactions among Fe-Ca-Al minerals. The dominant garnet-producing reaction calcite + quartz + clinozoisite = garnet + H2O + 5CO2 depends on the P–T conditions, XCO2 in the coexisting metamorphic fluids and bulk rock chemistry. (en)
Title
  • Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone
  • Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone (en)
skos:prefLabel
  • Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone
  • Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone (en)
skos:notation
  • RIV/00025798:_____/09:00000152!RIV10-MZP-00025798
http://linked.open...avai/riv/aktivita
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  • Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika
  • 3
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http://linked.open...aciTvurceVysledku
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http://linked.open...dnocenehoVysledku
  • 315965
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  • RIV/00025798:_____/09:00000152
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  • calc-silicate rocks, Polička Unit, Svratka Unit, Moldanubian Zone, P–T conditions, Czech Republic (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [4C78525D21E0]
http://linked.open...i/riv/nazevZdroje
  • Journal of Geosciences
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http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 54
http://linked.open...iv/tvurceVysledku
  • Buriánek, David
  • Pertoldová, Jaroslava
http://linked.open...n/vavai/riv/zamer
issn
  • 1802-6222
number of pages
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