About: An ultra-high-pressure metamorphic condition and isothermal decompression path obtained from a garnet-pyroxenite in the Horní Bory granulite of the Bohemian Massif     Goto   Sponge   NotDistinct   Permalink

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  • An ultrahigh-pressure metamorphic condition (140 km) at ca. 900 °C is identified from a garnet-pyroxenite, containing primary supersilicic clinopyroxene, as a part of mafic-ultramafic lenses enclosed in the Gföhl granulite at Horní Bory quarry of the Bohemian Massif, Czech Republic. Petrological data indicated that the garnet-pyroxenite has isothermally (ca. 900 °C) exhumed from upper mantle (140 km) to the lower crust (50 km), and the supersilicic clinopyroxene was decomposed to sodic augite and quartz during the exhumation. This ultra-high-pressure metamorphic evidence is the first to be derived from the mafic rock directly enclosed within the Horní Bory granulite in the Moldanubian Zone of the Bohemian Massif.
  • An ultrahigh-pressure metamorphic condition (140 km) at ca. 900 °C is identified from a garnet-pyroxenite, containing primary supersilicic clinopyroxene, as a part of mafic-ultramafic lenses enclosed in the Gföhl granulite at Horní Bory quarry of the Bohemian Massif, Czech Republic. Petrological data indicated that the garnet-pyroxenite has isothermally (ca. 900 °C) exhumed from upper mantle (140 km) to the lower crust (50 km), and the supersilicic clinopyroxene was decomposed to sodic augite and quartz during the exhumation. This ultra-high-pressure metamorphic evidence is the first to be derived from the mafic rock directly enclosed within the Horní Bory granulite in the Moldanubian Zone of the Bohemian Massif. (en)
Title
  • An ultra-high-pressure metamorphic condition and isothermal decompression path obtained from a garnet-pyroxenite in the Horní Bory granulite of the Bohemian Massif
  • An ultra-high-pressure metamorphic condition and isothermal decompression path obtained from a garnet-pyroxenite in the Horní Bory granulite of the Bohemian Massif (en)
skos:prefLabel
  • An ultra-high-pressure metamorphic condition and isothermal decompression path obtained from a garnet-pyroxenite in the Horní Bory granulite of the Bohemian Massif
  • An ultra-high-pressure metamorphic condition and isothermal decompression path obtained from a garnet-pyroxenite in the Horní Bory granulite of the Bohemian Massif (en)
skos:notation
  • RIV/67985831:_____/09:00329539!RIV10-AV0-67985831
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA3013006), Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika
  • 3
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
  • 302772
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/09:00329539
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • ultra-high-pressure metamorphism; P-T path; garnet pyroxenite (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • JP - Japonsko
http://linked.open...ontrolniKodProRIV
  • [75639490C8D2]
http://linked.open...i/riv/nazevZdroje
  • Journal of Mineralogical and Petrological Sciences
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
  • 104
http://linked.open...iv/tvurceVysledku
  • Hirajima, T.
  • Naemura, K.
  • Svojtka, Martin
  • Hisashima, H.
http://linked.open...ain/vavai/riv/wos
  • 000268375400006
http://linked.open...n/vavai/riv/zamer
issn
  • 1345-6296
number of pages
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