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rdf:type
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Description
| - 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)
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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)
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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)
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skos:notation
| - RIV/67985831:_____/09:00329539!RIV10-AV0-67985831
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
| - P(IAA3013006), Z(AV0Z30130516)
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/67985831:_____/09:00329539
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - ultra-high-pressure metamorphism; P-T path; garnet pyroxenite (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
| - Journal of Mineralogical and Petrological Sciences
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Hirajima, T.
- Naemura, K.
- Svojtka, Martin
- Hisashima, H.
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http://linked.open...ain/vavai/riv/wos
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http://linked.open...n/vavai/riv/zamer
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issn
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number of pages
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is http://linked.open...avai/riv/vysledek
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