About: High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif)

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About: High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif) Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	The garnet-sillimanite-cordierite kinzigite from Petrovice, Jihlava Pluton, Moldanubian Zone, Czech Republic has a hyperaluminous chemical composition. Its mineral assemblage consisting of garnet and prismatic sillimanite 1, relics of cordierite, hercynite, rutile 1, ilmenite and quartz, retrograde minerals - cordierite 11, fibrolitic sillimanite II and Ti-rich biotite and leucocratic portions with abundant K-feldspar, quartz and plagioclase which closely matches a restite. The prograde part of the reaction history was virtually obliterated and the mineral reactions: (1) Crd + Hrc = Grt + Sil; (2) Hrc+Qtz = Grt+Sil; (3) Grt+Sil+Qtz+L = Crd+Bt; (4) Grt+L = Crd+Bt+Qtz;, (5) Grt+Crd+L = Bt+Sil;, (6) Crd + L = Bt + Sil + Qtz took place during cooling. The relic assemblages cordierite+hercynite and hercynite+quartz, which represent a peak of metamorphism, are stable for P similar to 0.5 GPa at T > similar to 900 degrees C. The garnet-sillimanite-cordierite kinzigite from Petrovice, Jihlava Pluton, Moldanubian Zone, Czech Republic has a hyperaluminous chemical composition. Its mineral assemblage consisting of garnet and prismatic sillimanite 1, relics of cordierite, hercynite, rutile 1, ilmenite and quartz, retrograde minerals - cordierite 11, fibrolitic sillimanite II and Ti-rich biotite and leucocratic portions with abundant K-feldspar, quartz and plagioclase which closely matches a restite. The prograde part of the reaction history was virtually obliterated and the mineral reactions: (1) Crd + Hrc = Grt + Sil; (2) Hrc+Qtz = Grt+Sil; (3) Grt+Sil+Qtz+L = Crd+Bt; (4) Grt+L = Crd+Bt+Qtz;, (5) Grt+Crd+L = Bt+Sil;, (6) Crd + L = Bt + Sil + Qtz took place during cooling. The relic assemblages cordierite+hercynite and hercynite+quartz, which represent a peak of metamorphism, are stable for P similar to 0.5 GPa at T > similar to 900 degrees C. (en)
Title	High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif) High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif) (en)
skos:prefLabel	High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif) High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif) (en)
skos:notation	RIV/00216224:14310/07:00020862!RIV11-GA0-14310___
http://linked.open...avai/riv/aktivita	P Z
http://linked.open...avai/riv/aktivity	P(GA205/03/0040), Z(MSM0021622412)
http://linked.open...iv/cisloPeriodika	5
http://linked.open...vai/riv/dodaniDat	2011
http://linked.open...aciTvurceVysledku	Buriánek, David Burger, David Novák, Milan Leichmann, Jaromír
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Masarykova univerzita / Přírodovědecká fakulta
http://linked.open...dnocenehoVysledku	424105
http://linked.open...ai/riv/idVysledku	RIV/00216224:14310/07:00020862
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Moldanubian Zone; Jihlava Pluton; mineral reactions; HT metamorphism; heat source; garnet-sillimanite rock; restite (en)
http://linked.open.../riv/klicoveSlovo	heat source restite Moldanubian Zone mineral reactions HT metamorphism Jihlava Pluton garnet-sillimanite rock
http://linked.open...odStatuVydavatele	SK - Slovenská republika
http://linked.open...ontrolniKodProRIV	[6A98A554AE91]
http://linked.open...i/riv/nazevZdroje	Geologica Carpathica
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	4 (xsd:int)
http://linked.open...cetTvurcuVysledku	4 (xsd:int)
http://linked.open...vavai/riv/projekt	Partial melting of rocks in the root zone of the Variscan orogenic belt (Moldanubian zone, Bohemian Massif)
http://linked.open...UplatneniVysledku	2007
http://linked.open...v/svazekPeriodika	58
http://linked.open...iv/tvurceVysledku	Leichmann, Jaromír Novák, Milan Buriánek, David Burger, David
http://linked.open...n/vavai/riv/zamer	Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL)
issn	1335-0552
number of pages	10 (xsd:int)
http://localhost/t...ganizacniJednotka	14310
is http://linked.open...avai/riv/vysledek of	High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif) High temperature tu ultrahigh-temperature metamorpism related to multiple ultrapotassic intrusions:evidence from garnet-silimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif)

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