About: High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic)

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About: High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic) Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	Felsic granulites from the Kutná Hora complex in the Moldanubian zone preserve mineral assemblage that records transition from early eclogite to granulite facies conditions, and exhibits leucocratic banding, which is interpreted as an evidence for melt loss during the decompression path. Garnet cores grew during omphacite breakdown and phengite dehydration melting at 940 °C and 2.6 GPa, following by decompression heating to 1020 °C and 2.1 GPa. The maximum melt productivity was 26 and 18 vol.%, respectively, at peak temperature ~1.05–0.75 H2O wt.%, prior to the melting. The preservation of prograde garnet-rich assemblages required nearly complete melt loss (15–25 vol.%), interpreted to have occurred at 1000–1020 °C and 2.2–2.4 GPa by garnet mode isopleths, followed by crystallization of small amounts of residual melt at 760 °C and 1.0 GPa. Phase formation and melt productivity were independently determined by experiments in the piston-cylinder apparatus at 850–1100 °C and 1.7–2.1 GPa. Felsic granulites from the Kutná Hora complex in the Moldanubian zone preserve mineral assemblage that records transition from early eclogite to granulite facies conditions, and exhibits leucocratic banding, which is interpreted as an evidence for melt loss during the decompression path. Garnet cores grew during omphacite breakdown and phengite dehydration melting at 940 °C and 2.6 GPa, following by decompression heating to 1020 °C and 2.1 GPa. The maximum melt productivity was 26 and 18 vol.%, respectively, at peak temperature ~1.05–0.75 H2O wt.%, prior to the melting. The preservation of prograde garnet-rich assemblages required nearly complete melt loss (15–25 vol.%), interpreted to have occurred at 1000–1020 °C and 2.2–2.4 GPa by garnet mode isopleths, followed by crystallization of small amounts of residual melt at 760 °C and 1.0 GPa. Phase formation and melt productivity were independently determined by experiments in the piston-cylinder apparatus at 850–1100 °C and 1.7–2.1 GPa. (en)
Title	High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic) High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic) (en)
skos:prefLabel	High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic) High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic) (en)
skos:notation	RIV/00025798:_____/11:00000258!RIV12-MZP-00025798
http://linked.open...avai/predkladatel	Česká geologická služba
http://linked.open...avai/riv/aktivita	I P Z
http://linked.open...avai/riv/aktivity	I, P(GAP210/10/0249), P(GP205/09/P135), Z(MSM0021620855), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika	1-2
http://linked.open...vai/riv/dodaniDat	2012
http://linked.open...aciTvurceVysledku	Nahodilová, Radmila
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	Česká geologická služba
http://linked.open...dnocenehoVysledku	202084
http://linked.open...ai/riv/idVysledku	RIV/00025798:_____/11:00000258
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Felsic granulite, High-pressure metamorphism, Partial melting, Bohemian Massif, Variscan orogeny (en)
http://linked.open.../riv/klicoveSlovo	Bohemian Massif Felsic granulite High-pressure metamorphism Partial melting Variscan orogeny
http://linked.open...odStatuVydavatele	NL - Nizozemsko
http://linked.open...ontrolniKodProRIV	[22167914F12A]
http://linked.open...i/riv/nazevZdroje	Lithos
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	1 (xsd:int)
http://linked.open...cetTvurcuVysledku	5 (xsd:int)
http://linked.open...vavai/riv/projekt	Early convergence and exhumation history of ultrahigh-pressure lithologies in the Variscan orogen Geochemical cycle of volatiles at convergent plate boundaries: Thermodynamic models for aqueous fluids and silicate melts over wide range of pressures
http://linked.open...UplatneniVysledku	2011
http://linked.open...v/svazekPeriodika	125
http://linked.open...iv/tvurceVysledku	Dolejš, David Faryad, Wali Konzett, Jürgen Nahodilová, Radmila Tropper, Peter
http://linked.open...ain/vavai/riv/wos	000292663600040
http://linked.open...n/vavai/riv/zamer	Material flow mechanisms in the upper spheres of the Earth Geosciences for the Society of the 21st Century: from regional research to geological hazards and global changes.
issn	0024-4937
number of pages	18 (xsd:int)
http://bibframe.org/vocab/doi	10.1016/j.lithos.2011.03.017
is http://linked.open...avai/riv/vysledek of	High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic) High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic)

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