About: From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif)

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About: From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (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 Gföhl Unit is the largest migmatite terrain of the Variscan orogenic root in Europe. In its Rokytná Complex there is a well-preserved sequence documenting the entire migmatitization process on both outcrop and regional scales. The sequence starts with (i) banded orthogneiss with separated monomineralic layers, through (ii) migmatitic mylonitic gneiss, (iii) schlieren migmatite characterised by disappearance of monomineralic layering and finally to (iv) felsic nebulitic migmatite with no relics of the original banding. While each type of migmatite shows a distinct whole-rock geochemical and Sr-Nd isotopic fingerprint, the whole sequence evolves along regular, more or less smooth trends for most of the elements. The individual migmatites can be explained by different degrees of equilibration between the bulk rock and the passing granitic melt. The modelling of the mass balance resulted in identification of a component added by a heterogeneous nucleation of Fsp, Qz and Ap from the melt. The Gföhl Unit is the largest migmatite terrain of the Variscan orogenic root in Europe. In its Rokytná Complex there is a well-preserved sequence documenting the entire migmatitization process on both outcrop and regional scales. The sequence starts with (i) banded orthogneiss with separated monomineralic layers, through (ii) migmatitic mylonitic gneiss, (iii) schlieren migmatite characterised by disappearance of monomineralic layering and finally to (iv) felsic nebulitic migmatite with no relics of the original banding. While each type of migmatite shows a distinct whole-rock geochemical and Sr-Nd isotopic fingerprint, the whole sequence evolves along regular, more or less smooth trends for most of the elements. The individual migmatites can be explained by different degrees of equilibration between the bulk rock and the passing granitic melt. The modelling of the mass balance resulted in identification of a component added by a heterogeneous nucleation of Fsp, Qz and Ap from the melt. (en)
Title	From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif) From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif) (en)
skos:prefLabel	From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif) From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif) (en)
skos:notation	RIV/00216208:11310/08:10000547!RIV10-GA0-11310___
http://linked.open...avai/riv/aktivita	P Z
http://linked.open...avai/riv/aktivity	P(GA205/04/2065), P(GA205/07/0992), P(IAA3111401), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika	3-4
http://linked.open...vai/riv/dodaniDat	2010
http://linked.open...aciTvurceVysledku	Janoušek, Vojtěch Schulmann, Karel Štípská, Pavla
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	Univerzita Karlova v Praze / Přírodovědecká fakulta
http://linked.open...dnocenehoVysledku	368621
http://linked.open...ai/riv/idVysledku	RIV/00216208:11310/08:10000547
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Melt infiltration; Porous flow; Migmatites; Whole-rock geochemistry; Mass balance; Bohemian Massif (Gföhl Unit) (en)
http://linked.open.../riv/klicoveSlovo	Mass balance Bohemian Massif (Gföhl Unit) Melt infiltration Migmatites Porous flow Whole-rock geochemistry
http://linked.open...odStatuVydavatele	NL - Nizozemsko
http://linked.open...ontrolniKodProRIV	[59667EA8867D]
http://linked.open...i/riv/nazevZdroje	Lithos
http://linked.open...in/vavai/riv/obor	DD
http://linked.open...ichTvurcuVysledku	3 (xsd:int)
http://linked.open...cetTvurcuVysledku	5 (xsd:int)
http://linked.open...vavai/riv/projekt	Application of non-traditional isotopes in the petrogenesis of granitic rocks Relation of extrusion and horizontal flow of lower crust to the origin of the lower crustal wedge along eastern margin of Bohemian massive Rheology of quartzo-feldspathic rocks and its numerical modelling
http://linked.open...UplatneniVysledku	2008
http://linked.open...v/svazekPeriodika	102
http://linked.open...iv/tvurceVysledku	Erban, Vojtěch Janoušek, Vojtěch Schulmann, Karel Štípská, Pavla Hasalová, Pavlína
http://linked.open...ain/vavai/riv/wos	000256823100006
http://linked.open...n/vavai/riv/zamer	Geosciences for the Society of the 21st Century: from regional research to geological hazards and global changes.
issn	0024-4937
number of pages	30 (xsd:int)
http://localhost/t...ganizacniJednotka	11310
is http://linked.open...avai/riv/vysledek of	From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif) From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif) From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif) From orthogneiss to migmatite: Geochemical assessment of the melt infiltration model in the Gföhl Unit (Moldanubian Zone, Bohemian Massif)

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