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Description
| - Upper mantle xenoliths are abundant in the basanites of the Pliocene Kozákov volcano. The studied samples of spinel lherzolites come from the depth of about 50-75 km. The mineral assemblage preserved subsolidus temperatures of 1165-1052° from the time of xenolith entrapment. Mineralogical features as well as of the bulk lherzolite compositions are indicator of cryptic metasomatic events in the upper mantle.
- Upper mantle xenoliths are abundant in the basanites of the Pliocene Kozákov volcano. The studied samples of spinel lherzolites come from the depth of about 50-75 km. The mineral assemblage preserved subsolidus temperatures of 1165-1052° from the time of xenolith entrapment. Mineralogical features as well as of the bulk lherzolite compositions are indicator of cryptic metasomatic events in the upper mantle. (en)
- V bazanitech pliocénní kozákovské sopky jsou hojné xenolity svrchního pláště. Studované vzorky ultramafických xenolitů pocházejí z hloubky 50-75 km.Vypočítaná teplota subsolidifikace xenolitů odpovídá 1165-1052°a odpovídá období, kdy xenolity byly uzavřeny v bazaltové tavenině. Jak složení minerálů, tak celkové složení lherzolitů ukazují na skrytou metasomatózu ve svrchním plášti. (cs)
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Title
| - Upper mantle xenoliths from the Pliocene Kozákov volcano (NE Bohemia): P-T-fO2 and geochemical constrains
- Upper mantle xenoliths from the Pliocene Kozákov volcano (NE Bohemia): P-T-fO2 and geochemical constrains (en)
- Xenolity svrchního pláště pliocénní kozákovské sopky (sv. Čechy): P-T-fo2 a geochemické podmínky. (cs)
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skos:prefLabel
| - Upper mantle xenoliths from the Pliocene Kozákov volcano (NE Bohemia): P-T-fO2 and geochemical constrains
- Upper mantle xenoliths from the Pliocene Kozákov volcano (NE Bohemia): P-T-fO2 and geochemical constrains (en)
- Xenolity svrchního pláště pliocénní kozákovské sopky (sv. Čechy): P-T-fo2 a geochemické podmínky. (cs)
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skos:notation
| - RIV/00025798:_____/06:00000231!RIV07-MZP-00025798
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http://linked.open.../vavai/riv/strany
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
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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/00025798:_____/06:00000231
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Bohemian Massif, Cenozoic volcanism, ultramafic xenoliths, spinel lherzolite,harzburgite, peridotite. (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
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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...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Řanda, Zdeněk
- Ulrych, Jaromír
- Schovánek, Pavel
- Konečný, Patrik
- Huraiová, Monika
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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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