| Attributes | Values |
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| rdf:type
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| Description
| - V moldanubické zóně se vyskytují granulity a ultradraselné magmatity v úzkém prostorovém a časovém sepětí. Pro nejbazičtější ultradraselné horniny, vysoké Cr, Ni a mg# vyžadují tavení Ol-bohatého (tedy plášťového) zdroje. Zvýšené obsahy U, Th, LREE a LILE, spolu s ochuzením Ti, Nb a Ta, vysokými poměry K /Na a Rb/Sr a izotopickým složením blízkým zralé kůře na první pohled odporují vzniku ze zemského pláště. Tento dvojaký geochemický charakter ukazuje na tavení anomálního litosférického pláště. Pozdně devonská-raně karbonská subdukce zralého korového materiálu mohla vést k metasomatismu a přímé kontaminaci nadložního plášťového klínu. Brzy po HP metamorfním vrcholu (~340Ma) a odlomení subdukované desky, tyto anomální plášťové domény mohly být taveny teplem pronikající astenosféry. To vedlo ke vzniku ultradraselných intruzí, úzce spjatých s výskyty HP granulitů v prostoru a čase. (cs)
- In the Moldanubian Zone occur granulites and ultrapotassic magmatites in a close spatial and temporal relationship. For the most basic UK rocks, the high Cr, Ni and mg# require derivation from an Ol-rich source. Elevated concentrations of U, Th, LREE and LILE, depletion in Ti, Nb and Ta as well as high K /Na and Rb/Sr ratios and crustal-like isotopic compositions apparently contradict the mantle origin. This dual geochemical character requires melting of anomalous lithospheric mantle. The Late Devonian-Early Carboniferous subduction of the mature crustal material is thought to have caused direct contamination and metasomatism in the overlying lithospheric mantle wedge. Shortly after the HP metamorphic peak (~340Ma) and the slab break off, these metasomatized and contaminated mantle domains were melted by advected heat from the invading asthenosphere, generating ultrapotassic intrusions, closely related to the granulite occurrences in space and time.
- In the Moldanubian Zone occur granulites and ultrapotassic magmatites in a close spatial and temporal relationship. For the most basic UK rocks, the high Cr, Ni and mg# require derivation from an Ol-rich source. Elevated concentrations of U, Th, LREE and LILE, depletion in Ti, Nb and Ta as well as high K /Na and Rb/Sr ratios and crustal-like isotopic compositions apparently contradict the mantle origin. This dual geochemical character requires melting of anomalous lithospheric mantle. The Late Devonian-Early Carboniferous subduction of the mature crustal material is thought to have caused direct contamination and metasomatism in the overlying lithospheric mantle wedge. Shortly after the HP metamorphic peak (~340Ma) and the slab break off, these metasomatized and contaminated mantle domains were melted by advected heat from the invading asthenosphere, generating ultrapotassic intrusions, closely related to the granulite occurrences in space and time. (en)
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| Title
| - The causal link between HP-HT metamorphism and ultrapotassic magmatism in collisional orogens: case study from the Moldanubian Zone of the Bohemian Massif
- The causal link between HP-HT metamorphism and ultrapotassic magmatism in collisional orogens: case study from the Moldanubian Zone of the Bohemian Massif (en)
- Zákonitá souvislost mezi HP-HT metamorfózou a ultradraselným magmatismem v kolizních orogénech: příkladová studie z moldanubické zóny Českého masívu (cs)
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| skos:prefLabel
| - The causal link between HP-HT metamorphism and ultrapotassic magmatism in collisional orogens: case study from the Moldanubian Zone of the Bohemian Massif
- The causal link between HP-HT metamorphism and ultrapotassic magmatism in collisional orogens: case study from the Moldanubian Zone of the Bohemian Massif (en)
- Zákonitá souvislost mezi HP-HT metamorfózou a ultradraselným magmatismem v kolizních orogénech: příkladová studie z moldanubické zóny Českého masívu (cs)
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| skos:notation
| - RIV/00025798:_____/07:00000029!RIV08-MZP-00025798
|
| http://linked.open.../vavai/riv/strany
| |
| http://linked.open...avai/riv/aktivita
| |
| http://linked.open...avai/riv/aktivity
| - P(GA205/02/0514), P(GA205/03/0040), P(GA205/07/0992), Z(MZP0002579801)
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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
| |
| http://linked.open...ai/riv/idVysledku
| - RIV/00025798:_____/07:00000029
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| http://linked.open...riv/jazykVysledku
| |
| http://linked.open.../riv/klicovaSlova
| - granulites, whole-rock geochemistry, continental collision, subduction, ultrapotassic magmatism, mantle metasomatism, Variscan belt, durbachites (en)
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| http://linked.open.../riv/klicoveSlovo
| |
| http://linked.open...odStatuVydavatele
| - GB - Spojené království Velké Británie a Severního Irska
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| http://linked.open...ontrolniKodProRIV
| |
| http://linked.open...i/riv/nazevZdroje
| - Proceedings of the Geologists' Association
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| http://linked.open...in/vavai/riv/obor
| |
| http://linked.open...ichTvurcuVysledku
| |
| http://linked.open...cetTvurcuVysledku
| |
| http://linked.open...vavai/riv/projekt
| |
| http://linked.open...UplatneniVysledku
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| http://linked.open...v/svazekPeriodika
| |
| http://linked.open...iv/tvurceVysledku
| - Holub, František
- Janoušek, Vojtěch
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| http://linked.open...n/vavai/riv/zamer
| |
| issn
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| number of pages
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| is http://linked.open...avai/riv/vysledek
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