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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F06%3A9902%21RIV10-GA0-11310___
rdf:type
n12:Vysledek skos:Concept
dcterms:description
The presence of numerous roof pendants, stoped blocks and discordant intrusive contacts suggests that magmatic stoping was a widespread, large-scale process during the final construction of the Central Bohemian Plutonic Complex, Bohemian Massif. The measured total length of the discordant contacts formed by stoping corresponds to about half of all contacts with the upper-crustal host rocks. In addition, at least some of the straight, cleavage-parallel intrusive contacts may also have recorded complex intrusive histories ending with piecemeal stoping of thin cleavage-bounded host rock blocks into the magma chamber. Based on the above, we argue that the fast strain rates required for emplacement of large plutons of the Central Bohemian Plutonic Complex into brittle upper crustal host rocks over relatively short-time span could not have been accommodated entirely by slow ductile flow or slip along faults. The presence of numerous roof pendants, stoped blocks and discordant intrusive contacts suggests that magmatic stoping was a widespread, large-scale process during the final construction of the Central Bohemian Plutonic Complex, Bohemian Massif. The measured total length of the discordant contacts formed by stoping corresponds to about half of all contacts with the upper-crustal host rocks. In addition, at least some of the straight, cleavage-parallel intrusive contacts may also have recorded complex intrusive histories ending with piecemeal stoping of thin cleavage-bounded host rock blocks into the magma chamber. Based on the above, we argue that the fast strain rates required for emplacement of large plutons of the Central Bohemian Plutonic Complex into brittle upper crustal host rocks over relatively short-time span could not have been accommodated entirely by slow ductile flow or slip along faults.
dcterms:title
Magmatic stoping as an important emplacement mechanism of Variscan plutons: evidence from roof pendants in the Central Bohemian Plutonic Complex (Bohemian Massif) Magmatic stoping as an important emplacement mechanism of Variscan plutons: evidence from roof pendants in the Central Bohemian Plutonic Complex (Bohemian Massif)
skos:prefLabel
Magmatic stoping as an important emplacement mechanism of Variscan plutons: evidence from roof pendants in the Central Bohemian Plutonic Complex (Bohemian Massif) Magmatic stoping as an important emplacement mechanism of Variscan plutons: evidence from roof pendants in the Central Bohemian Plutonic Complex (Bohemian Massif)
skos:notation
RIV/00216208:11310/06:9902!RIV10-GA0-11310___
n3:aktivita
n9:P n9:V
n3:aktivity
P(GA205/02/0514), V
n3:cisloPeriodika
5
n3:dodaniDat
n10:2010
n3:domaciTvurceVysledku
n6:1848941 n6:8387699 n6:7631219
n3:druhVysledku
n18:J
n3:duvernostUdaju
n13:S
n3:entitaPredkladatele
n16:predkladatel
n3:idSjednocenehoVysledku
483843
n3:idVysledku
RIV/00216208:11310/06:9902
n3:jazykVysledku
n17:eng
n3:klicovaSlova
Bohemian Massif; Emplacement; Magmatic stoping; Pluton; Variscides
n3:klicoveSlovo
n4:Bohemian%20Massif n4:Magmatic%20stoping n4:Emplacement n4:Variscides n4:Pluton
n3:kodStatuVydavatele
DE - Spolková republika Německo
n3:kontrolniKodProRIV
[78910DBA54AC]
n3:nazevZdroje
International Journal of Earth Sciences
n3:obor
n15:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
3
n3:projekt
n14:GA205%2F02%2F0514
n3:rokUplatneniVysledku
n10:2006
n3:svazekPeriodika
95
n3:tvurceVysledku
Kachlík, Václav Holub, František Žák, Jiří
s:issn
1437-3254
s:numberOfPages
19
n11:organizacniJednotka
11310