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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F08%3A00000100%21RIV09-MZP-00025798
rdf:type
n8:Vysledek skos:Concept
dcterms:description
This paper elaborates on the concept of multiple magmatic fabrics in plutons. After a general overview of various types of multiple fabrics that may develop in magmatic rocks, two case examples of porphyritic granite and melasyenite plutons in the Bohemian Massif are examined. Multiple magmatic fabrics in these two plutons are interpreted in terms of fabric superposition, where late weak strain is superposed onto high-strength phenocryst framework, but is recorded only by small mineral grains (biotite, magnetite) in the melt-bearing matrix. This mechanism may explain the discrepancy between mesoscopic feldspar fabric and AMS. We conclude that multiple magmatic fabrics may thus result from accumulated strain caused by different processes during final pluton crystallization and, as such, may serve as a sensitive indicator of the evolving interactions between magmatic and tectonic processes in the Earth's crust. This paper elaborates on the concept of multiple magmatic fabrics in plutons. After a general overview of various types of multiple fabrics that may develop in magmatic rocks, two case examples of porphyritic granite and melasyenite plutons in the Bohemian Massif are examined. Multiple magmatic fabrics in these two plutons are interpreted in terms of fabric superposition, where late weak strain is superposed onto high-strength phenocryst framework, but is recorded only by small mineral grains (biotite, magnetite) in the melt-bearing matrix. This mechanism may explain the discrepancy between mesoscopic feldspar fabric and AMS. We conclude that multiple magmatic fabrics may thus result from accumulated strain caused by different processes during final pluton crystallization and, as such, may serve as a sensitive indicator of the evolving interactions between magmatic and tectonic processes in the Earth's crust. This paper elaborates on the concept of multiple magmatic fabrics in plutons. After a general overview of various types of multiple fabrics that may develop in magmatic rocks, two case examples of porphyritic granite and melasyenite plutons in the Bohemian Massif are examined. Multiple magmatic fabrics in these two plutons are interpreted in terms of fabric superposition, where late weak strain is superposed onto high-strength phenocryst framework, but is recorded only by small mineral grains (biotite, magnetite) in the melt-bearing matrix. This mechanism may explain the discrepancy between mesoscopic feldspar fabric and AMS. We conclude that multiple magmatic fabrics may thus result from accumulated strain caused by different processes during final pluton crystallization and, as such, may serve as a sensitive indicator of the evolving interactions between magmatic and tectonic processes in the Earth's crust.
dcterms:title
Multiple magmatic fabrics in plutons: an overlooked tool for exploring interactions between magmatic processes and regional deformation? Multiple magmatic fabrics in plutons: an overlooked tool for exploring interactions between magmatic processes and regional deformation? Mnohonásobná magmatická stavba v plutonech: přehlížený indikátor interakcí mezi magmatickými procesy a regionální deformací?
skos:prefLabel
Multiple magmatic fabrics in plutons: an overlooked tool for exploring interactions between magmatic processes and regional deformation? Multiple magmatic fabrics in plutons: an overlooked tool for exploring interactions between magmatic processes and regional deformation? Mnohonásobná magmatická stavba v plutonech: přehlížený indikátor interakcí mezi magmatickými procesy a regionální deformací?
skos:notation
RIV/00025798:_____/08:00000100!RIV09-MZP-00025798
n3:aktivita
n4:V n4:Z n4:P
n3:aktivity
P(GP205/07/P226), V, Z(MSM0021620855)
n3:cisloPeriodika
4
n3:dodaniDat
n11:2009
n3:domaciTvurceVysledku
n13:8387699 n13:7257910 n13:2387689
n3:druhVysledku
n14:J
n3:duvernostUdaju
n12:C
n3:entitaPredkladatele
n18:predkladatel
n3:idSjednocenehoVysledku
381191
n3:idVysledku
RIV/00025798:_____/08:00000100
n3:jazykVysledku
n16:eng
n3:klicovaSlova
deformation, granite, fabric, magnetic susceptibility anisotropy, pluton
n3:klicoveSlovo
n5:deformation n5:magnetic%20susceptibility%20anisotropy n5:granite n5:fabric n5:pluton
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[3A052144B35C]
n3:nazevZdroje
Geological Magazine
n3:obor
n17:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
3
n3:projekt
n15:GP205%2F07%2FP226
n3:rokUplatneniVysledku
n11:2008
n3:svazekPeriodika
145
n3:tvurceVysledku
Žák, Jiří Verner, Kryštof Týcová, Patricie
n3:wos
257848500006
n3:zamer
n10:MSM0021620855
s:issn
0016-7568
s:numberOfPages
15