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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10283110%21RIV15-MSM-11310___
rdf:type
n3:Vysledek skos:Concept
rdfs:seeAlso
http://dx.doi.org/10.1016/j.jog.2013.10.002
dcterms:description
The mid-Carboniferous Pelhrimov core complex, Bohemian Massif, is a crustal-scale elongated granite-migmatite dome interpreted to have formed by gravity-driven diapiric upwelling of the metapelitic middle crust. The vertical diapiric flow is evidenced by outward-dipping foliation and lineation patterns, deformation coeval with the widespread presence of melt, rapid exhumation of the dome center from depths corresponding to pressure of about 0.6 GPa to shallow levels (pressure less than 0.2 GPa) within 2 M.y., and kinematic indicators of downward return flow of the mantling rocks. As compared to common diapirs, however, the Pelhrimov complex exhibits a more complicated inferred strain pattern with two perpendicular, irregularly alternating directions of horizontal extension in what is interpreted as the diapir head. Comparison of structural data from migmatites with anisotropy of magnetic susceptibility (AMS) data in granites also reveals that only final increments of strain are recorded in the granites. The map dimensions and gravity image of the, complex suggest that the diapiric upwelling affected a large portion of the orogen's interior between two microplates brought together during continental collision. The mid-Carboniferous Pelhrimov core complex, Bohemian Massif, is a crustal-scale elongated granite-migmatite dome interpreted to have formed by gravity-driven diapiric upwelling of the metapelitic middle crust. The vertical diapiric flow is evidenced by outward-dipping foliation and lineation patterns, deformation coeval with the widespread presence of melt, rapid exhumation of the dome center from depths corresponding to pressure of about 0.6 GPa to shallow levels (pressure less than 0.2 GPa) within 2 M.y., and kinematic indicators of downward return flow of the mantling rocks. As compared to common diapirs, however, the Pelhrimov complex exhibits a more complicated inferred strain pattern with two perpendicular, irregularly alternating directions of horizontal extension in what is interpreted as the diapir head. Comparison of structural data from migmatites with anisotropy of magnetic susceptibility (AMS) data in granites also reveals that only final increments of strain are recorded in the granites. The map dimensions and gravity image of the, complex suggest that the diapiric upwelling affected a large portion of the orogen's interior between two microplates brought together during continental collision.
dcterms:title
Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens
skos:prefLabel
Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens
skos:notation
RIV/00216208:11310/14:10283110!RIV15-MSM-11310___
n4:aktivita
n9:Z n9:I n9:P
n4:aktivity
I, P(GA13-16315S), P(GAP210/11/1168), Z(MSM0021620855)
n4:cisloPeriodika
leden
n4:dodaniDat
n5:2015
n4:domaciTvurceVysledku
n16:2387689 n16:1305794 n16:8387699
n4:druhVysledku
n15:J
n4:duvernostUdaju
n6:S
n4:entitaPredkladatele
n21:predkladatel
n4:idSjednocenehoVysledku
17271
n4:idVysledku
RIV/00216208:11310/14:10283110
n4:jazykVysledku
n18:eng
n4:klicovaSlova
metamorphic core complex; granite-migmatite dome; exhumation; Bohemian Massif; anisotropy of magnetic susceptibility (AMS)
n4:klicoveSlovo
n7:granite-migmatite%20dome n7:Bohemian%20Massif n7:metamorphic%20core%20complex n7:anisotropy%20of%20magnetic%20susceptibility%20%28AMS%29 n7:exhumation
n4:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n4:kontrolniKodProRIV
[0901594ECCE9]
n4:nazevZdroje
Journal of Geodynamics
n4:obor
n19:DB
n4:pocetDomacichTvurcuVysledku
3
n4:pocetTvurcuVysledku
8
n4:projekt
n17:GA13-16315S n17:GAP210%2F11%2F1168
n4:rokUplatneniVysledku
n5:2014
n4:svazekPeriodika
73
n4:tvurceVysledku
Finger, Fritz Johnson, Kenneth Šrámek, Josef Žák, Jiří Verner, Kryštof Machek, Matěj Paclíková, Jana Zavřelová, Alice
n4:wos
000336235900009
n4:zamer
n13:MSM0021620855
s:issn
0264-3707
s:numberOfPages
18
n14:doi
10.1016/j.jog.2013.10.002
n10:organizacniJednotka
11310