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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10281515%21RIV15-MSM-11310___
rdf:type
n12:Vysledek skos:Concept
rdfs:seeAlso
http://dx.doi.org/10.1016/j.jsg.2014.05.015
dcterms:description
The Melechov pluton, Bohemian Massif, is interpreted as a mid-crustal nested granitic diapir with an apical part exposed at the present-day erosion level. The diapir head exhibits a concentric structure defined by lithologic zoning and by the anisotropy of magnetic susceptibility (AMS). In concert with theoretical models, outward-dipping margin-parallel magnetic foliations are associated with oblate shapes of the susceptibility ellipsoids and higher degree of anisotropy, passing inward into weaker triaxial to prolate fabric. By contrast, magnetic fabric in an inner granite unit is in places oriented at a high angle to internal contacts and is interpreted as recording an internal diapir circulation. We use inverse modeling to calculate strain variations across the diapir from the AMS data. The magnetic fabric parameters and calculated strains are in agreement with strain distribution in heads of model Newtonian diapirs traveling a distance of two body radii and suggest granitic magma ascent as a crystal-poor suspension followed by crystallization of fabric markers and their response to strain near the final emplacement level. The intrusive fabric thus formed late but, though generally weak, was still capable of recording incremental strain gradient in the granite diapir. (C) 2014 Elsevier Ltd. All rights reserved. The Melechov pluton, Bohemian Massif, is interpreted as a mid-crustal nested granitic diapir with an apical part exposed at the present-day erosion level. The diapir head exhibits a concentric structure defined by lithologic zoning and by the anisotropy of magnetic susceptibility (AMS). In concert with theoretical models, outward-dipping margin-parallel magnetic foliations are associated with oblate shapes of the susceptibility ellipsoids and higher degree of anisotropy, passing inward into weaker triaxial to prolate fabric. By contrast, magnetic fabric in an inner granite unit is in places oriented at a high angle to internal contacts and is interpreted as recording an internal diapir circulation. We use inverse modeling to calculate strain variations across the diapir from the AMS data. The magnetic fabric parameters and calculated strains are in agreement with strain distribution in heads of model Newtonian diapirs traveling a distance of two body radii and suggest granitic magma ascent as a crystal-poor suspension followed by crystallization of fabric markers and their response to strain near the final emplacement level. The intrusive fabric thus formed late but, though generally weak, was still capable of recording incremental strain gradient in the granite diapir. (C) 2014 Elsevier Ltd. All rights reserved.
dcterms:title
Magnetic fabric and modeled strain distribution in the head of a nested granite diapir, the Melechov pluton, Bohemian Massif Magnetic fabric and modeled strain distribution in the head of a nested granite diapir, the Melechov pluton, Bohemian Massif
skos:prefLabel
Magnetic fabric and modeled strain distribution in the head of a nested granite diapir, the Melechov pluton, Bohemian Massif Magnetic fabric and modeled strain distribution in the head of a nested granite diapir, the Melechov pluton, Bohemian Massif
skos:notation
RIV/00216208:11310/14:10281515!RIV15-MSM-11310___
n3:aktivita
n8:P n8:I
n3:aktivity
I, P(GAP210/11/1168)
n3:cisloPeriodika
Sep
n3:dodaniDat
n15:2015
n3:domaciTvurceVysledku
n14:7243111 n14:8387699 n14:3621413
n3:druhVysledku
n4:J
n3:duvernostUdaju
n19:S
n3:entitaPredkladatele
n5:predkladatel
n3:idSjednocenehoVysledku
26886
n3:idVysledku
RIV/00216208:11310/14:10281515
n3:jazykVysledku
n13:eng
n3:klicovaSlova
Strain; Granite; Fabric; Emplacement; Diapir; Anisotropy of magnetic susceptibility (AMS)
n3:klicoveSlovo
n6:Strain n6:Diapir n6:Granite n6:Fabric n6:Emplacement n6:Anisotropy%20of%20magnetic%20susceptibility%20%28AMS%29
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[2772A743A5E0]
n3:nazevZdroje
Journal of Structural Geology
n3:obor
n9:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
4
n3:projekt
n20:GAP210%2F11%2F1168
n3:rokUplatneniVysledku
n15:2014
n3:svazekPeriodika
66
n3:tvurceVysledku
Žák, Jiří Trubač, Jakub Janoušek, Vojtěch Chlupáčová, Marta
n3:wos
000340978000018
s:issn
0191-8141
s:numberOfPages
13
n17:doi
10.1016/j.jsg.2014.05.015
n7:organizacniJednotka
11310