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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10284557%21RIV15-MSM-11310___
rdf:type
n15:Vysledek skos:Concept
rdfs:seeAlso
http://dx.doi.org/10.3190/jgeosci.175
dcterms:description
The Sevetin Pluton, located c. 15 km NNE of Ceske Budejovice, is a small, isolated, petrologically and structurally complex intrusive body that is genetically related to the youngest intrusions of the Moldanubian Batholith. As documented in this study, its overall shape, internal magmatic fabric as well as brittle structures (dikes, veins, joints, faults) are, however, related to the formation and polyphase tectonic evolution of the Blanice Graben, an about 200 km long and 5-15 km wide NNE-SSW-trending, deep-seated fault zone that cuts across the Moldanubian Unit. In total, one pre-intrusive and three syn- to post-intrusive tectonic phases have been distinguished. The oblique, NW-SE oriented compression controlled both the intrusion of the Sevetin biotite-muscovite granite and the early stage of its brittle deformation. Sigmoidal pattern of magnetic foliations in this pluton documents its mostly solid-state deformation during oblique sinistral movements on the main faults of the Blanice Graben. The subsequent strike-slip phase was characterized by E-W oriented subhorizontal extension and can be correlated with the intrusion of c. 270 Ma old microgranodiorite dikes. The last extensional phase was associated with the formation of subeconomic Pb-Zn-(Ag?) quartz-calcite veins at c. 265 Ma. The Sevetin Pluton, located c. 15 km NNE of Ceske Budejovice, is a small, isolated, petrologically and structurally complex intrusive body that is genetically related to the youngest intrusions of the Moldanubian Batholith. As documented in this study, its overall shape, internal magmatic fabric as well as brittle structures (dikes, veins, joints, faults) are, however, related to the formation and polyphase tectonic evolution of the Blanice Graben, an about 200 km long and 5-15 km wide NNE-SSW-trending, deep-seated fault zone that cuts across the Moldanubian Unit. In total, one pre-intrusive and three syn- to post-intrusive tectonic phases have been distinguished. The oblique, NW-SE oriented compression controlled both the intrusion of the Sevetin biotite-muscovite granite and the early stage of its brittle deformation. Sigmoidal pattern of magnetic foliations in this pluton documents its mostly solid-state deformation during oblique sinistral movements on the main faults of the Blanice Graben. The subsequent strike-slip phase was characterized by E-W oriented subhorizontal extension and can be correlated with the intrusion of c. 270 Ma old microgranodiorite dikes. The last extensional phase was associated with the formation of subeconomic Pb-Zn-(Ag?) quartz-calcite veins at c. 265 Ma.
dcterms:title
Intrusive and deformation history of the Sevetin Pluton, Moldanubian Batholith: record of polyphase tectonic evolution of the Blanice Graben, Bohemian Massif Intrusive and deformation history of the Sevetin Pluton, Moldanubian Batholith: record of polyphase tectonic evolution of the Blanice Graben, Bohemian Massif
skos:prefLabel
Intrusive and deformation history of the Sevetin Pluton, Moldanubian Batholith: record of polyphase tectonic evolution of the Blanice Graben, Bohemian Massif Intrusive and deformation history of the Sevetin Pluton, Moldanubian Batholith: record of polyphase tectonic evolution of the Blanice Graben, Bohemian Massif
skos:notation
RIV/00216208:11310/14:10284557!RIV15-MSM-11310___
n4:aktivita
n9:S n9:I
n4:aktivity
I, S
n4:cisloPeriodika
4
n4:dodaniDat
n17:2015
n4:domaciTvurceVysledku
n12:6360386
n4:druhVysledku
n10:J
n4:duvernostUdaju
n13:S
n4:entitaPredkladatele
n18:predkladatel
n4:idSjednocenehoVysledku
22659
n4:idVysledku
RIV/00216208:11310/14:10284557
n4:jazykVysledku
n5:eng
n4:klicovaSlova
Pb-Zn veins; AMS study; paleostress analysis; Blanice Graben; Moldanubian Batholith; Moldanubian Zone
n4:klicoveSlovo
n14:paleostress%20analysis n14:Moldanubian%20Batholith n14:Blanice%20Graben n14:Pb-Zn%20veins n14:AMS%20study n14:Moldanubian%20Zone
n4:kodStatuVydavatele
CZ - Česká republika
n4:kontrolniKodProRIV
[673EA1EBB48B]
n4:nazevZdroje
Journal of Geosciences
n4:obor
n8:DB
n4:pocetDomacichTvurcuVysledku
1
n4:pocetTvurcuVysledku
2
n4:rokUplatneniVysledku
n17:2014
n4:svazekPeriodika
59
n4:tvurceVysledku
Zachariáš, Jiří Trubac, Jakub
n4:wos
000346149500009
s:issn
1802-6222
s:numberOfPages
16
n16:doi
10.3190/jgeosci.175
n3:organizacniJednotka
11310