Intrusive and deformation history of the Sevetin Pluton, Moldanubian Batholith: record of polyphase tectonic evolution of the Blanice Graben, Bohemian Massif
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10284557" target="_blank" >RIV/00216208:11310/14:10284557 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.3190/jgeosci.175" target="_blank" >http://dx.doi.org/10.3190/jgeosci.175</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3190/jgeosci.175" target="_blank" >10.3190/jgeosci.175</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Intrusive and deformation history of the Sevetin Pluton, Moldanubian Batholith: record of polyphase tectonic evolution of the Blanice Graben, Bohemian Massif
Popis výsledku v původním jazyce
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 Blanic
Název v anglickém jazyce
Intrusive and deformation history of the Sevetin Pluton, Moldanubian Batholith: record of polyphase tectonic evolution of the Blanice Graben, Bohemian Massif
Popis výsledku anglicky
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 Blanic
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Journal of Geosciences
ISSN
1802-6222
e-ISSN
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Svazek periodika
59
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
16
Strana od-do
441-456
Kód UT WoS článku
000346149500009
EID výsledku v databázi Scopus
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