Polyphase deformation of the Variscan accretionary wedge: an
example from the southern part of the Moravian Karst (Bohemian
Massif, Czech Republic)

J 2011

Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic)

REZ, Jiří, Rostislav MELICHAR a Jiří KALVODA

Základní údaje

Originální název

Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic)

Autoři

REZ, Jiří (203 Česká republika, domácí), Rostislav MELICHAR (203 Česká republika, garant, domácí) a Jiří KALVODA (203 Česká republika, domácí)

Vydání

Geological Society, London, Special Publications, London, Geological Society, London, 2011, 0305-8719

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Kód RIV

RIV/00216224:14310/11:00064409

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1144/SP349.12

UT WoS

000288800900012

Klíčová slova česky

deformation geology Moravia Karst

Klíčová slova anglicky

deformation geology Moravia Karst

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 24. 6. 2020 09:19, Mgr. Marie Šípková, DiS.

Anotace

V originále

The presence of two different coeval pre-flysch carbonate facies juxtaposed in numerous profiles in the southern part of the Moravian Karst proves that the Variscan nappe tectonics affected the pre-flysch basement of the main Culmian flysch nappes. Two main thrust events were recognized: (1) a ‘thin-skinned’ event, during which two sedimentary facies were juxtaposed along bedding sub-parallel thrusts, and (2) a ‘thick-skinned’ event, which generated younger thrusts oblique to bedding, involved crystalline rocks of the Brno Massif, and resulted in refolding of the older thrusts.

Návaznosti

MSM0021622412, záměr

Název: Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální, regionální a lokální úrovni (INCHEMBIOL) (Akronym: INCHEMBIOL)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální , regionální a lokální úrovni

Citovat

REZ, Jiří, Rostislav MELICHAR a Jiří KALVODA. Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic). Geological Society, London, Special Publications. London: Geological Society, London, 2011, roč. 349, č. 2011, s. 223-235. ISSN 0305-8719. Dostupné z: https://dx.doi.org/10.1144/SP349.12.

@article{1092090,
   author = {Rez, Jiří and Melichar, Rostislav and Kalvoda, Jiří},
   article_location = {London},
   article_number = {2011},
   doi = {http://dx.doi.org/10.1144/SP349.12},
   keywords = {deformation geology Moravia Karst},
   language = {eng},
   issn = {0305-8719},
   journal = {Geological Society, London, Special Publications},
   title = {Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic)},
   url = {http://dx.doi.org/10.1144/SP349.12},
   volume = {349},
   year = {2011}
}

TY  - JOUR
ID  - 1092090
AU  - Rez, Jiří - Melichar, Rostislav - Kalvoda, Jiří
PY  - 2011
TI  - Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic)
JF  - Geological Society, London, Special Publications
VL  - 349
IS  - 2011
SP  - 223-235
EP  - 223-235
PB  - Geological Society, London
SN  - 03058719
KW  - deformation geology Moravia Karst
UR  - http://dx.doi.org/10.1144/SP349.12
L2  - http://dx.doi.org/10.1144/SP349.12
N2  - The presence of two different coeval pre-flysch carbonate facies juxtaposed in numerous profiles in the southern part of the Moravian Karst proves that the Variscan nappe tectonics affected the pre-flysch basement of the main Culmian flysch nappes. Two main thrust events were recognized: (1) a ‘thin-skinned’ event, during which two sedimentary facies were juxtaposed along bedding sub-parallel thrusts, and (2) a ‘thick-skinned’ event, which generated younger thrusts oblique to bedding, involved crystalline rocks of the Brno Massif, and resulted in refolding of the older thrusts.
ER  -

REZ, Jiří, Rostislav MELICHAR a Jiří KALVODA. Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic). \textit{Geological Society, London, Special Publications}. London: Geological Society, London, 2011, roč.~349, č.~2011, s.~223-235. ISSN~0305-8719. Dostupné z: https://dx.doi.org/10.1144/SP349.12.

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