Orientations of paleostresses in the Jurassic limestones on the
front of the West Carpathian flysch nappes (Pavlov Hills, South
Moravia)

J 2003

Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia)

HAVÍŘ, Josef a Zdeněk STRÁNÍK

Základní údaje

Originální název

Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia)

Autoři

HAVÍŘ, Josef a Zdeněk STRÁNÍK

Vydání

Geologica Carpathica, Bratislava, SAV, 2003, 1335-0552

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Slovensko

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 0.397

Označené pro přenos do RIV

Organizační jednotka

Přírodovědecká fakulta

UT WoS

000189225600006

Klíčová slova anglicky

Neogene; Outer Western Carpathians; Waschberg-Ždánice Belt; paleostresses

Štítky

Neogene, Outer Western Carpathians, paleostresses, Waschberg-Ždánice Belt

Změněno: 10. 2. 2004 14:01, Mgr. Josef Havíř, Dr.

Anotace

V originále

The paleostress analysis was applied at 16 sites in the Mesozoic limestones, which are tectonically incorporate into the Cretaceous and the Paleogene strata on the front of the Western Carpathian Flysch nappes (South Moravia, Czech Republic). 25 solutions were obtained. These solutions can be divided into two groups. First group represents the paleostress field with predominantly NW-SE compression and NE-SW extension connected with the Early Neogene movements of the Ždánice nappe. The azimuth of eigenvector of acceptable compression axes varies from 97 up to 167. This variability can be explained by rotation of individual tectonic slices of the Ždánice nappe during the movement this nappe. The different tectonic scales rotated probably in different sense (anticlockwise rotation in the case of some scales, clockwise rotation in the case of other scales). Second group of solutions represents the paleostress field with NE-SW compression and NW-SE extension.

Citovat

HAVÍŘ, Josef a Zdeněk STRÁNÍK. Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia). Geologica Carpathica. Bratislava: SAV, 2003, roč. 54, č. 6, s. 409-416. ISSN 1335-0552.

@article{492829,
   author = {Havíř, Josef and Stráník, Zdeněk},
   article_location = {Bratislava},
   article_number = {6},
   keywords = {Neogene; Outer Western Carpathians; Waschberg-Ždánice Belt; paleostresses},
   language = {eng},
   issn = {1335-0552},
   journal = {Geologica Carpathica},
   title = {Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia)},
   volume = {54},
   year = {2003}
}

TY  - JOUR
ID  - 492829
AU  - Havíř, Josef - Stráník, Zdeněk
PY  - 2003
TI  - Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia)
JF  - Geologica Carpathica
VL  - 54
IS  - 6
SP  - 409-416
EP  - 409-416
PB  - SAV
SN  - 13350552
KW  - Neogene
KW  - Outer Western Carpathians
KW  - Waschberg-Ždánice Belt
KW  - paleostresses
N2  - The paleostress analysis was applied at 16 sites in the Mesozoic limestones, which are tectonically incorporate into the Cretaceous and the Paleogene strata on the front of the Western Carpathian Flysch nappes (South Moravia, Czech Republic). 25 solutions were obtained. These solutions can be divided into two groups. First group represents the paleostress field with predominantly NW-SE compression and NE-SW extension connected with the Early Neogene movements of the Ždánice nappe. The azimuth of eigenvector of acceptable compression axes varies from 97 up to 167. This variability can be explained by rotation of individual tectonic slices of the Ždánice nappe during the movement this nappe. The different tectonic scales rotated probably in different sense (anticlockwise rotation in the case of some scales, clockwise rotation in the case of other scales). Second group of solutions represents the paleostress field with NE-SW compression and NW-SE extension.
ER  -

HAVÍŘ, Josef a Zdeněk STRÁNÍK. Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia). \textit{Geologica Carpathica}. Bratislava: SAV, 2003, roč.~54, č.~6, s.~409-416. ISSN~1335-0552.

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