Thrust tectonics of the Upper Jurassic limestones in the Pavlov
Hills (Outer Western Carpathians, Czech Republic)

J 2011

Thrust tectonics of the Upper Jurassic limestones in the Pavlov Hills (Outer Western Carpathians, Czech Republic)

POUL, Ivan; Rostislav MELICHAR a Jiri JANECKA

Základní údaje

Originální název

Thrust tectonics of the Upper Jurassic limestones in the Pavlov Hills (Outer Western Carpathians, Czech Republic)

Autoři

POUL, Ivan; Rostislav MELICHAR a Jiri JANECKA

Vydání

KINEMATIC EVOLUTION AND STRUCTURAL STYLES OF FOLD-AND-THRUST BELTS, BATH, GEOLOGICAL SOC PUBLISHING HOUSE, 2011, 0305-8719

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10505 Geology

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Označené pro přenos do RIV

Ano

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

GEOMETRY

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 29. 6. 2020 11:41, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

The Pavlov Hills are formed by separated limestone blocks previously identified as klippen. A new flat-ramp-flat thrust model of the Pavlov Hills is formulated in this paper. The main tectonic detachment is located at the base of the limestone plate and other subsidiary detachments are located within the nodular limestone horizon and also at the base and top of the Upper Cretaceous deposits. The ramps are situated in the Klentnice Fm and Ernstbrunn Lst. The ramp angle was determined by structural evidence combined with interpretation of seismic profiles. Two parallel antiformal structures plunging to the NE are recognized within the study area. The antiformal fold axes are gently plunging to the NE so the anticlines are not ideal for 3-point hydrocarbon trap setting. These anticlines were subsequently cut by sinistral strike-slip faults perpendicular to the fold axis which resulted in the formation of a large-scale pseudo en-echelon structure in an approximate north-south direction.

Citovat

POUL, Ivan; Rostislav MELICHAR a Jiri JANECKA. Thrust tectonics of the Upper Jurassic limestones in the Pavlov Hills (Outer Western Carpathians, Czech Republic). KINEMATIC EVOLUTION AND STRUCTURAL STYLES OF FOLD-AND-THRUST BELTS. BATH: GEOLOGICAL SOC PUBLISHING HOUSE, 2011, roč. 349, č. 2011, s. 237-248. ISSN 0305-8719. Dostupné z: https://doi.org/10.1144/SP349.13.

@article{1668281,
   author = {Poul, Ivan and Melichar, Rostislav and Janecka, Jiri},
   article_location = {BATH},
   article_number = {2011},
   doi = {https://doi.org/10.1144/SP349.13},
   keywords = {GEOMETRY},
   language = {eng},
   issn = {0305-8719},
   journal = {KINEMATIC EVOLUTION AND STRUCTURAL STYLES OF FOLD-AND-THRUST BELTS},
   title = {Thrust tectonics of the Upper Jurassic limestones in the Pavlov Hills (Outer Western Carpathians, Czech Republic)},
   url = {https://sp.lyellcollection.org/content/349/1/237},
   volume = {349},
   year = {2011}
}

TY  - JOUR
ID  - 1668281
AU  - Poul, Ivan - Melichar, Rostislav - Janecka, Jiri
PY  - 2011
TI  - Thrust tectonics of the Upper Jurassic limestones in the Pavlov Hills (Outer Western Carpathians, Czech Republic)
JF  - KINEMATIC EVOLUTION AND STRUCTURAL STYLES OF FOLD-AND-THRUST BELTS
VL  - 349
IS  - 2011
SP  - 237-248
EP  - 237-248
PB  - GEOLOGICAL SOC PUBLISHING HOUSE
SN  - 03058719
KW  - GEOMETRY
UR  - https://sp.lyellcollection.org/content/349/1/237
L2  - https://sp.lyellcollection.org/content/349/1/237
N2  - The Pavlov Hills are formed by separated limestone blocks previously identified as klippen. A new flat-ramp-flat thrust model of the Pavlov Hills is formulated in this paper. The main tectonic detachment is located at the base of the limestone plate and other subsidiary detachments are located within the nodular limestone horizon and also at the base and top of the Upper Cretaceous deposits. The ramps are situated in the Klentnice Fm and Ernstbrunn Lst. The ramp angle was determined by structural evidence combined with interpretation of seismic profiles. Two parallel antiformal structures plunging to the NE are recognized within the study area. The antiformal fold axes are gently plunging to the NE so the anticlines are not ideal for 3-point hydrocarbon trap setting. These anticlines were subsequently cut by sinistral strike-slip faults perpendicular to the fold axis which resulted in the formation of a large-scale pseudo en-echelon structure in an approximate north-south direction.
ER  -

POUL, Ivan; Rostislav MELICHAR a Jiri JANECKA. Thrust tectonics of the Upper Jurassic limestones in the Pavlov Hills (Outer Western Carpathians, Czech Republic). \textit{KINEMATIC EVOLUTION AND STRUCTURAL STYLES OF FOLD-AND-THRUST BELTS}. BATH: GEOLOGICAL SOC PUBLISHING HOUSE, 2011, roč.~349, č.~2011, s.~237-248. ISSN~0305-8719. Dostupné z: https://doi.org/10.1144/SP349.13.

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