New Knowledge of the Development of the Petřkovice Member in the South of the Czech Part of the Upper Silesian Basin (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F09%3A00021747" target="_blank" >RIV/61989100:27350/09:00021747 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

New Knowledge of the Development of the Petřkovice Member in the South of the Czech Part of the Upper Silesian Basin (Czech Republic)

Popis výsledku v původním jazyce

Modelling of the development of thickness of the Petřkovice Member and its partial sequences in the south of the Czech part of the Upper Silesian Coal Basin brought interesting information about the character of spatial development of this unit of strata. It has been found that the east-west polarity (characteristic of the development of all strata units of the Ostrava Formation) began to manifest itself in the development of the Petřkovice Member as late as the period of sedimentation of the upper partof the Petřkovice Member. The development of thicknesses of the lower part of the Petřkovice Member has the insular character that indicates spatial variability in sedimentation. The sedimentation of the lower part of the Petřkovice Member has thus retained the spatial development of thicknesses typical for this area, e.g. in the period of sedimentation of basal clastics of Devonian age and of clastic-carbonate formation of Early Carboniferous age. This information has helped us to comp

Název v anglickém jazyce

New Knowledge of the Development of the Petřkovice Member in the South of the Czech Part of the Upper Silesian Basin (Czech Republic)

Popis výsledku anglicky

Modelling of the development of thickness of the Petřkovice Member and its partial sequences in the south of the Czech part of the Upper Silesian Coal Basin brought interesting information about the character of spatial development of this unit of strata. It has been found that the east-west polarity (characteristic of the development of all strata units of the Ostrava Formation) began to manifest itself in the development of the Petřkovice Member as late as the period of sedimentation of the upper partof the Petřkovice Member. The development of thicknesses of the lower part of the Petřkovice Member has the insular character that indicates spatial variability in sedimentation. The sedimentation of the lower part of the Petřkovice Member has thus retained the spatial development of thicknesses typical for this area, e.g. in the period of sedimentation of basal clastics of Devonian age and of clastic-carbonate formation of Early Carboniferous age. This information has helped us to comp

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2009

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

GeoLines

ISSN

1210-9606

e-ISSN

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Svazek periodika

22

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

7

Strana od-do

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Kód UT WoS článku

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EID výsledku v databázi Scopus

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