The Petřkovice Member (Ostrava Formation, Mississippian) of the Upper Silesian Basin (Czech Republic and Poland)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F13%3A33147774" target="_blank" >RIV/61989592:15310/13:33147774 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61989100:27350/13:86088162

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.coal.2013.01.004" target="_blank" >http://dx.doi.org/10.1016/j.coal.2013.01.004</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.coal.2013.01.004" target="_blank" >10.1016/j.coal.2013.01.004</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The Petřkovice Member (Ostrava Formation, Mississippian) of the Upper Silesian Basin (Czech Republic and Poland)

Popis výsledku v původním jazyce

The Petřkovice Member (Carboniferous, Mississippian, Early Namurian) is in many ways the most interesting lithostratigraphic unit of the paralic part of the Carboniferous coal-bearing Upper Silesian Basin (described as the Ostrava Formation in the Czechpart or as the Paralic Series in the Polish part). Petřkovice Member represents a transition between the non-coal-bearing Carboniferous flysch sedimentation of the Moravian-Silesian Basin and the coal-bearing sedimentation of the Upper Silesian Basin. The paper includes maps of the basic sedimentological parameters of this unit - thickness, sand content and coal-bearing capacity. The thickness of the Petřkovice Member ranges from approximately 50 m in the east of the basin to around 770 m in the west and has a clear polarity in the NNW-SSE direction. Sand content ranges from 23% in the west of the basin to more than 90% in the east. Its polarity is approximately the same as its thickness. The greatest coal-bearing capacity, expressed as

Název v anglickém jazyce

The Petřkovice Member (Ostrava Formation, Mississippian) of the Upper Silesian Basin (Czech Republic and Poland)

Popis výsledku anglicky

The Petřkovice Member (Carboniferous, Mississippian, Early Namurian) is in many ways the most interesting lithostratigraphic unit of the paralic part of the Carboniferous coal-bearing Upper Silesian Basin (described as the Ostrava Formation in the Czechpart or as the Paralic Series in the Polish part). Petřkovice Member represents a transition between the non-coal-bearing Carboniferous flysch sedimentation of the Moravian-Silesian Basin and the coal-bearing sedimentation of the Upper Silesian Basin. The paper includes maps of the basic sedimentological parameters of this unit - thickness, sand content and coal-bearing capacity. The thickness of the Petřkovice Member ranges from approximately 50 m in the east of the basin to around 770 m in the west and has a clear polarity in the NNW-SSE direction. Sand content ranges from 23% in the west of the basin to more than 90% in the east. Its polarity is approximately the same as its thickness. The greatest coal-bearing capacity, expressed as

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

2013

Kód důvěrnosti údajů

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

Název periodika

International Journal of Coal Geology

ISSN

0166-5162

e-ISSN

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Svazek periodika

106

Číslo periodika v rámci svazku

FEB

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

14

Strana od-do

11-24

Kód UT WoS článku

000316436500002

EID výsledku v databázi Scopus

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