Lateral development of coalification in the Czech part of the Upper Silesian Coal Basin and its connection with gas deposits
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F09%3A00021752" target="_blank" >RIV/61989100:27350/09:00021752 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Lateral development of coalification in the Czech part of the Upper Silesian Coal Basin and its connection with gas deposits
Popis výsledku v původním jazyce
The degree of coalification is an essential parameter influencing the quality of coal reserves. Modelling of the development of this parameter in the Czech part of the Upper Silesian Coal Basin (Carboniferous, Mississippian to Pennsylvanian ? Lower Namurian to Westphalian A) revealed the distribution of coalification within the basin in all its stratal units. The grade of coalification was found in principle to be similar but its intensity in general decreases upwards into the hanging wall. Because of different areal extents of individual stratal units the degree of coalification is demonstrated on the oldest and areally most extensive unit ? the Petřkovice Member. The studies and their results presented in this paper are based on more than 29,000 analyses of the moisture- and ash-free volatile matter (Vdaf) in coal samples from surface and underground boreholes drilled in the years 1946 ? 2000. Three zones of enhanced coalification were distinguished: the Ostrava-Příbor Zone, the Rožn
Název v anglickém jazyce
Lateral development of coalification in the Czech part of the Upper Silesian Coal Basin and its connection with gas deposits
Popis výsledku anglicky
The degree of coalification is an essential parameter influencing the quality of coal reserves. Modelling of the development of this parameter in the Czech part of the Upper Silesian Coal Basin (Carboniferous, Mississippian to Pennsylvanian ? Lower Namurian to Westphalian A) revealed the distribution of coalification within the basin in all its stratal units. The grade of coalification was found in principle to be similar but its intensity in general decreases upwards into the hanging wall. Because of different areal extents of individual stratal units the degree of coalification is demonstrated on the oldest and areally most extensive unit ? the Petřkovice Member. The studies and their results presented in this paper are based on more than 29,000 analyses of the moisture- and ash-free volatile matter (Vdaf) in coal samples from surface and underground boreholes drilled in the years 1946 ? 2000. Three zones of enhanced coalification were distinguished: the Ostrava-Příbor Zone, the Rožn
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
V - Vyzkumna aktivita podporovana z jinych verejnych zdroju
Ostatní
Rok uplatnění
2009
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
International Journal of Coal Geology
ISSN
0166-5162
e-ISSN
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Svazek periodika
78
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
8
Strana od-do
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Kód UT WoS článku
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EID výsledku v databázi Scopus
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