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作者:Stanislav Opluštil , Ivana Sýkorová
来源:[J].International Journal of Coal Geology(IF 2.976), 2018
摘要:... 40), the erosional remnant of which covers about 5000 km 2 , is the thickest seam of the Upper Silesian Basin situated along the Czech – Polish border. This basin-wide coal is unusual in its thickness and high inertinite and very low ash contents. In the Czech sector, thi...
作者:Lada Hýlová , Janusz Jureczka , Jakub Jirásek ...
来源:[J].International Journal of Coal Geology(IF 2.976), 2013, Vol.106, pp.11-24
摘要:Abstract(#br)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 Czech part or as...
作者:Zbyněk Šimůnek , Sławomir Florjan
来源:[J].Review of Palaeobotany and Palynology(IF 1.933), 2013, Vol.197, pp.26-49
摘要:Abstract(#br)Cordaitalean cuticles represent a great deal of the dispersed cuticular assemblages obtained from coal seams of the Upper Silesian Basin. Cordaitalean cuticles are easy to distinguish having stomatal complexes mostly with two polar and two lateral subsidiary cells. ...
作者:Jiří Bek
来源:[J].Review of Palaeobotany and Palynology(IF 1.933), 2008, Vol.152 (1), pp.40-57
摘要:Abstract(#br)Palynological samples from thirty-four boreholes drilled in the Bohemian part of the Upper Silesian Basin in the Czech Republic during more than last fifty years were examined. Coal samples from the Ostrava (Jaklovec and Poruba members) and Karviná (Saddle, Lower a...
作者:Zuzana Weishauptová , Ivana Sýkorová
来源:[J].Fuel(IF 3.357), 2010, Vol.90 (1), pp.312-323
摘要:Abstract(#br)The effect of the rank and of the maceral composition of bituminous coal on carbon dioxide sorption capacity was studied on the basis of samples from two coal mines (Darkov, ČSM) from the Czech part of the Upper Silesian Basin. The samples from the two mines co...
作者:Jakub Jirásek , Stanislav Opluštil , Martin Sivek ...
来源:[J].Earth-Science Reviews(IF 7.339), 2018, Vol.177, pp.715-741
摘要:Abstract(#br)The ~ 3-km-thick Ostrava Formation in the foreland Upper Silesian Basin, which is located along the Czech-Polish border, provides the thickest and most complete record of mixed shallow-marine to continental sediments of Serpukhovian (Carboniferous) age in the former ...
作者:Zbyněk Šimůnek
来源:[J].Review of Palaeobotany and Palynology(IF 1.933), 2018
摘要:... This assemblage comes from the coal seam 26 of the Karviná Formation, Lower Suchá Member, a few meters above the Namurian/Westphalian boundary in the Upper Silesian Basin. Cordaitaleans represent 23% of the cuticular assemblage, and consist of two species of abaxial cut...
作者:Marian Marschalko , Işık Yilmaz , Veronika Křístková ...
来源:[J].Engineering Geology(IF 1.403), 2011, Vol.124, pp.130-138
摘要:Abstract(#br)This study deals with the determination of the actual limit angles in the long-term formed subsidence basin in the Czech part of the Upper Silesian Basin (the remaining part lays in Poland). Here there was the most extensive underground exploitation of black coal...
作者:V. Hudeček , J. Šancer , V. Zubíček ...
来源:[J].Journal of Mining Science(IF 0.223), 2017, Vol.53 (1), pp.99-108
摘要:A significant quantity of available hard coal reserves in the area of Upper Silesian Basin in the Czech Republic occurs below the areas where surface mine subsidence is unacceptable or may be only minimal. An effort is made to mine these reserves by means of a new, mining me...
作者:D. Matýsek , J. Jirásek , M. Osovský ...
来源:[J].Mineralogical Magazine(IF 2.212), 2015, Vol.78 (5), pp.1265-1286
摘要:Abstract This study describes the occurrences of sulfate minerals in mines of the Czech part of the Upper Silesian Basin. This mineralization originates from the oxidation of Fe disulfides contained in the coal matrix and enclosing sediments. The oxidation occurs in the pres...

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