"3"^^ . . . "S" . "Vebr, Luk\u00E1\u0161" . . . "Thickness of the Lower Hru\u0161ov Member (Namurian) in the Czech Part of the Upper Silesian Basin"@en . . . "RIV/61989100:27350/12:86082914" . "Thickness of the Lower Hru\u0161ov Member (Namurian) in the Czech Part of the Upper Silesian Basin"@en . "Mocnost spodn\u00EDch hru\u0161ovsk\u00FDch vrstev (namur) v \u010Desk\u00E9 \u010D\u00E1sti hornoslezsk\u00E9 p\u00E1nve" . "27350" . "RIV/61989100:27350/12:86082914!RIV13-MSM-27350___" . "Jir\u00E1sek, Jakub" . "1-2" . "Mocnost spodn\u00EDch hru\u0161ovsk\u00FDch vrstev (namur) v \u010Desk\u00E9 \u010D\u00E1sti hornoslezsk\u00E9 p\u00E1nve" . . . "Sivek, Martin" . "Mocnost spodn\u00EDch hru\u0161ovsk\u00FDch vrstev (namur) v \u010Desk\u00E9 \u010D\u00E1sti hornoslezsk\u00E9 p\u00E1nve"@cs . . "Byla vytvo\u0159ena mapa mocnosti spodn\u00EDch hru\u0161ovsk\u00FDch vrstev (namur, mississipp). Je zalo\u017Eena na profilech pr\u016Fzkumn\u00FDch vrt\u016F z \u010Desk\u00E9 \u010D\u00E1sti hornoslezsk\u00E9 p\u00E1nve. Mocnost se pohybuje v rozmez\u00ED 52.55 m to 415.48 m. Nejvy\u0161\u0161\u00ED hodnoty se nach\u00E1zej\u00ED v SSV-JJZ prota\u017Een\u00E9 z\u00F3n\u011B z\u00E1padn\u011B od orlovsk\u00E9 struktury v severn\u00ED \u010D\u00E1sti p\u0159\u00EDborsk\u00E9 oblasti a v z\u00E1padn\u00ED \u010D\u00E1sti ostravsk\u00E9 oblasti. Nejni\u017E\u0161\u00ED hodnoty jsou ve fren\u0161t\u00E1tsk\u00E9 oblasti v\u00FDchodn\u011B od kozlovick\u00E9ho sedla, v mo\u0159kovsk\u00E9 oblasti ji\u017En\u011B od janovick\u00E9ho zlomu a z\u00E1padn\u011B od kozlovick\u00E9ho sedla a v t\u011B\u0161\u00EDnsk\u00E9 a karvinsk\u00E9 oblasti v\u00FDchodn\u011B od orlovsk\u00E9 struktury. Celkov\u00E1 mocnost spodn\u00EDch hru\u0161ovsk\u00FDch vrstev se sni\u017Euje od z\u00E1padu k v\u00FDchodu a m\u00E1 z\u0159ejmou z\u00E1pado-v\u00FDchodn\u00ED polaritu. Z\u00E1padn\u00ED \u010D\u00E1st post-erozivn\u00EDho v\u00FDskytu spodn\u00EDch hru\u0161ovsk\u00FDch vrstev p\u0159edstavuje osu maxim\u00E1ln\u00ED subsidence p\u00E1nve v dob\u011B sedimentace vrstevn\u00ED jednotky. Z\u00F3na redukovan\u00FDch mocnost\u00ED je p\u016Fvodn\u00ED v\u00FDchodn\u00ED \u010D\u00E1st p\u00E1nve. P\u016Fvodn\u00ED z\u00E1padn\u00ED \u010D\u00E1st se z d\u016Fvod\u016F pokarbonsk\u00E9 eroze nedochovala." . . . "Mocnost spodn\u00EDch hru\u0161ovsk\u00FDch vrstev (namur) v \u010Desk\u00E9 \u010D\u00E1sti hornoslezsk\u00E9 p\u00E1nve"@cs . . . "Byla vytvo\u0159ena mapa mocnosti spodn\u00EDch hru\u0161ovsk\u00FDch vrstev (namur, mississipp). Je zalo\u017Eena na profilech pr\u016Fzkumn\u00FDch vrt\u016F z \u010Desk\u00E9 \u010D\u00E1sti hornoslezsk\u00E9 p\u00E1nve. Mocnost se pohybuje v rozmez\u00ED 52.55 m to 415.48 m. Nejvy\u0161\u0161\u00ED hodnoty se nach\u00E1zej\u00ED v SSV-JJZ prota\u017Een\u00E9 z\u00F3n\u011B z\u00E1padn\u011B od orlovsk\u00E9 struktury v severn\u00ED \u010D\u00E1sti p\u0159\u00EDborsk\u00E9 oblasti a v z\u00E1padn\u00ED \u010D\u00E1sti ostravsk\u00E9 oblasti. Nejni\u017E\u0161\u00ED hodnoty jsou ve fren\u0161t\u00E1tsk\u00E9 oblasti v\u00FDchodn\u011B od kozlovick\u00E9ho sedla, v mo\u0159kovsk\u00E9 oblasti ji\u017En\u011B od janovick\u00E9ho zlomu a z\u00E1padn\u011B od kozlovick\u00E9ho sedla a v t\u011B\u0161\u00EDnsk\u00E9 a karvinsk\u00E9 oblasti v\u00FDchodn\u011B od orlovsk\u00E9 struktury. Celkov\u00E1 mocnost spodn\u00EDch hru\u0161ovsk\u00FDch vrstev se sni\u017Euje od z\u00E1padu k v\u00FDchodu a m\u00E1 z\u0159ejmou z\u00E1pado-v\u00FDchodn\u00ED polaritu. Z\u00E1padn\u00ED \u010D\u00E1st post-erozivn\u00EDho v\u00FDskytu spodn\u00EDch hru\u0161ovsk\u00FDch vrstev p\u0159edstavuje osu maxim\u00E1ln\u00ED subsidence p\u00E1nve v dob\u011B sedimentace vrstevn\u00ED jednotky. Z\u00F3na redukovan\u00FDch mocnost\u00ED je p\u016Fvodn\u00ED v\u00FDchodn\u00ED \u010D\u00E1st p\u00E1nve. P\u016Fvodn\u00ED z\u00E1padn\u00ED \u010D\u00E1st se z d\u016Fvod\u016F pokarbonsk\u00E9 eroze nedochovala."@cs . "150875" . "Computer Modelling; Thickness; Ostrava Formation; Mississippian"@en . "Geologick\u00E9 v\u00FDzkumy na Morav\u011B a Slezsku" . "[6CEC9E01A4AC]" . . "CZ - \u010Cesk\u00E1 republika" . "H\u00FDlov\u00E1, Lada" . "19" . . "4"^^ . . . "1212-6209" . "3"^^ . . "Map of the thickness of the Lower Hru\u0161ov Member (Namurian, Mississippian) was made. It is based on exploratory boreholes\u00B4 information from the Czech part of the Upper Silesian Basin. The thickness varies from 52.55 m to 415.48 m. The highest values are situated in a NNE\u2013SSW rending zone west of the Orlov\u00E1 Structure in the northern part of the P\u0159\u00EDbor area and in the western part of the Ostrava area. The lowest values are reached in the Fren\u0161t\u00E1t area east of the Kozlovice Saddle, in the Mo\u0159kov area south of the Janovice Fault and west of the Kozlovice Saddle, and in the T\u011B\u0161\u00EDn and Karvin\u00E1 areas east of the Orlov\u00E1 Structure. Total thickness of the Lower Hru\u0161ov Member is decreasing from the West to the East and shows evident west-east polarity. The western part of the post-erosive area of the Lower Hru\u0161ov Member represents the axis of maximum subsidence of the basin in times of sedimentation. The zone of reduced thickness is the original eastern part of the basin. The western part of the basin is not preserved due to the post-Carboniferous erosion."@en .