National Repository of Grey Literature 5 records found  Search took 0.00 seconds. 
Geomorphological analysis and relief development of central part of Troskovická Highland
David, Daniel ; Balatka, Břetislav (advisor) ; Přibyl, Václav (referee)
David, D. (2010): Geomorphological analysis and development relief of central part in Troskovická vrchovina (Highland) (Bohemian Paradise). Charles University in Prague, Faculty of Sience, Department of Physical Geography and Geoecology. The central part of Troskovická vrchovina Highland lies between towns Turnov and Jičín in Jičínská pahorkatina (Hilly land) in Geopark Bohemian Paradise. It is a rugged rocky area mostly built of sedimetary rocks (Cretaceous quartz sandstones). The relief is cut by canyons and in the center of plateau is vulcanic neck Trosky. This book contains results of detailed geomorphological mapping and analysing of the area. The major product of this study is detailed geomorphological map 1:10 000. Key words: Bohemian Paradise, detailed geomorphological mapping, geomorphological analysis, Střeleč pit (main), sandstone relief, vulcanic rocks and Trosky neck.
Influence of composition and fabric of volcanic rocks on their technological properties
Krutilová, Kateřina
Because of a very variable geological composition of the Czech Republic, there is a various scale of all genetic types of rocks that are used for the production of crushed stone. The most often used group of rocks are effusive magmatic rocks, which represent about 34 % of crushed stone marketed (Starý et al. 2010). These rocks are used for all kinds of construction purposes including roads. The experimental material of crushed stone used in this thesis was sampled from 40 active quarries in the Czech Republic. The studied volcanic rocks originated from Neoproterozoic and Paleozoic complexes of Barrandien, Carboniferous and Permian of Krkonose Piedmont Basin, Carboniferous and Permian of Intrasudetic basin, area of ordovician Železné Hory, from the main volcanic center of Bohemian Massif in the north-west Bohemia (České středohoří Mts. and Doupov Mts.), Neovolcanic area of Czech Cretaceous basin and area of Neovolcanic East and West Sudeten. Petrographic study was carried out in a form of standard petrographic analysis of thin sections and chemical analysis, which helped inclusion of rocks to a classified systems. The whole suite of volcanic rocks was separated to five petrographic-technologic subgroups defined as: (1) rhyolites / porphyres, (2) phonolites, (3) basalts s.l., (4) spilites and (5)...
Influence of composition and fabric of volcanic rocks on their technological properties
Krutilová, Kateřina
Because of a very variable geological composition of the Czech Republic, there is a various scale of all genetic types of rocks that are used for the production of crushed stone. The most often used group of rocks are effusive magmatic rocks, which represent about 34 % of crushed stone marketed (Starý et al. 2010). These rocks are used for all kinds of construction purposes including roads. The experimental material of crushed stone used in this thesis was sampled from 40 active quarries in the Czech Republic. The studied volcanic rocks originated from Neoproterozoic and Paleozoic complexes of Barrandien, Carboniferous and Permian of Krkonose Piedmont Basin, Carboniferous and Permian of Intrasudetic basin, area of ordovician Železné Hory, from the main volcanic center of Bohemian Massif in the north-west Bohemia (České středohoří Mts. and Doupov Mts.), Neovolcanic area of Czech Cretaceous basin and area of Neovolcanic East and West Sudeten. Petrographic study was carried out in a form of standard petrographic analysis of thin sections and chemical analysis, which helped inclusion of rocks to a classified systems. The whole suite of volcanic rocks was separated to five petrographic-technologic subgroups defined as: (1) rhyolites / porphyres, (2) phonolites, (3) basalts s.l., (4) spilites and (5)...
Influence of composition and fabric of volcanic rocks on their technological properties
Krutilová, Kateřina ; Přikryl, Richard (advisor) ; Vavro, Martin (referee) ; Holzer, Rudolf (referee)
Because of a very variable geological composition of the Czech Republic, there is a various scale of all genetic types of rocks that are used for the production of crushed stone. The most often used group of rocks are effusive magmatic rocks, which represent about 34 % of crushed stone marketed (Starý et al. 2010). These rocks are used for all kinds of construction purposes including roads. The experimental material of crushed stone used in this thesis was sampled from 40 active quarries in the Czech Republic. The studied volcanic rocks originated from Neoproterozoic and Paleozoic complexes of Barrandien, Carboniferous and Permian of Krkonose Piedmont Basin, Carboniferous and Permian of Intrasudetic basin, area of ordovician Železné Hory, from the main volcanic center of Bohemian Massif in the north-west Bohemia (České středohoří Mts. and Doupov Mts.), Neovolcanic area of Czech Cretaceous basin and area of Neovolcanic East and West Sudeten. Petrographic study was carried out in a form of standard petrographic analysis of thin sections and chemical analysis, which helped inclusion of rocks to a classified systems. The whole suite of volcanic rocks was separated to five petrographic-technologic subgroups defined as: (1) rhyolites / porphyres, (2) phonolites, (3) basalts s.l., (4) spilites and (5)...
Geomorphological analysis and relief development of central part of Troskovická Highland
David, Daniel ; Balatka, Břetislav (advisor) ; Přibyl, Václav (referee)
David, D. (2010): Geomorphological analysis and development relief of central part in Troskovická vrchovina (Highland) (Bohemian Paradise). Charles University in Prague, Faculty of Sience, Department of Physical Geography and Geoecology. The central part of Troskovická vrchovina Highland lies between towns Turnov and Jičín in Jičínská pahorkatina (Hilly land) in Geopark Bohemian Paradise. It is a rugged rocky area mostly built of sedimetary rocks (Cretaceous quartz sandstones). The relief is cut by canyons and in the center of plateau is vulcanic neck Trosky. This book contains results of detailed geomorphological mapping and analysing of the area. The major product of this study is detailed geomorphological map 1:10 000. Key words: Bohemian Paradise, detailed geomorphological mapping, geomorphological analysis, Střeleč pit (main), sandstone relief, vulcanic rocks and Trosky neck.

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