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National Repository of Grey Literature 2 records found  Search took 0.00 seconds. 
Klikov Formation in a newly localized landslide area near České Budějovice
 Pilařová, Eliška ; Jerman, Jan (advisor) ; Mužík, Vlastimil (referee)
Diploma thesis is focused on obtaining new knowledge about the Klikov Formation of the České Budějovice Tertiary Basin during the extraordinary opportunity of construction a section of the D3 highway at the southern edge of České Budějovice near the villages of Roudné and Včelná. The location is also interesting because of newly detected landslide. The route of the highway is designed in large side-hill cut. The cut reached a total height of up to 20 m and was mainly carried out in the soft rock of the Klikov Formation, while vertical rock slopes up to several meters high remained without any stabilization during excavation. This made it possible to examine the soft rock of Klikov Formation in various aspects, e.g. stability, structural properties, properties of the rock material itself, etc. The text is divided into two parts. The first part describes construction works during the excavation of side cut, and the second to laboratory tests. The diploma thesis presents the connection between field observation and laboratory results.
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Low sinuosity rivers with example of sediments of klikov formation from locality Hosín-Orty, Late Crataceous, České Budějovice basin
 Kavková, Radana ; Martínek, Karel (advisor) ; Opluštil, Stanislav (referee)
The literature research part of this bachelors thesis is devoted to the definition of river styles, namely to those with low sinuosity. The aim was the description of types of deposits and diagnostic features of these rivers. Available literature, especially scientific papers devoted to fluvial sedimetology served as the sources of information for this study. Summarization of processes and products of these river styles and definition of different approaches to their study were achieved. Practical part of the thesis explores the fluvial style in Hosín-Orty region. The aim was to interpret sedimentary environment. Litology of four selected outcrops, from which fotomozaics were prepared, was studied in detail. Facies and architectural elements recognized in outcrops were defined. Furthermore, measured sedimentary sections of these outcrops were delineated. Character of sedimentary structures and the sedimentary body geometries point to river environment of sedimentation. Low spread of palaeocurrent vectors is interpreted as low sinuosity river system. The absence of structures typical for anastomosing river style finally allow us to interpret the river environment as braided. Powered by TCPDF (www.tcpdf.org)
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