National Repository of Grey Literature 101 records found  previous11 - 20nextend  jump to record: Search took 0.00 seconds. 
The Silurian-Devonian boundary in the Barrandian (Czech Republic): Sedimentology, magnetic susceptibility and gamma-ray spectrometry stratigraphy
Vacek, František ; Bosák, Pavel (advisor) ; Pruner, Petr (referee) ; Kukal, Zdeněk (referee)
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Performance Measurement Company CHEDO, spol. s r.o.
Bosák, Pavel ; Pilka, Josef (referee) ; Bartoš, Vojtěch (advisor)
This diploma thesis deals with the assessment of productivity in the company CHEDO, Ltd. The activity field of this company comprises distribution of coating materials. The analysis used in the theoretical part inspects the position of the company from the view of effectiveness of the business process with the emphasis especially on the negative findings. With the method Balanced Scorecard we are given the right direction towards the behaviour and attitude of the company towards the process of management control in order to increase the performance of the company on the market to achieve adequate financial stability.
Palaeomagnetic research of cave fill in Hermanshöhle, Austria : final report
Bosák, Pavel ; Pruner, Petr ; Mock, A.
Zpráva je volně šiřitelná od roku 2015. Anotace: Detailed paleomagnetic analysis of sedimentary profile at Teichkluft showed that sediments are characterized by varying magnetic susceptibilities and NRM with increasing tendency of anisotropy parameter with increase of susceptibility. The component analysis identified 2 short R polarity intervals (0.41 m; 2.19–2.26 m) within samples with the N polarity. Rock magnetic and AMS measurements indicated mostly the presence of oblate, low coercivity magnetic fraction, presumably magnetite. However, the R polarity interval (2.19–2.26 m) revealed also other, higher coercivity fraction (maybe due to hematite/goethite content). The identity of this fraction is still unknown. The R polarity interval in 0.41 m represents a geomagnetic excursion without any doubt. The sedimentary profile with the R polarity interval in 0.41 m must be older than 162.7 ± 3.9 ka old topmost speleothem. The paleomagnetic directions (D, I) are very close to the present magnetic field. Therefore we assume deposition of studied sediments within the Brunhes chron (<780 Ka) and the excursion may be correlated with Jamaica-Pringle Falls (205–215 ka) or Calabrian Ridge 1 excursions (315–325 ka; Langereis et al. 1997). Other Th/U date was obtained at the tourist trail opposite to Teichkluft entrance (ca 495 ka +67/-41 ka) in an altitude corresponding to the top of the Teichkluft profile. This might indicate that the Teichkluft was completely or nearly completely filled twice (before 163 and ca 495 ka) and once completely excavated (between ca 205/325 and ca 495 ka). The fragments of cuticle of ring-like shape at the level of 2.30 m belongs to attemsiid millipedes. The probability that fragments represent Polyphematia moniliformis (Latzel, 1884; Diplopoda: Chordeumatida: Attemsiidae) known in the cave is high. It is supposed they are Tertiary relict (Mock and Tajovský 2008). It is not detected, if fragments represent relics of recent/subrecent animal
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Plný tet: 0443832 Hermanshoehle_report_final - Download fulltextPDF
Výzkum vybraných travertinů na Slovensku : etapová zpráva č. 2 - Liptov
Bosák, Pavel ; Pruner, Petr ; Bella, P.
Zpráva je volně šiřitelná. Anotace: Bylo provedeno doplňující vzorkování 2 travertinových těles v Liptovské kotlině mezi Liptovským Mikulášem a Ružomberkem (Čerená a Liptovské Sliače–Skalie) pro paleomagnetický výzkum, Th/U datování a analýzu stabilních izotopů (O, C). Vzorky byly odebrány z pozic, u kterých paleomagnetická analýza vzorků z roku 2012 ukázala inverzní nebo přechodnou (inverzní – normální) polaritu. Báze travertinů na lokalitě Čerená lze datovat do období mezi 419 a 283 ka.
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Plný tet: 0399071 - Download fulltextPDF
16th International Congress of Speleology : Czech Republic, Brno July 21–28,2013 : proceedings
Filippi, Michal ; Bosák, Pavel
Proceedings of the 16th International Congress of Speleology consist of 3 separate Volumes. The Congress was visited by 1007 participants from 53 countries across the world. Volume III also starts with traditional, heavily attended topics organized in two sessions: “Karst and Caves in Carbonate Rocks, Salt and Gypsum” and “Karst and Caves in Other Rocks, Pseudokarst”. These topics are supplemented by the related session “Speleogenesis”. This last volume of the Proceedings is ended by the study of cave minerals, included in a specific session “Cave Minerals”.

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