Výsledky vyhľadávania
- Title
Názov Návrh a vyhotovenie názornej učebnej pomôcky pre vyučovací predmet Technológia; téma: Vlasové implantáty - moderná technológia v úprave vlasov Súbež.n. [Design and realization of practical teaching aid for subject Technology; theme: Hair implants - modern technology in hair-gear] Podnázov bakalárska práca Aut.údaje Marcela Petreková; vedúci práce: Mária Lichvárová Autor Petreková Marcela
Ďalší autori Lichvárová Mária 1958- (Školiteľ (konzultant))
Korp. Univerzita Mateja Bela . Fakulta prírodných vied . Katedra techniky a technológií , Banská Bystrica, Slovensko Vyd.údaje Banská Bystrica , 2009. - 44 s. : obr. + Prílohy Poznámka Súbežný názov angl.. - Katedra techniky a technológií Fakulta prírodných vied Univerzita Mateja Bela v Banskej Bystrici Kľúč.slová učebné pomôcky - teaching aids odborný výcvik - professional training vlasové implantáty special training hair implants Jazyk dok. slovenčina Krajina Slovenská republika Systematika 611.78 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xk - Kvalifikačné práce Počet ex. 1, z toho voľných 0, prezenčne 1 
kniha
Stepwise clockwise rotation of the Cenozoic stress field in the Western Carpathians as revealed by kinematic analysis of minor faults in the Manin Unit (western Slovakia)Author infoViera Šimonová, Dušan PlašienkaAuthorCo-authorsSource documentGeological Quarterly. Vol. 61, no. 1 (2017), pp. 251-264. - Warszaw : Polish Geological Institute - National Research Institute, 2017KeywordsHeadings Geogr.LanguageEnglishCountryPolandsystematicsAnnotationThis study aims at quantitative kinematic analysis of fault-slip data and palaeostress reconstruction of polyphase brittle structures developed in the Manin Unit cropping out in the Middle Vah River Valley of western Slovakia. The Manin Unit neighbours the Pieniny Klippen Belt that follows the boundary between the Paleogene accretionary wedge of the Outer Carpathians and the Cretaceous nappe system of the Central Western Carpathians. After the nappe emplacement during mid-Cretaceous times, the Manin Unit was incorporated into the Pieniny Klippen Belt and attained its complex tectonic style. Based on kinematic analysis of meso-scale faults with slickensides, six (D-1-D-6) brittle deformation stages have been discerned. The relative succession of individual palaeostress states was derived from field structural relationships; their strati graphic age was estimated primarily by comparison with other published data. Palaeostress analysis in the Manin Unit revealed the existence of six different palaeostress fields acting from the Middle Eocene to the Quaternary. The first three generations of meso-scale brittle structures were formed under a transpressional tectonic regime during the pre-Late Eocene-Early Miocene D-1-D-3 deformation. Generally, the maximum horizontal stress axis rotated clockwise from a W-E to an approximately N-S direction. Thereafter, a transtensional tectonic regime was characterized by a WNW-ESE to NNW-SSE oriented minimum horizontal stress axis during Middle and Late Miocene D-4-D-5 deformation. A general extensional tectonic regime influenced the structural evolution of the area in the Pliocene to Quaternary, when a gradual reorientation of the palaeostress field resulted in the development of variable, often reactivated, fault structures.