prikaz prve stranice dokumenta Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti
Embargo period 2025-09-19
undergraduate thesis
Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti
Zagreb: University of Zagreb, Faculty of Science, 2024. urn:nbn:hr:217:395160
Dudaš, David
University of Zagreb
Faculty of Science
Department of Geography

Institutional repository: Repository of the Faculty of Science

Cite this document

Dudaš, D. (2024). Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti (Undergraduate thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:395160

Dudaš, David. "Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti." Undergraduate thesis, University of Zagreb, Faculty of Science, 2024. https://urn.nsk.hr/urn:nbn:hr:217:395160

Dudaš, David. "Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti." Undergraduate thesis, University of Zagreb, Faculty of Science, 2024. https://urn.nsk.hr/urn:nbn:hr:217:395160

Dudaš, D. (2024). 'Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti', Undergraduate thesis, University of Zagreb, Faculty of Science, accessed 22 March 2025, https://urn.nsk.hr/urn:nbn:hr:217:395160

Dudaš D. Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti [Undergraduate thesis]. Zagreb: University of Zagreb, Faculty of Science; 2024 [cited 2025 March 22] Available at: https://urn.nsk.hr/urn:nbn:hr:217:395160

D. Dudaš, "Analiza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti", Undergraduate thesis, University of Zagreb, Faculty of Science, Zagreb, 2024. Available at: https://urn.nsk.hr/urn:nbn:hr:217:395160

Metadata
TitleAnaliza vijugavosti izabranih dijelova korita rijeke Drave kao indikatora tektonske aktivnosti
Title (english)Analysis of channel sinuosity of the selected Drava River segments as an indicator of tectonic activity
AuthorDavid Dudaš
MentorSanja Faivre (mentor)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geography)
Zagreb
Defense date and country2024-09-19, Croatia
Scientific / art field,
discipline and subdiscipline		INTERDISCIPLINARY AREAS OF KNOWLEDGE
Geography
Abstract
Strukturno geomorfološki procesi izrazito su bitni za oblikovanje reljefa, međutim determiniranje tektonski aktivnih područja, tj. aktivnih rasjeda izrazito je kompleksan problem. U novije vrijeme kao indikator pomaka i aktivnosti rasjeda može se koristi vijugavost rijeka. U ovome radu istražena je vijugavost toka rijeke Drave kako bi se istražila tektonska aktivnost. Na vijugavost toka rijeke Drave na području Hrvatske utječu tri rasjedne zone, Periadriatsko – Dravski rasjed, Dravski rasjed,... More te rasjedi na području Mađarske koji direktno presijecaju tok rijeke. Rijeka Drava svoj tok mijenja većinski pod utjecajem pomaka rasjeda koji su prostorno bliži njenom toku. Na sjeveru Hrvatske dolazi do izravnog presijecanja toka rijeke Drave rasjedima, pa taj dio toka ima veću vijugavost od ostalih dijelova Drave. Iz ovog rada je vidljivo da je vijugavost dobar indikator tektonske aktivnosti jer se povećava u blizini aktivnih rasjeda. Less
Abstract (english)
Structural geomorphological processes are critically important for shaping the landscape; however, determining tectonically active areas, particularly faults, is a highly complex problem. Recently, river sinuosity has been used as a measure for identifying fault displacements and activities. In this work, the sinuosity of the Drava River was investigated to demonstrate the tectonic activity of faults. The meandering of the Drava River in the Croatian region is influenced by three fault... More zones: the Periadriatic-Drava Fault, the Drava Fault, and the normal faults in Hungary that directly intersect the river's course. The Drava River changes its course primarily under the influence of fault shifts that are spatially closer to its flow, while in Northern Croatia, the river's course is directly intersected, resulting in this section having greater sinuosity compared to other parts of the Drava's flow .It has been proven that sinuosity is a good indicator of tectonic activity, as it increases in areas where faults are tectonically active and exhibit greater fault plane displacements. Less
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:395160
Study programmeTitle: Undergraduate study; specializations in: research
Course: research
Study programme type: university
Study level: undergraduate
Academic / professional title: sveučilišni/a prvostupnik/prvostupnica (baccalaureus/baccalaurea) geografije (sveučilišni/a prvostupnik/prvostupnica (baccalaureus/baccalaurea) geografije)
Type of resourceText
File originBorn digital
Access conditionsEmbargoed access
Embargo expiration date: 2025-09-19
Terms of useLicence In copyright icon
Created on2024-09-20 08:51:31
accessibility

closeAccessibilityrefresh

If you wish to permanently save changes, click on Save, if not - your settings will be reset when you restart the browser.