Autor: |
Telbisz Tamás, Mari László, Ćalić Jelena |
Jazyk: |
English<br />Serbian |
Rok vydání: |
2007 |
Předmět: |
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Zdroj: |
Glasnik Srpskog Geografskog Društva, Vol 87, Iss 2, Pp 21-30 (2007) |
Druh dokumentu: |
article |
ISSN: |
0350-3593 |
DOI: |
10.2298/GSGD0702021T |
Popis: |
Mt. Miroč doline karst evolution and its determining factors such as geology, relief and structure are analyzed using GIS tools. The 3064 dolines found in a 123 km2 area support the use of different statistical methods. Doline density (24.9 km-2) is relatively high and mean doline area (1697 m2) is relatively small. Both frequency analysis and field evidence suggest that doline karst evolution of the area is at a relatively young stage. Spatial distribution of the dolines is mainly determined by the Upper Jurassic limestone, and slope angle less than 12°. Furthermore, the anticline limbs and axis as well as the SW-NE trend fault lines are also in connection with doline density. However, doline long axis orientation is tpyically NW-SE, which is not in accordance with the observed rupture systems. Therefore, this issue requires further research. |
Databáze: |
Directory of Open Access Journals |
Externí odkaz: |
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