Active tectonics of western Kosovo: Insights from geomorphic and structural analyses
Yıl 2024,
Cilt: 173 Sayı: 173, 153 - 173, 26.04.2024
Alper Gürbüz
Astrit Shala
Shemsi Mustafa
Aytekin Erten
Öz
Kosovo is located in a key position in the central-west part of the Balkans providing an opportunity to understand the far-field effects of distributed intracontinental deformation caused by the Aegean extension in the south and Adriatic compression in the west. It is also situated along the NE-SW trending Shkodër-Pejë transverse zone, where the Dinarides and Albanides-Hellenides orogenic belts are juxtaposed. While the instrumental seismicity of Kosovo indicates the activity of this fault zone and many others, the active faults in the country were not discussed in detail in the current literature. In this study, we analyzed both the geomorphic and structural features of major mountain front faults in western Kosovo (i.e., Pejë, Istog, Krojmir, and Prizren faults) to reveal the relative assessment of their activities and kinematic characters. Geomorphic and morphometric analyses of all the studied four different mountain fronts indicated high activity and tectonic uplift rates of over 0.5 mm/a. On the other hand, according to the collected kinematic data from the observed fault planes, the studied faults are mainly of normal character representing a dominance of NWSE- directed extension in western Kosovo, which is most probably caused by the rollback of the subducting slab in the Hellenic trench.
Teşekkür
The authors are grateful to two reviewers for their constructive criticisms and to Dr. Ercan SANGU for suggestions on the kinematic analysis. The stress analysis results were obtained using Win-Tensor, a software developed by Dr. Damien DELVAUX, Royal Museum for Central Africa, Tervuren, Belgium
Kaynakça
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Yıl 2024,
Cilt: 173 Sayı: 173, 153 - 173, 26.04.2024
Alper Gürbüz
Astrit Shala
Shemsi Mustafa
Aytekin Erten
Kaynakça
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- Aubouin, J., Blanchet, R., Cadet, J. P., Celet, P., Charvet, J., Chorowicz, J., Cousin, M., Rampnoux, J. P. 1970. Essai sur la géologie des Dinarides. Bulletin de la Société géologique de France 7(6), 1060-1095.
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- D’Agostino, N., Avallone, A., Cheloni, D., D’Anastasio, E., Mantenuto, S., Selvaggi, G. 2008. Active tectonics of the Adriatic region from GPS and earthquake slip vectors. Journal of Geophysical Research 113(B12), B0940.
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- D’Agostino, N., Copley, A., Jackson, J., Koçi, R., Hajrullai, A., Duni, L., Kuka, N. 2022. Active tectonics and fault evolution in the Western Balkans. Geophysical Journal International 231(3), 2102-2126.
- Delvaux, D., Sperner, B. 2003. Stress tensor inversion from fault kinematic indicators and focal mechanism data: the TENSOR program. Nieuwland, D. (Ed.). New Insights into Structural Interpretation and Modelling. Geological Society of London, Special Publications 212, 75-100.
- Dibiase, R. A., Whipple, K. X., Heimsath, A. M., Ouimet, W.
B. 2010. Landscape form and millennial erosion rates in the San Gabriel Mountains, CA. Earth and Planetary Science Letters 289(1-2), 134-144.
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- Elezaj, Z. 2002. Seismotectonic characteristics of Kosovo as basis for its seismic zonation. Ph.D. Thesis, Prishtina, Kosovo (in Albanian).
- Elezaj, Z. 2009. Seismotectonic settings of Kosovo. Journal of International Environmental Application and Science 4(2), 167-176.
- Elezaj, Z. 2012. Late and young tectonics (Neotectonics) and seismicity of Kosovo. Journal of International Environmental Application and Science 7(4), 744-749.
- Elezaj, Z., Kodra, A. 2007. Gjeologjia e Kosovës. Univ. i Prishtinës, Fak. i Xehetarisë dhe Metalurgjisë Mitrovicë 293.
- El Hamdouni, R., Irigaray, C., Fernández, T., Chacón, J., Keller, E. A. 2008. Assessment of relative active tectonics, southwest border of the Sierra Nevada (southern Spain). Geomorphology 96(1-2), 150-173.
- Faccenna, C., Jolivet, L., Piromallo, C., Morelli, A. 2003. Subduction and the depth of convection in the Mediterranean mantle. Journal of Geophysical Research: Solid Earth 108(B2), 2099.
- Faccenna, C., Piromallo, C., Crespo-Blanc, A., Jolivet, L., Rossetti, F. 2004. Lateral slab deformation and the origin of the western Mediterranean arcs. Tectonics 23(1), TC1012.
- Flint, J. J. 1974. Stream gradient as a function of order, magnitude, and discharge. Water Resources Research, 10(5), 969-973.
- Han, Z., Li, X., Wang, N., Chen, G., Wang, X., Lu, H. 2017. Application of river longitudinal profile morphometrics to reveal the uplift of Lushan Mountain. Acta Geologica Sinica 91(5), 1644–1652.
- Handy, M. R., Ustaszewski, K., Kissling, E. 2015. Reconstructing the Alps–Carpathians–Dinarides as a key to understanding switches in subduction polarity, slab gaps and surface motion. International Journal of Earth Sciences 104(1), 1-26.
- Handy, M. R., Giese, J., Schmid, S. M., Pleuger, J., Spakman, W., Onuzi, K., Ustaszewski, K. 2019. Coupled crust-mantle response to slab tearing, bending, and rollback along the Dinaride-Hellenide orogen. Tectonics 38(8), 2803-2828.
- Hare, P. W., Gardner, T. W. 1985. Geomorphic indicators of vertical neotectonism along converging plate margins, Nicoya Peninsula, Costa Rica. Tectonic Geomorphology 4, 75-104.
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