Tectonic geomorphology of the Hoyran Graben (Western Anatolia, Türkiye) : insights from geomorphic indices

• Autorzy: Çetin Yaren Sena , Ağar Hasan Salih , Kahraman Burcu , Bayram Levent , Kul Ahmet Özkan , Özsayin Erman , Üner Serkan

Identyfikatory

DOI

10.7306/gq.1724

• Języki publikacji: EN

Abstrakty

EN

The area between Western Anatolia and Isparta Bend comprises numerous depressions and the active faults that bound them. The Hoyran Graben is one of these depressions, located at the northernmost part of the Isparta Bend. This NE-SW-oriented graben is bounded by the Hoyran Fault in the northwest and the Uluborlu, Senirkent and Kumdanlı faults in the south-east, respectively. We evaluate the seismic activity potential among segments of the boundary faults in the light of fieldwork and morphometric indices. These boundary faults of the Hoyran Graben are divided into twelve segments for the analysis, with indices used including mountain-front sinuosity (Smf: 1.05-2.02), valleyfloorwidth-to-valiey height ratio (Vf: 0.11-1.34), hypsometric curve and integral (Hi: 0.4-0.73), asymmetry factor (Af: 13.76-87.03), stream length-gradient (SL: 1.48-9450) and normalized channel steepness (Ksn: 2.38-990.38). The results obtained, together with field observations, indicate that the Uluborlu, Senirkent and Kumdanlı faults, as well as the western segments of the Hoyran Fault, represent higher potential in terms of seismic activity with uplift rates >0.5 mm/y, while the central and eastern segments show moderate activity with uplift rates between 0.05 and 0.5 mm/y. Thus, the boundary faults of the Hoyran Graben need further attention in terms of regional seismic hazard.

Słowa kluczowe

EN

seismic activity; boundary faults; morphometric analysis; palaeostress analysis; seismic hazard

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2024
• Tom: Vol. 68, No. 1
• Strony: art. no. 1
• Opis fizyczny: Bibliogr. 132 poz., fot., rys., tab., wykr.

Twórcy

autor

Çetin Yaren Sena

• Hacettepe University, Graduate School of Science and Engineering, TR-06800, Ankara, Türkiye

• https://orcid.org/0000-0001-6801-1804

autor

Ağar Hasan Salih

• Hacettepe University, Department of Geological Engineering, TR-06800, Ankara, Türkiye

• https://orcid.org/0009-0006-8666-5186

autor

Kahraman Burcu

• Hacettepe University, Department of Geological Engineering, TR-06800, Ankara, Türkiye

• https://orcid.org/0000-0003-4172-5086

autor

Bayram Levent

• Hacettepe University, Department of Geological Engineering, TR-06800, Ankara, Türkiye

• https://orcid.org/0000-0002-6197-4330

autor

Kul Ahmet Özkan

• Van Yüzüncü Yıl University, Department of Geological Engineering, TR-65080, Van, Türkiye

• https://orcid.org/0000-0003-1854-2206

autor

Özsayin Erman

• Hacettepe University, Department of Geological Engineering, TR-06800, Ankara, Türkiye

• https://orcid.org/0000-0003-3948-5482

autor

Üner Serkan

• Van Yüzüncü Yıl University, Department of Geological Engineering, TR-65080, Van, Türkiye

• https://orcid.org/0000-0001-5974-1856

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Uwagi

Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki (2025).