Akademik Çalışmalar

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http://hdl.handle.net/11527/13121
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Konu "active tectonics" ile Akademik Çalışmalar'a göz atma
  • Öge
    Active deformation pattern in the western flank of the central Taurides, southern margin of the central Anatolian plateau: inferences from geomorphic markers and kinematic indicators
    (Wiley, 2023) Aykut, Tunahan ; Yıldırım, Cengiz ; Uysal, I. Tonguç ; orcid.org/0000-0003-0503-3859 ; orcid.org/0000-0001-5253-028X ; orcid.org/0000-0002-8263-8774 ; Katı Yer Bilimleri
    The southwestern margin of the Central Anatolian Plateau corresponds to the upper crust of the subduction between African and Anatolian plates, with a high relief of up to 2 km. This mountainous region has distinctive geomorphological features and presents a unique setting to investigate the mechanism of orogenic plateau margin development related to subduction and topographic evolution around the Eastern Mediterranean. We present new kinematic data from exposed fault planes and tectonic landforms from high-resolution digital elevation models to elucidate the deformation pattern and its relation with the crustal deformation. We evaluate the deformation pattern based on the spatial distribution of kinematic analyses and geomorphic markers like low relief upland surfaces, disrupted karst basins, knickpoints, and deep bedrock incisions from watershed to shoreline. Our geomorphic analysis reveals a post-orogenic transient actively deforming topography. The geomorphic markers constrain long-term surface uplift pattern with a mean cumulative surface uplift of 1,710 ± 50 m and shows an increasing trend from west to east, from 1,600 ± 50 to 1,800 ± 50 m. Our results suggest a dome-like uplift pattern in the west-east direction across the southern margin that reaches up to maximum cumulative uplift values in the quadrangle of Alanya-Başyayla-Ermenek-Gazipaşa. Our kinematic measurements along the youngest generation of faults revealed an active NE-SW extensional deformation across a broad 200 km zone in the north of the subduction. Our findings have significant implications for understanding the morphotectonic evolution and post-orogenic deformation in the plateau margins and geodynamic evolution of the Eastern Mediterranean. Key Points River longitudinal profiles and low-relief upland surfaces indicated an increasing vertical deformation toward the eastern Central Taurides Geomorphic markers constrained mean cumulative 1,710 ± 50 m surface uplift that peaks in the quadrangle of Alanya-Başyayla-Ermenek-Gazipaşa Kinematic indicators from the youngest brittle structures revealed an active NE-SW extension above the Cyprus Subduction Zone
  • Öge
    Source geometry and rupture characteristics of the 20 February 2023 Mw 6.4 Hatay (Türkiye) earthquake at southwest edge of the East Anatolian Fault
    (Wiley, 2024) Yolsal-Çevikbilen, Seda ; Taymaz, Tuncay ; Irmak, Tahir Serkan ; Erman, Ceyhun ; Kahraman, Metin ; Özkan, Berkan ; Eken, Tuna ; Öcalan, Taylan ; Doğan, Ali Hasan ; Altuntaş, Cemali ; orcid.org/0000-0002-7250-4617 ; orcid.org/0000-0001-6807-9622 ; Jeofizik Mühendisliği
    Following the catastrophic 6 February 2023 Mw 7.8 and Mw 7.6 Kahramanmaraş earthquakes in the East Anatolian Fault Zone (EAFZ; southeast Türkiye), numerous aftershocks occurred along the major branches of this left-lateral shear zone. The spatio-temporal distribution of the earthquakes implied the stress-triggering effects of co-seismic ruptures on closely connected fault segments over large distances. On the 20 February 2023 two earthquakes with Mw 6.4 and Mw 5.2 struck Hatay (Türkiye) located near the Samandağ-Antakya segment of the EAFZ. To understand the rupture evolution of these earthquakes, we first re-located the aftershock sequence that occurred over a 3-month period in the Hatay-Syria region. A normal faulting mechanism with a significant amount of left-lateral strike-slip component at a shallow focal depth of 12 km was estimated for the 2023 Mw 6.4 earthquake from the inversion of seismological data. Our slip models describe a relatively simple and unilateral rupture propagation along about 36 km-long active segments of the EAFZ. The co-seismic horizontal displacements inferred from the Global Navigation Satellite System data are compatible with the oblique slip kinematics. Furthermore, we suggest that this earthquake did not produce notable tsunami waves on the adjacent coasts since the rupture plane did not extend to the seafloor of the Eastern Mediterranean with substantial amount of vertical displacement. We reckon that a future large earthquake (Mw ≥ 7.0) in the Hatay-Syria region where increased stress was transferred to the fault segments of the EAFZ and the Dead Sea Fault Zone (DSFZ) after the 2023 earthquakes will be a probable source of tsunami at the coastal plains of the Eastern Mediterranean Sea region. Key Points The 20 February 2023 Mw 6.4 Hatay (Türkiye) earthquake indicates a normal fault mechanism with a significant left-lateral strike-slip component Transtensional deformation is evident in the Hatay-Syria (SE Türkiye) region Most of the 2023 Hatay-Syria aftershocks appear to concentrate on the depth range of 10–20 km of the crust Plain Language Summary The destructive 6 February 2023 Mw 7.8 and Mw 7.6 SE Türkiye earthquakes triggered an intense seismic activity along the major segments of the East Anatolian Fault Zone (EAFZ) in SE Türkiye. On 20 February 2023, distinct earthquake clusters occurred along the Amanos and Samandağ-Antakya segments in the southwest edge of the EAFZ. In this manuscript, source characteristics and rupture kinematics of the 20 February 2023 Mw 6.4 Hatay (Türkiye) earthquake were estimated by analyzing seismological and geodetic data. Our results mainly indicate a normal faulting mechanism with a significant amount of left-lateral strike-slip component for this earthquake. The slip models show a simple slip distribution pattern along the strike of the fault plane that lasted about 10–12 s. The analyzed time series of the available Global Navigation Satellite System stations present horizontal co-seismic displacements consistent with oblique slip kinematics of the rupture. We finally suggest that this earthquake serves as a reminder of the seismic and tsunami hazard potential in the Hatay-Syria area.