North aegean trough

Web25 de fev. de 2024 · According to the gravity inversion study derived from the satellite gravity data (Tirel et al. 2004), the North Aegean Trough is related with a two-stage evolution of the Aegean extension. References Altınok Y, Alpar B and Yaltırak C 2003 Şarköy–Mürefte 1912 earthquake’s tsunami extension of the associated faulting in the … Web1 de nov. de 2015 · Seismicity of the 24 May 2014 Mw 7.0 Aegean Sea earthquake sequence along the North Aegean Trough. E. Görgün, Burçak Görgün. Published 1 November 2015. Geology. Journal of Asian Earth Sciences. View via Publisher. Save to …

An Earthquake-Clustering Model in North Aegean Area (Greece)

WebThe North Aegean Trough is tectonically controlled by the projection of the North Anatolian Fault from western Turkey and the Sea of Marmara into the Aegean, where deformation is distributed... WebThe North Aegean trough is a zone of deep water trending from northeast to southwest across the N Aegean Sea. The western part of the trough, the Sporadhes basin, contains a thick sequence of late Cenozoic sediments. Le Pichon et al. 1984 suggested that the … cinemark in weslaco tx https://turnaround-strategies.com

List of fault zones - Wikipedia

WebThings to Do in Northeast Aegean Islands, Greece: See Tripadvisor's 216,536 traveler reviews and photos of Northeast Aegean Islands tourist attractions. Find what to do today, this weekend, or in April. We have reviews of the best places to see in Northeast … Web1 de dez. de 2014 · The Dalrymple Trough is a 150-km-long, 30-km-wide basin located at the northern termination of the Owen Fracture Zone (OFZ), which is the present-day active India–Arabia plate boundary. The Dalrymple Trough is closely associated with the Murray Ridge, a complex of prominent bathymetric highs located on its eastern flank. WebThe localization of the North Anatolian Fault in the northern Aegean Sea (North Aegean Trough) is an intriguing example of continental transform fault propagation. cinemark in yuba city california

Structure of the Central North Aegean Trough: an active strike‐slip ...

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North aegean trough

List of fault zones - Wikipedia

Web26 de abr. de 2024 · Plan your visit to The North Aegean, Turkey: find out where to go and what to do in The North Aegean with Rough Guides. Read about itineraries, activities, places to stay and travel essentials and get inspiration from the blog in the best guide to … Web9 de ago. de 2024 · nature of faulting as the North Anatolian Fault system enters the north Aegean in the easternmost North Aegean Trough (Figures 1 and 2). Several different models have been proposed for deformation within the Gulf of Saros based …

North aegean trough

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Web16 de jan. de 2024 · The North Aegean Trough is a strike-slip basin emplaced along the North Anatolian Fault. Its tectono-sedimentary context is very similar to the Marmara Sea with splays of the North Anatolian Fault, triggering frequent earthquakes up to M w ∼7 (such as the 24 May 2014 M w =6.9 event in the Gulf of Saros) and with locally gas-charged … Web1 de mar. de 2024 · The North Aegean Trough (NAT) (marked by the box in Fig. 1) consists the northern boundary of the Aegean microplate, first proposed by Papazachos et al. and further studied by many researchers (e.g. Kahveci et al. 2024). NAT is the …

WebThe North Aegean Trough is tectonically controlled by the projection of the North Anatolian Fault from western Turkey and the Sea of Marmara into the Aegean, where deformation is distributed... Web16 de out. de 2024 · Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain.

Web1 de jan. de 2006 · Basin-bounding faults within the North Aegean trough are dominantly characterized by apparently normal components as well as strike-slip components. Plate boundary conditions, as well as pre-existing structures with a favorable orientation relative to the current crustal motion, control and variably affect the present-day deformation along … WebTherefore, the geodynamics of the Aegean The North Aegean Trough follows the western continuation seems to be independent of (or only weakly dependent on) the of the dextral strike-slip North Anatolian Fault, which in movement of Anatolia (Le Pichon et al. 1995). McKenzie & western Turkey, before entering the North Aegean Sea, splits

WebAmong the most recent strong earthquakes is the 24 May 2014 M w 6.9 main shock, which occurred approximately 20 km southeast of Samothraki Island in North Aegean Trough (lat. 40.286 °, lon. 25.375 °). The absence of strong aftershocks with M > 5.0 as well as aftershocks very close to the main shock are two of its main characteristics [52,53].

WebThe zone is over 100 km long and has both transtensional and transpressive features observable on the seismic lines. We suggest that dextral strike‐slip displacement along the zone is on the order of 5–7 km. The structure and fault patterns of Recent deformation in … cinemark in wayneWeb10 de jul. de 2002 · The regional seismic hazard and slope stability analysis shows that the North Aegean marginal upper–middle slopes are highly unstable. The calculated values of horizontal ground acceleration able to initiate failures (kc) range from 80 to 300 Gal … diabetic tussin interactionsWebThe western North Aegean Trough (west of Lemnos Island) constitutes a complicate d oblique - rifting/shear-zone system with the angle of obliquity decreasing from west to east while the rate of... cinemark in willowbrook mallWeb10 de jul. de 2002 · The regional seismic hazard and slope stability analysis shows that the North Aegean marginal upper–middle slopes are highly unstable. The calculated values of horizontal ground acceleration able to initiate failures (kc) range from 80 to 300 Gal downslope. This is lower than what is expected within 50 yr (especially in the … cinemark irvingWeb1 de jan. de 2002 · The North Aegean Trough, deepest among the Aegean marine troughs has been con- sidered as a site example for discussing the evolutionary models of continental crustal structure towards thinning ... diabetic tussin max st precioWebThe zone is over 100 km long and has both transtensional and transpressive features observable on the seismic lines. We suggest that dextral strike-slip displacement along the zone is on the order of 5–7 km. The structure and fault patterns of Recent deformation in … diabetic tussin interaction with depakoteWeb16 de out. de 2024 · As mentioned earlier the North Aegean Trough represents an area that is affected by deformation due to the combined influence of the westward escape of Anatolia and the gravitational spreading of the Aegean lithosphere. cinemark irving mall