North aegean trough

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August undefined, 2024

WebThis list covers all faults and fault-systems that are either geologically important [clarification needed] or connected to prominent seismic activity. [clarification needed] It is not intended to list every notable fault, but only major fault zones.[clarification needed Web16 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.

Tectonics of the Dalrymple Trough and uplift of the Murray Ridge …

Web1 de mar. de 2012 · Division of the North Aegean into four subareas according to seismotectonic similarities: 1: Sporades, 2: North Aegean Trough (NAT), 3: Central Area, 4: Chios-Lesvos. Earthquakes between 1970 and 2010 with M = 5.0 are indicated as red circles (dark grey circles in print), 4.5 = M < 5.0 as green (light grey) circles and M c = M … WebM. Brooks G. Ferentinos (1980) ArticleTitle Structure and evolution of the Sporadhes Basin of the north Aegean trough, Northern Aegean Sea Tectonophysics 68 15–30 Occurrence Handle 10.1016/0040-1951(80)90006-2 cleopatra history in tamil

North Aegean Trough : Near Vertical and Wide-angle Seismic Data

Web10 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 … Web1 de fev. de 2002 · The most prominent feature in this area is the North Aegean Trough (NAT), which represents the northwesternmost continuation of the North Anatolian Fault (NAF) in the North Aegean , with the general earthquake pattern corresponding to … WebRight-lateral major continental strike-slip faults (e.g. North and East Anato- strike-slip deformation associated with the NAFZ extends into the C 2005 RAS, GJI, 162, 633–640 Curie-point depth map of Turkey 635 north Aegean (north Aegean trough), terminating near the Gulf of plate beneath the Aegean and Anatolian plates may cause an up- Corinth. blue water dental advisors

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

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 … WebDownload scientific diagram Fault line sketch map constructed from the interpreted seismic sections. Major faults are shown in bold lines. The faults on land were adopted from Görür et al. (1995). blue water cruising yachts for sale australiaWeb10 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 … bluewater day spa greenhills

"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 … " - North aegean trough

North aegean trough

Late Cenozoic Evolution and Present Tectonic Setting of the Aegean ...

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 … WebThe rates and configuration of seismic deformation in the North Aegean trough-North Anatolian fault are determined from the moment tensor mechanisms of the earthquakes that occurred within this region. The analysis is based onKostrov's (1974) formulation. The …

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WebThe 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... 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 …

WebThe 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 through extension. It marks the recent interaction of the strike … Web23 de fev. de 2024 · The map of the Moho depth (Figure 2A) indicates that the thinnest crust is observed in the Cretan basin, the Karpathos trough (15–20 km) and the North Aegean trough (20–25 km). The Cretan and Mykonos–Ikaria basins are deep troughs, where a relatively thin crustal basement is buried beneath a thick sedimentary cover (e.g., [ 24 ] …

Web[9] The North Aegean Trough is the westward continuation of the Saros basin passing between the islands of Samothraki and Gökçeada ( Figure 2 ). Prominent fault-controlled escarpments bound the north and south of the basin with significant vertical … Web1 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 ...

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

WebContinuous seismic (Air-Gun) subbotom profiling in the N.Aegean was revealed a large submarine translational slide. The failure zone is extended from about 300m depth down to 800 m and covers an area of 85 Km2. The mean thickness of the slide reaches about 55 m and an estimated total volume of 4 Km3 of Quaternary sediments have been slided along … blue water csinoWeb9 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 … cleopatra history channelWeb1 de abr. de 2015 · The May 24, 2014 North Aegean earthquake was caused by the activation of a segment of North Aegean Trough, the western extension of the North Anatolian Fault Zone. cleopatra hospital company mubasherWebAmong 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]. cleopatra hookah lounge cleopatra holtWebNorth Aegean Sea map. The North Aegean islands are a number of scattered islands in the North Aegean Sea, also known as the Northeastern Aegean islands, belonging mostly to Greece and a few of them to … cleopatra history storyWeb1 de fev. de 2002 · The most prominent feature in this area is the North Aegean Trough (NAT), which represents the northwesternmost continuation of the North Anatolian Fault (NAF) in the North Aegean ( Fig. 1 ), with the general earthquake pattern corresponding to dextral strike-slip faulting ( Papazachos 1990 ). bluewater dental ionia mi