North aegean trough
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 … WebNorth 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 …
North aegean trough
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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 …
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 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 …
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 ] … Web23 de jan. de 2024 · “During the Pleistocene glacial and interglacial periods, connections among many Aegean islands and adjacent mainland were established or broken in a labyrinthine sequence of events At 480–250 ka, the North Aegean Trough (NAT) was isolated from the open sea and the North Aegean Island Bridge connected mainland …
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 …
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). poppin white scissorsWeb1 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 … poppin white key deskWeb1 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 ... shari locante attorney sparta wiWeb1 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. poppin wholesaleWebThe 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 … poppin white stow 3-drawer file cabinetWeb1 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 … poppin white stow file cabinetWebAmong 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]. poppin yeat 1 hour