North aegean trough
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 ... 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 …
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 … WebIn contrast to most other arcs with oceanic plate subduction, the Aegean arc is characterized by continent-continent subduction. Noble gas abundances and isotopic compositions of 45 gas samples have
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 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.
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 … 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 …
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
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 … tsx red eagle mining stock quoteWebAmong 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]. phoebe bag free patternWebRight-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. tsx recent iposWebDownload 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). tsx reeWeb6 de nov. de 2007 · Dextral strike‐slip motions along the North Aegean Trough fault zone were possible on NE‐SW‐striking faults. During the Pliocene‐Lower Pleistocene, normal fault components were higher; however, because the angle between the NE‐SW trend of the tensional axis and the strike of the fault zone was acute, dextral strike‐slip components … phoebe bag pattern freeWeb1 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 ). tsx rear window spoilerWebThe localization of the North Anatolian Fault in the northern Aegean Sea (North Aegean Trough) is an intriguing example of continental transform fault propagation. tsx ref报错