North aegean trough

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 … 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

Extension of the North Anatolian Fault into the North Aegean …

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 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 … diabetes education az https://ahlsistemas.com

Variation in noble gas isotopic composition of gas samples from …

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 … 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. 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. diabetes education bengali

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Category:Seismicity rate changes in association with the evolution of the …

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North aegean trough

(PDF) The May 24, 2014 North Aegean Trough earthquake: stress …

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 … 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.

North aegean trough

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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 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 …

Web1 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. 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 …

Web10 de jul. de 2002 · General morphological features of the North Aegean region and major marginal fault zones (red lines). Western Anatolian fault (WAF) and their western extension (North Aegean fault) which configure the North Aegean Trough (NAT) is also indicated … 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 …

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 ( Fig. 1 ), with the general earthquake pattern corresponding to dextral strike-slip faulting ( Papazachos 1990 ).

WebCorporate author : UNESCO Person as author : Dani, Ahmad Hasan [editor] Person as author : Mohen, Jean Pierre [editor] Person as author : Lorenzo, José Luis [editor] cinderella\\u0027s royal table bookingWebThe 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 … diabetes education boardWeb1 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 … diabetes education benefitsWeb1 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 … cinderella\\u0027s royal table bathroomWebThe 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 … cinderella\u0027s royal table change reservationWebThe 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 … diabetes education birmingham alWebThis 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 cinderella\\u0027s royal table at magic kingdom