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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 ... Web11 de abr. de 2024 · The Iberian Abyssal Plain, off the west coast of Portugal and Spain, formed 126 Ma. This separated Newfoundland 's Grand Banks, with Galicia Bank and Flemish Cap being split at 118 Ma. By Early Cretaceous, 110 Ma rifting occurs on west and north west edges. During the time of the supercontinent Pangea, the Iberian plate was …

Postcollisional contractional and extensional deformation in the Aegean …

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 … 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 … gimp 4k theme https://theresalesolution.com

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

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 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... 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 … gimp 64 bit windows 10 download

Propagation and termination of a strike slip fault in an extensional ...

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

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North aegean trough

Postcollisional contractional and extensional deformation in the Aegean …

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]. Web30 de jun. de 2024 · We identify an extensive basin developing in the Thermaikos Gulf inner shelf, outer shelf, and slope leading to the 1500 m deep West North Aegean Trough (NAT). We establish the unconformable extent of Eocene and Oligocene sequences on the upper shelf and trace their continuation in the deeper shelf and slope of Thermaikos Gulf.

North aegean trough

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WebThese mechanisms show that the faulting in the western part of the Aegean region is mostly extensional in nature, on normal faults with a NW to WNW strike and with slip vectors directed NNW to NNE. There is evidence from palaeomagnetism that this western region rotates clockwise relative to stable Europe. 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 localization of the North Anatolian Fault in the northern Aegean Sea (North Aegean Trough) is an intriguing example of continental transform fault propagation. Webextensional environment of the Aegean, it splits into two main branches composed of en echelon segments with linking pull- apart basins. The northern branch is predominant. It forms the deep Marmara Sea basins and crosses the northern edge of the Gelibolu Peninsula to reach the Gulf of Saros and the North Aegean Trough (Figures I and 2).

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 … 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

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 …

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 … fullband count bandogWebCorporate author : UNESCO Person as author : Dani, Ahmad Hasan [editor] Person as author : Mohen, Jean Pierre [editor] Person as author : Lorenzo, José Luis [editor] gimp 64 bit windows 10Web10 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 … fullband signal booster