North aegean trough

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August undefined, 2024

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 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...

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

WebCorporate author : UNESCO Person as author : Dani, Ahmad Hasan [editor] Person as author : Mohen, Jean Pierre [editor] Person as author : Lorenzo, José Luis [editor] WebThe North Aegean trough is a zone of deep water trending from northeast to southwest across the N Aegean Sea. The western part of the trough, the Sporadhes basin, contains a thick sequence of late Cenozoic sediments. Le Pichon et al. 1984 suggested that the … simple chain drawing

Tectonic setting of the North Aegean Trough (NAT

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. 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 … rawafd international co

Rates of crustal deformation in the North Aegean trough-North …

An Earthquake-Clustering Model in North Aegean Area (Greece)

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 … 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 … simple chain for menhttp://www.geophysics.geol.uoa.gr/papers/makro/makro165.pdf raw a fat32

"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 … " - North aegean trough

North aegean trough

Fault line sketch map constructed from the interpreted seismic ...

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 … WebThe North Aegean islands promise the most exquisite treats. Samos will serve you its award-winning dessert wine, whose reputation dates back to antiquity. Lesvos’ ouzo is world-renowned, the most famous brands being Plomari and Mini. Chios’ most treasured …

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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. 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.

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. 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 …

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 … 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).

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 ] …

Web1 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 … rawad mounzer md azWebIn 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 rawad mounzer md peoria azWebDownload 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). rawafed al torokWebThe 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... simple chain gold necklaceWebThe 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 … raw adrenal glandular benefitsWeb1 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. simple center pieces for wedding tableWeb16 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. rawafed company