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 ... 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
North aegean trough
Did you know?
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 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 …
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 … 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
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. 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
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 …
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 … temple market daysWeb[9] The North Aegean Trough is the westward continuation of the Saros basin passing between the islands of Samothraki and Gökçeada ( Figure 2 ). Prominent fault-controlled escarpments bound the north and south of the basin with significant vertical … temple maya jungleWeb30 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. templemarketWebNorth 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 … temple matlab kya hota haiWeb9 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 … temple mayanWeb11 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 … temple matang kuchingWeb10 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 … temple mayase