North aegean trough

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 … 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 ).

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

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 WebDownload 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). iron protector 2016 film https://instrumentalsafety.com

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

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 … 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]. 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 … iron protection

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Category:Active tectonics of the north and central Aegean Sea

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North aegean trough

Evidence for active faulting in the eastern part of the Gulf of Saros ...

WebThe studied core comes from the North Aegean Trough (NAT; Figure 1 a), a northeast–southwest (NE–SW) elongated depression with a depth range between 800 and 1590 m that includes several interconnected sub-basin depressions, separated from each other by 100- to 350-m-deep intervening shoals and associated islands [ 5, 61 ]. Figure 1. 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 …

North aegean trough

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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 …

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 …

WebCorporate author : UNESCO Person as author : Dani, Ahmad Hasan [editor] Person as author : Mohen, Jean Pierre [editor] Person as author : Lorenzo, José Luis [editor] WebThings to Do in Northeast Aegean Islands, Greece: See Tripadvisor's 216,536 traveler reviews and photos of Northeast Aegean Islands tourist attractions. Find what to do today, this weekend, or in April. We have reviews of the best places to see in Northeast …

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 …

http://www.geophysics.geol.uoa.gr/papers/makro/makro165.pdf iron protector 2016 downloadWebThe 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 … port richey realtorWeb1 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 … iron protector coverWeb16 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. port richey rec centerWebM. 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 iron protector imdbWeb[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 … iron protector downloadWebThe 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 … port richey real estate for sale