scholarly journals Challenges of the Seismic Image Resolution for Gas Exploration in the East Mediterranean Sea

2021 ◽  
Vol 0 (0) ◽  
pp. 1-13
Author(s):  
Moataz Barakat ◽  
Nader El-Gendy ◽  
Adly El-Nikhely ◽  
Ahmed Zakaria ◽  
Hany Hellish
Jurnal Hukum ◽  
2020 ◽  
Vol 36 (2) ◽  
pp. 126
Author(s):  
Edanur Yıldız

Turkey and Greece are again dragged into a new conflict in the East Mediterranean. Turkey and Greece vie for supremacy in the eastern Mediterranean. Turkey, for its part, indicated that Greece's claim to the territory would amount to a siege in the country by giving Greece a disproportionate amount of territory. This study aims to rethink the conflict between Greece and Turkey in the waters of the Mediterranean sea in the view of international maritime law. This study uses an empirical juridical approach. The Result of this research is Turkey does not ignore the Greece rights, Greece ignores the international law with its extended or excessive maritime claims. Greece tries to give full entitlement of the islands in Mediterranean and Agean. Whereas the effect Formula is applied by international courts.


2020 ◽  
Vol 211 ◽  
pp. 104267
Author(s):  
Moufida Abdennadher ◽  
Amel Bellaaj Zouari ◽  
Wafa Feki Sahnoun ◽  
Lamia Dammak Walha ◽  
Mabrouka Mahfoudi ◽  
...  

2005 ◽  
Author(s):  
Michael Fehler ◽  
Lianjie Huang ◽  
Ru‐Shan Wu ◽  
Xiao‐Bi Xie

2020 ◽  
Author(s):  
Michael Nirrengarten ◽  
Geoffroy Mohn ◽  
François Sapin ◽  
Jon Teasdale ◽  
Charlotte Nielsen ◽  
...  

<p>At the transition between the Atlantic and the Tethys oceanic systems, the plate kinematic configuration of the East Mediterranean domain during the early Mesozoic is still poorly understood. Several factors like the Messinian salt, the different compressional events, the thick carbonate platforms and Cenozoic deltaic deposits combine to blur the imaging of Eastern Mediterranean rifted margins. This has led to distinct and often markedly contrasting interpretations of the timing of opening (ranging from Carboniferous to Cretaceous), structural evolution (divergent to transform segments) and kinematics (N-S to WNW-ESE extension).</p><p>To address this long-standing problem, we gathered disparate geological observations from the margins surrounding the Eastern Mediterranean Sea to integrate them in a global plate model. Distinct, end-member plate kinematic scenarios were tested, challenged and iterated by observations from the Eastern Mediterranean rifted margins.</p><p>The N-African and NW-Arabian margins of the Eastern Mediterranean Sea are relatively weakly reactivated by the different compressional events and were chosen as the starting point of our integrative tectonic study. Legacy plate models for the area mostly show N-S to NNE-SSW opening of the Eastern Mediterranean of pre-Jurassic age. We have integrated dense industrial seismic data, deep boreholes and dredge data, as well as enhanced satellite gravity images that strongly suggests WNW-ESE oriented lithospheric extension and sea floor spreading during the Late Triassic to Early Jurassic.</p><p>Our approach starts by the mapping of the main extensional and compressional structures, the different crustal domains and the pre-rift facies distribution. We investigate the potential conjugate margins now located and imbricated in the Dinarides, Hellenides and Taurides on the northern side of the East Mediterranean Sea by looking at the drowning ages of the Mesozoic carbonate platform and the related rift structures. We refine the full fit and initial spreading of the Atlantic Ocean using crustal thickness and features observed on both sides of the system to calibrate the motion of Eurasia and Africa, which determine the space available to develop the Eastern Mediterranean Sea. Initial tests on the evolution of the main tectonic plates highlight an insufficient eastward motion of Africa relative to Eurasia (Iberia) to accommodate the extension of Eastern Mediterranean during the Jurassic with a purely WNW-ESE direction of extension. Further hypotheses remain to be tested. However, for now, a scenario involving poly-phased and poly-directional motion of the conjugate continent “Greater Adria” during Jurassic is favoured to model the Eastern Mediterranean plate evolution in relation with the closure of the Neo-Tethys further north.</p>


2018 ◽  
Vol 8 (3) ◽  
pp. 65
Author(s):  
Kalathaki Maria

In this paper is describing an initiative in cultural, outdoor science education that took place in the west Crete-Greece(Chania & Rethymnon counties) in 2015, and organized in collaboration with teachers and social bodies, to connectScience, Education and Local Communities for a better quality of everyday life. The initiative concentrated inorganizing the European Educational Conference “Mediterranean Sea Connects Us: Progress in Education withLocal Communities”, which hosted as a training program that can be applied elsewhere, with different target groups,promoting the aims of participatory acquisition of knowledge by sharing them in company, with experientialactivities in moments of joy, happiness and wisdom. Educators-officials of high level and much experienced in thethree levels of Education from Greece, Cyprus, Turkey and Romania, with representatives from local bodies, wereinvited to deposit experience, aspects, ideas and expectations on future educational collaboration in the area ofBalkans, East Mediterranean and widely. As coexisting in the same geographical area, with long and importantcommon past, as collaborators in educational projects from the past, intended to be partners in important andinnovative future jointed actions in cultural STEM Education, for the progress of Mediterranean local educationalcommunities.


Molecules ◽  
2020 ◽  
Vol 25 (7) ◽  
pp. 1509
Author(s):  
Maria Harizani ◽  
Eleni Katsini ◽  
Panagiota Georgantea ◽  
Vassilios Roussis ◽  
Efstathia Ioannou

From the organic extracts of five bacterial strains isolated from marine sediments collected in the East Mediterranean Sea, three new (15, 16, 31) and twenty-nine previously reported (1–14, 17–30, 32) metabolites bearing the 2,5-diketopiperazine skeleton were isolated. The structures of the chlorinated compounds 15, 16, and 31 were elucidated by extensive analysis of their spectroscopic data (NMR, MS, UV, IR). Compounds 15 and 16 were evaluated for their antifungal activity against Candida albicans and Aspergillus niger but were proven inactive. The relevant literature is supplemented with complete NMR assignments and revisions for the 29 previously reported compounds.


2021 ◽  
Vol 139 ◽  
pp. 103879
Author(s):  
Christos Tsabaris ◽  
Konstantinos Tsiaras ◽  
Georgios Eleftheriou ◽  
Georgios Triantafyllou

2016 ◽  
Vol 73 (4) ◽  
pp. 1611-1619 ◽  
Author(s):  
S. Christodoulaki ◽  
G. Petihakis ◽  
N. Mihalopoulos ◽  
K. Tsiaras ◽  
G. Triantafyllou ◽  
...  

Abstract The historical and future impacts of atmospheric deposition of inorganic nitrogen (N) and phosphorus (P) on the marine ecosystem in the east Mediterranean Sea are investigated by using a 1D coupled physical– biogeochemical model, set up for the Cretan Sea as a representative area of the basin. For the present-day simulation (2010), the model is forced by observations of atmospheric deposition fluxes at Crete, while for the hindcast (1860) and forecast (2030) simulations, the changes in atmospheric deposition calculated by global chemistry–transport models are applied to the present-day observed fluxes. The impact of the atmospheric deposition on the fluxes of carbon in the food chain is calculated together with the contribution of human activities to these impacts. The results show that total phytoplanktonic biomass increased by 16% over the past 1.5 centuries. Small fractional changes in carbon fluxes and planktonic biomasses are predicted for the near future. Simulations show that atmospheric deposition of N and P may be the main mechanism responsible for the anomalous N:P ratio observed in the Mediterranean Sea.


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