Academic literature on the topic 'Mer du Levant'
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Journal articles on the topic "Mer du Levant"
Vatin, Nicolas. "Les premiers exploits en mer des frères Barberousse." Journal des savants 2, no. 1 (2020): 611–27. http://dx.doi.org/10.3406/jds.2020.6434.
Full textBrumont, Francis. "Marins et marchands marseillais en Normandie vers 1570." Annales du Midi : revue archéologique, historique et philologique de la France méridionale 132, no. 311 (2020): 315–33. http://dx.doi.org/10.3406/anami.2020.9056.
Full textHocquet, Jean-Claude. "L’Adriatique, golfe de Venise? Commerce, ports et relations à la fin du Moyen Âge." Anales de la Universidad de Alicante. Historia Medieval, no. 23 (May 26, 2022): 13. http://dx.doi.org/10.14198/medieval.20224.
Full textHeyberger, Bernard. "Le catholicisme tridentin au Levant (XVIIe-XVIIIe siècles)." Mélanges de l’École française de Rome. Italie et Méditerranée 101, no. 2 (1989): 897–909. http://dx.doi.org/10.3406/mefr.1989.4069.
Full textWall, Erika. "Levande samtal om den odödliga Henrietta: Biografin som stöd för reflekterande diskussion och lärande." Högre utbildning 11, no. 2 (2021): 46. http://dx.doi.org/10.23865/hu.v11.2971.
Full textRos, Nathalie. "¿Compartir o repartir? Retos de delimitación marítima en el Mediterráneo oriental." Revista Estudios Jurídicos. Segunda Época, no. 23 (September 25, 2023): e7888. http://dx.doi.org/10.17561/rej.n23.7888.
Full textLundegård, Iann, and Helen Hasslöf. "Antropocen och utbildning – direkta naturmöten och demokratiska processer." Pedagogisk forskning i Sverige 27, no. 3 (November 1, 2022): 54–71. http://dx.doi.org/10.15626/pfs27.03.04.
Full textHeyberger, Bernard. "Pro nunc, nihil respondendum. Recherche d'information et prise de décision à la Propagande : l'exemple du Levant (XVIIIe siècle)." Mélanges de l’École française de Rome. Italie et Méditerranée 109, no. 2 (1997): 539–54. http://dx.doi.org/10.3406/mefr.1997.4503.
Full textÆsøy, Knut Ove. "Om læraren sin levande kunnskap." Studier i Pædagogisk Filosofi 7, no. 2 (January 9, 2020): 58–72. http://dx.doi.org/10.7146/spf.v7i2.115630.
Full textKfoury, Mira. "Tracing working-class cultural historical heritage through one building's story: 'La Grande Brasserie du Levant'." Journal of Urban Cultural Studies 6, no. 2 (September 1, 2019): 287–310. http://dx.doi.org/10.1386/jucs_00014_1.
Full textDissertations / Theses on the topic "Mer du Levant"
Papadimitriou, Nikolaos. "Geodynamics and synchronous filling of a rift type-basin evolved through compression tectonics (The western margin of the Levant Basin)." Electronic Thesis or Diss., Paris 6, 2017. http://www.theses.fr/2017PA066540.
Full textThe Eastern Mediterranean owes its complex nature to the movement of Africa, Arabia and Eurasia. The recent gas discoveries in the Levant Basin (2009) provoked the necessity of necessity of conducting a combined (seismic and field) study to better understand the geological evolution of the Basin. The combination of geophysical and field data allows the conceptualization of onshore and, offshore 3D models in order to characterize the tectonostratigraphic evolution of this area and eventually trace the main sources and pathways that contributed to the infilling of the Levant Basin. The evolution of the Levant Basin is marked by the transition from a pure carbonate system to a mix system (carbonate /siliciclastic) during the Cenozoic. The Eratosthenes block corresponds to a fault block platform. Four major seismic sequences, characterized by periods of aggradation, retrogradation and progradation, punctuated by major unconformities and drowning surfaces have been recognized on the Eratosthenes Seamount. These periods are: the Late Jurassic; the Early Cretaceous, the Late Cretaceous and the Miocene. The initiation of the collision during the Miocene between the African and Eurasian plates coincides with the uplift of the Eratosthenes Seamount with a peak during the upper Miocene (pre-Messinian Salinity Crisis) followed by its northward tilting under Cyprus thrusting. We show that the collision of the two plates caused the formation of small basins in southern part of Cyprus; a piggyback basin (Polis), and a flexural basin (Limassol) that were controlled by the different substratum of the Mesozoic sediments
Abbani, Ghina. "Geophysical characterization of a carbonate platform reservoir based on outcrop analogue study (onshore, Lebanon)." Electronic Thesis or Diss., Sorbonne université, 2023. http://www.theses.fr/2023SORUS393.
Full textReservoir characterization in frontier basins remains a challenge for exploration efforts. The Levant Basin, located in the easternmost part of the Mediterranean region, represents a frontier basin that is extensively mapped in terms of seismic survey but lacks well log calibration. The sparse data coverage results in substantial uncertainties in seismic interpretation and evaluation of reservoir properties. In the absence of well data, outcrop analogues can play a key role in the characterization of subsurface carbonate platforms. The main objective of this thesis is to characterize a large-scale Cenomanian – Turonian carbonate platform located northern Lebanon based on integrating sedimentological characterization with geophysical and petrophysical measurements. The investigation of the onshore analogue outcrop allows to constrain the carbonate platform’s properties on onshore seismic data. The developed approach is first applied to the Mid – Late Bathonian limestones of Massangis quarry (Oolithe Blanche formation), representing an analogue of the geothermal reservoir targeted by many municipalities in the Ile-de-France region. Sedimentologic description is completed for the studied outcrop and petrographic analysis is accomplished for representative samples. A total of 1000 acoustic velocities are acquired at 40 kHz to generate a 2D synthetic seismogram. The sedimentologic and acoustic characterization of the section allows to understand the influence of facies variation and diagenetic features (firm grounds, bioturbation, stylolites, etc) on the acoustic measurements and the generation of seismic reflectors. The studied outcrop in Kfarhelda northern Lebanon is a Cenomanian – Turonian shallow marine carbonate platform representing Sannine and Maameltain formations. The formations represent bedded limestones with important Turonian rudist-rich rudstones. A thorough sedimentary description is completed for the 400 m-thick carbonate platform. P-wave velocity is acquired directly on the outcrop, and the petrophysical properties are measured on 44 representative samples. The data are used to generate a 1D synthetic seismogram with a 25 Hz Ricker wavelet. The resulting reflectors are mainly (1) high amplitude reflectors at the limit between two facies with contrasting physical properties enhanced by diagenesis, (2) moderate amplitude reflectors corresponding to stratigraphic limits at the transition between facies, and (3) very low amplitude reflectors in karstified units. The integration of outcrop and seismic data is based on the generation of the synthetic seismogram. Interpretation and seismic facies analysis are completed for the 2D onshore seismic profile acquired in 2013. The best fit between the synthetic seismic and seismic profile resulted in the identification of two distinctive reflectors related to the Marly Limestone Zone causing sharp contrast in acoustic impedance, and the overlying channel facies characterised by higher porosity. The approach developed in this thesis work highlights the importance of combining sedimentologic and acoustic measurements together with synthetic seismic modelling to identify the geological origin of seismic reflectors and improve the seismic interpretation in terms of facies and reservoir properties
Symeou, Vasilis. "Transition from compression to strike-slip tectonic styles along the northern margin of the Levant Basin." Electronic Thesis or Diss., Sorbonne université, 2018. http://www.theses.fr/2018SORUS003.
Full textThe Cyprus Arc system is major plate boundary of the Eastern Mediterranean where different plates interact, namely Arabia, Africa, Eurasia, as well as the Anatolian micro-plate. It constitutes the northern boundary of the Levant Basin (of thin stretched continental crust) and the Herodotus Basin (of oceanic crust). The Cyprus Arc is directly linked with the northward convergence of the African continental plate with respect to the Eurasian continental plate since Late Cretaceous time. The indentation of the Arabian plate and the slab pull effect of the African plate roll back in the Aegean region on the eastern and western part of the Anatolian plate respectively, leads to the westward escape of Anatolia from Late Miocene to Recent, which results in a strike-slip component along the Cyprus Arc system and onshore Cyprus. Several scientific questions with regard to the geological setting of the region were investigated during this project. How is the deformation accommodated at the Cyprus Arc system? Is this deformation style affected by the variation of the crustal nature at each domain? How is this deformation recorded on the sedimentary pile onshore Cyprus? How does the onshore and offshore deformation connect within the geodynamic context of the region? In order to answer these scientific questions, 2D reflection seismic data were utilized, that image the main plate structures and their lateral evolution south and east of Cyprus. Interpretation of these data lead to the identification of nine tectono-sedimentary packages in three different crustal domains south of the Cyprus Arc system: (1) The Levant Basin (attenuated continental crust), (2) The Eratosthenes micro-continent (continental crust) and (3) The Herodotus Basin (oceanic crust). Within these domains, numerous tectonic structures were documented and analysed in order to understand the mechanism and timing of deformation. At the northern boundary of the Levant Basin domain, thrust faults verging towards the south were documented in the Cyprus Basin with the thrust movement commencing in Early Miocene time as indicated by on the Larnaca and Margat Ridges. On the Latakia Ridge no activity was identified during this time interval. The acme of deformation occurred in Middle to Late Miocene time, with the activity of the Latakia Ridge indicating the forward propagation of the deformation front towards the south. This southward migration was documented from the development of flexural basins and from stratigraphic onlaps in the Cyprus Basin. Successive tectonic pulses through the Late Miocene until Recent times, are indicated from the angular unconformities and the piggy back basins. In Plio-Pleistocene time, the westward escape of the Anatolian micro-plate resulted in the reactivation of existing structures. The evolution of deformation along the plate boundary is identified from the creation of positive flower structures revealing transpressive movements along the Larnaca and Latakia Ridges (eastern domains). The central domain includes the Eratosthenes Seamount which is characterized as a Mesozoic carbonate platform covered by a thin sequence of sediments ranging from Miocene-Messinian to Pliocene-Pleistocene depositions
Papadimitriou, Nikolaos. "Geodynamics and synchronous filling of a rift type-basin evolved through compression tectonics (The western margin of the Levant Basin)." Thesis, Paris 6, 2017. http://www.theses.fr/2017PA066540/document.
Full textThe Eastern Mediterranean owes its complex nature to the movement of Africa, Arabia and Eurasia. The recent gas discoveries in the Levant Basin (2009) provoked the necessity of necessity of conducting a combined (seismic and field) study to better understand the geological evolution of the Basin. The combination of geophysical and field data allows the conceptualization of onshore and, offshore 3D models in order to characterize the tectonostratigraphic evolution of this area and eventually trace the main sources and pathways that contributed to the infilling of the Levant Basin. The evolution of the Levant Basin is marked by the transition from a pure carbonate system to a mix system (carbonate /siliciclastic) during the Cenozoic. The Eratosthenes block corresponds to a fault block platform. Four major seismic sequences, characterized by periods of aggradation, retrogradation and progradation, punctuated by major unconformities and drowning surfaces have been recognized on the Eratosthenes Seamount. These periods are: the Late Jurassic; the Early Cretaceous, the Late Cretaceous and the Miocene. The initiation of the collision during the Miocene between the African and Eurasian plates coincides with the uplift of the Eratosthenes Seamount with a peak during the upper Miocene (pre-Messinian Salinity Crisis) followed by its northward tilting under Cyprus thrusting. We show that the collision of the two plates caused the formation of small basins in southern part of Cyprus; a piggyback basin (Polis), and a flexural basin (Limassol) that were controlled by the different substratum of the Mesozoic sediments
Le, Béon Maryline. "Cinématique d'un segment de faille décrochante à différentes échelles de temps : la faille du Wadi Araba, segment sud de la faille transformante du Levant." Paris, Institut de physique du globe, 2008. http://www.theses.fr/2008GLOB0001.
Full textThe Dead Sea fault is the transform plate boundary between the Arabia plate and theSinai sub-plate. This manuscript focuses on the Wadi Araba fault segment, located betweenthe Dead Sea basin and the Gulf of Aqaba. We aim at studying the slip rate of this faultsegment at different time scales, in order to better constrain the slip rate, which has beenestimated between 2 and 10 mm/yr depending on the authors, and to understand its seismicbehavior. Based on GPS campaign data distributed along three profiles perpendicular to thefault, we provide a present-day slip rate of 4. 9 +/- 1 1. 4 mm/yr since the last 6 years, betterconstrained than previous studies. Data processing in the ITRF2000 reference frame allowsinvestigating the relative kinematics between Arabia, Sinai and Africa (Nubia). Thegeomorphologic analysis and 10Be cosmogenic dating of alluvial surfaces offset by the faultinvalidate previous studies and yield a slip rate of 4. 6 +/- 2 mm/yr since ~12 ka, a minimumslip rate of 2. 3 mm/yr since ~50 ka and a slip rate of 7. 4 +/- 3 mm/yr since ~94 ka. Thegeomorphologic analysis at the scale of the Wadi Araba Valley, associated to 10Be exposureages, leads to a new morpho-tectonic map. The offset of large (~10 km long) abandonedalluvial surfaces at the centre of the valley is turned out not to be precise enough to bring newconstraints on the slip rate since the last 100-300 ka. Some sites however worth furtherinvestigation. Although our results complemented by previous studies do not excludevariations in fault slip rate at the time scale of a few ten thousands years, they agree on aconstant slip rate of 5 +/- 1 2 mm/yr and suggest that the Wadi Araba fault produces largeearthquakes (M > 6. 5) quasi-periodically. Combining all the ages obtained in the Wadi Arabasuggests a clustered distribution of ages that could correspond to periods characterized by ahumid climate, as recorded by various paleoclimatic proxies at the local, and possibly,regional scales
Symeou, Vasilis. "Transition from compression to strike-slip tectonic styles along the northern margin of the Levant Basin." Thesis, Sorbonne université, 2018. http://www.theses.fr/2018SORUS003/document.
Full textThe Cyprus Arc system is major plate boundary of the Eastern Mediterranean where different plates interact, namely Arabia, Africa, Eurasia, as well as the Anatolian micro-plate. It constitutes the northern boundary of the Levant Basin (of thin stretched continental crust) and the Herodotus Basin (of oceanic crust). The Cyprus Arc is directly linked with the northward convergence of the African continental plate with respect to the Eurasian continental plate since Late Cretaceous time. The indentation of the Arabian plate and the slab pull effect of the African plate roll back in the Aegean region on the eastern and western part of the Anatolian plate respectively, leads to the westward escape of Anatolia from Late Miocene to Recent, which results in a strike-slip component along the Cyprus Arc system and onshore Cyprus. Several scientific questions with regard to the geological setting of the region were investigated during this project. How is the deformation accommodated at the Cyprus Arc system? Is this deformation style affected by the variation of the crustal nature at each domain? How is this deformation recorded on the sedimentary pile onshore Cyprus? How does the onshore and offshore deformation connect within the geodynamic context of the region? In order to answer these scientific questions, 2D reflection seismic data were utilized, that image the main plate structures and their lateral evolution south and east of Cyprus. Interpretation of these data lead to the identification of nine tectono-sedimentary packages in three different crustal domains south of the Cyprus Arc system: (1) The Levant Basin (attenuated continental crust), (2) The Eratosthenes micro-continent (continental crust) and (3) The Herodotus Basin (oceanic crust). Within these domains, numerous tectonic structures were documented and analysed in order to understand the mechanism and timing of deformation. At the northern boundary of the Levant Basin domain, thrust faults verging towards the south were documented in the Cyprus Basin with the thrust movement commencing in Early Miocene time as indicated by on the Larnaca and Margat Ridges. On the Latakia Ridge no activity was identified during this time interval. The acme of deformation occurred in Middle to Late Miocene time, with the activity of the Latakia Ridge indicating the forward propagation of the deformation front towards the south. This southward migration was documented from the development of flexural basins and from stratigraphic onlaps in the Cyprus Basin. Successive tectonic pulses through the Late Miocene until Recent times, are indicated from the angular unconformities and the piggy back basins. In Plio-Pleistocene time, the westward escape of the Anatolian micro-plate resulted in the reactivation of existing structures. The evolution of deformation along the plate boundary is identified from the creation of positive flower structures revealing transpressive movements along the Larnaca and Latakia Ridges (eastern domains). The central domain includes the Eratosthenes Seamount which is characterized as a Mesozoic carbonate platform covered by a thin sequence of sediments ranging from Miocene-Messinian to Pliocene-Pleistocene depositions
Lupo, Sébastien. "Révolution(s) d'échelles : Le marché levantin et la crise du commerce marseillais au miroir des maisons Roux et de leurs relais à Smyrne (1740-1787)." Thesis, Aix-Marseille, 2015. http://www.theses.fr/2015AIXM3030.
Full textThe capitulations granted by the Porte in 1740 set a favourable framework for French trade in Levant. However, the 18th century means decline for it. Smyrna, which emerged at that time as the first Ottoman échelle, offered a fitting place to observe and to understand this crisis stemming from the debasement of exchange rates and woolen clothes, the most exported articles. And yet, the Roux company from Marseilles established a firm in Smyrna in 1759 after turning to outsiders. Thanks to the contributions of economic sociology, this research shows that the Levantine context, prone to revolutions of all kinds, didn't offer all the expected amenities. The social structure legally enforced and dominated by the merchants of Marseilles worked in accordance to embedded cautiousness which likened the expatriated partners to potentially opportunist subordinates. Such an organization hampered their activity in the Eastern market. Whereas the Mediterranean became an outlying space for world trade, the Roux failed to develop their Levantine firm despite the diversity of their networks. The domination of Marseilles over the clothing industry in Languedoc contributed, in fact, to its jeopardizing and the quality decline of its products. At the end of the Seven Years' War, these exportations entered in a declining stage maintained by the inertia of the merchants' practices which also account for the lack of diversification. Thus, network defects combine with the complexity of the Levantine market, the geopolitical troubles of the 18th century and the transition to English hegemony to explain the crisis of the Levantine trade from Marseilles
Baaklini, Georges. "Characterization of the Eastern Mediterranean surface dynamics : Insights from drifter assimilation and machine learning techniques." Electronic Thesis or Diss., Sorbonne université, 2022. http://www.theses.fr/2022SORUS186.
Full textAn accurate estimation of the surface circulation is crucial because of its direct impact on physical and bio-geochemical water properties. However, currents estimation remains challenging because the stream field is affected by quickly changing flows. This problem increases in the Eastern Mediterranean Sea, where in-situ observations are relatively scarce and the inaccuracies of altimetric observations increase. Therefore, some of the mesoscale features are still debated or unknown, especially in the Levantine Basin. The thesis goal is to characterize these highly-evolving mesoscale features. In the first part of the thesis, we present a variational assimilation method that merges altimetry with drifters to improve the surface circulation representation along and around the assimilated drifters’ trajectories. We assess the method’s efficiency by comparing the velocities resulting from assimilation with independent in-situ observations and ocean color images. We use the corrected velocities to characterize short-term and local events occurring in the Levantine Basin. However, because of the significant spatio-temporal gaps in drifters’ coverage, the assimilation does not allow a continuous investigation of all the mesoscale patterns and their long-term variabilities in the basin. In the second part of the thesis, we use machine learning techniques to build a catalog of the several circulation regimes in the Levantine Basin, providing a long-term characterization of these features. We also try to explain the possible reasons behind previous contradictory assessments about some features, such as the Mid-Mediterranean Jet. The obtained results in the thesis improve the knowledge of the main mesoscale features’ characteristics, behaviors, and tendencies. The thesis applications could take advantage of other in-situ observations and of future altimetric missions like SWOT, promising to mitigate some of the actual altimetric shortcomings
Bustad, Ola. "Gör Historien mer levande i klassrummet : En intervjustudie om hur historieämnet, genom artefakter, kan göras mer levande i klassrummet." Thesis, Karlstads universitet, Institutionen för samhälls- och kulturvetenskap (from 2013), 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:kau:diva-69308.
Full textTahchi, Elias. "Le bassin Levantin et l'Arc de Chypre : processus sédimentaires et structuraux le long d'une frontière de plaque sous-marine." Perpignan, 2007. http://www.theses.fr/2007PERP0818.
Full textThe convergence of Eurasian and African plates started since the Cretaceous by a succession of subduction and pre-collision zones that witness a closure process of the Mediterranean. The Cyprus Arc is the easternmost segment of this Mediterranean convergence system which got complicated with the westward extrusion of the Anatolian microplate. This movement generates in the Eastern Mediterranean and in particularly along the Cyprus Arc a complex tectonic regime. During the research cruise BLAC in 2003 onboard the R/V Le Suroît, 20. 000 sq Km of seafloor has been mapped including the easternmost segment of Cyprus Arc and going from Hecataeus Seamount till the Syrian margins. The following data have been acquired continuously and in a simultaneous way: Multibeam bathymetry and backscatter imagery with the multibeam echousounder EM300, 6-traces seismic reflection, subbottom sediment echousounder (CHIRP), gravity and magnetic data. This manuscript gives structural and morphological analysis of the easternmost segment of the Cyprus Arc as well as a detailed study of gravity induced instabilities on the Syrian margin and the different mud and salt activities in the adjacent basins of the Cyprus Arc
Books on the topic "Mer du Levant"
Les Français du Levant dans la tourmente de la Révolution (1789-1814): Les echelles de la mer Egée. İstanbul: Libra Kitapçılık ve Yayıncılık, 2018.
Find full textDöd men ganska levande. [Stockholm]: Podium, 2012.
Find full textOoggetuigen van de vaderlandse geschiedenis in meer dan honderd reportages. 2nd ed. Amsterdam: Bakker, 2007.
Find full textDal Mar Nero al delta del Nilo: I pisani e i loro commerci nel Levante (secoli XIII-XIV). Udine: Forum, 2021.
Find full textMen in the public eye: The construction and deconstruction of public men and public patriarchies. London: Routledge, 1992.
Find full textSetti, Cristina. Una repubblica per ogni porto: Venezia e lo Stato da Mar negli itinerari dei Sindici inquisitori in Levante (secoli XVI-XVII). [Milan]: Edizioni Unicopli, 2021.
Find full textSeligman, Adrian. War in the Islands: Undercover operations in the Aegean 1942-4 ; recalled by men of the Levant Schooner Flotilla, the Greek Sacred Company and Aegean Raiding Forces. Stroud, Gloucestershire: A. Sutton Pub., 1996.
Find full textLehtipuu, Outi, and Michael Labahn, eds. Tolerance, Intolerance, and Recognition in Early Christianity and Early Judaism. NL Amsterdam: Amsterdam University Press, 2021. http://dx.doi.org/10.5117/9789462984462.
Full textA republic of men: The American founders, gendered language, and patriarchal politics. New York: New York University Press, 1998.
Find full textYe heart of a man: The domestic life of men in colonial New England. New Haven, Conn: Yale University Press, 1999.
Find full textBook chapters on the topic "Mer du Levant"
Kat, Fiona, Maura Beenackers, and Willemijn ter Brugge. "Wat is er met me aan de hand?" In Leven met ADHD, 11–28. Houten: Bohn Stafleu van Loghum, 2009. http://dx.doi.org/10.1007/978-90-313-6925-6_1.
Full textKat, Fiona, Maura Beenackers, and Willemijn ter Brugge. "Hoe heeft het zover kunnen komen?" In Leven met ADHD, 29–37. Houten: Bohn Stafleu van Loghum, 2009. http://dx.doi.org/10.1007/978-90-313-6925-6_2.
Full textKat, Fiona, Maura Beenackers, and Willemijn ter Brugge. "Wat staat me te wachten?" In Leven met ADHD, 39–50. Houten: Bohn Stafleu van Loghum, 2009. http://dx.doi.org/10.1007/978-90-313-6925-6_3.
Full textKat, Fiona, Maura Beenackers, and Willemijn ter Brugge. "Wat betekent ADHD voor mij en mijn omgeving?" In Leven met ADHD, 51–60. Houten: Bohn Stafleu van Loghum, 2009. http://dx.doi.org/10.1007/978-90-313-6925-6_4.
Full textKat, Fiona, Maura Beenackers, and Willemijn ter Brugge. "Wat kan ik er zelf aan doen?" In Leven met ADHD, 61–79. Houten: Bohn Stafleu van Loghum, 2009. http://dx.doi.org/10.1007/978-90-313-6925-6_5.
Full textKat, Fiona, Maura Beenackers, and Willemijn ter Brugge. "Welke behandelingen bestaan er?" In Leven met ADHD, 81–94. Houten: Bohn Stafleu van Loghum, 2009. http://dx.doi.org/10.1007/978-90-313-6925-6_6.
Full textKat, Fiona, Maura Beenackers, and Willemijn ter Brugge. "Adressen en literatuur." In Leven met ADHD, 95–98. Houten: Bohn Stafleu van Loghum, 2009. http://dx.doi.org/10.1007/978-90-313-6925-6_7.
Full textvan Schayck, C. P., and G. Wesseling. "Wat is er met me aan de hand?" In Leven met COPD, 17–32. Houten: Bohn Stafleu van Loghum, 2010. http://dx.doi.org/10.1007/978-90-313-7580-6_1.
Full textvan Schayck, C. P., and G. Wesseling. "Hoe ontstaat COPD?" In Leven met COPD, 33–44. Houten: Bohn Stafleu van Loghum, 2010. http://dx.doi.org/10.1007/978-90-313-7580-6_2.
Full textvan Schayck, C. P., and G. Wesseling. "Wat staat me te wachten?" In Leven met COPD, 45–56. Houten: Bohn Stafleu van Loghum, 2010. http://dx.doi.org/10.1007/978-90-313-7580-6_3.
Full textConference papers on the topic "Mer du Levant"
Souza, Isabella Cristina Cantelles de, Enzo Henrique Morás, and Isabel Ribeiro Do Valle Teixeira. "UMA REVISÃO DE LITERATURA: ATIVIDADE ANTIMICROBIANA DO MEL DERIVADO DE ABELHAS SEM FERRÃO." In II Congresso Brasileiro de Ciências Biológicas On-line. Revista Multidisciplinar Educação e Meio Ambiente, 2021. http://dx.doi.org/10.51189/rema/1657.
Full textBarbosa, Francisco Ronald Araújo, Antonio Rafael Braga, and Danielo G. Gomes. "Aplicando Blockchain Hyperledger Iroha para Rastrear Mel de Abelha." In Workshop de Computação Aplicada à Gestão do Meio Ambiente e Recursos Naturais. Sociedade Brasileira de Computação - SBC, 2023. http://dx.doi.org/10.5753/wcama.2023.229849.
Full text"Genetikai adatok az Urál vidék kora középkori temetkezéseiből a korai magyarsággal kapcsolatba hozható régészeti hagyaték tükrében." In „Hadak útján” : A népvándorláskor fiatal kutatóinak XXIX. konferenciája. Bölcsészettudományi Kutatóközpont Magyar Őstörténeti Kutatócsoport, PPKE BTK Régészettudományi Intézet, Martin Opitz Kiadó, 2023. http://dx.doi.org/10.55722/arpad.kiad.2023.4.2_06.
Full textLinge, Sara, and Iulia Mircan. "The Green Way." In SLM ONLINE: Projektarbeten från kandidatprogrammet Språk, litteratur och medier. Linköping University Electronic Press, 2023. http://dx.doi.org/10.3384/wcc30/thegreenway.
Full textCunha Ribeiro, Victor, Maria Júlia Silva Moreira de Souza, Laura Abreu Lhamas, Juliana Batalha Pereira Rampazzo, and Márcia Azevedo Caldas. "Bradicardia sinusal sintomática por hipermagnesemia após automedicação em paciente com doença renal crônica: um relato de caso." In Semana Científica da Faculdade de Medicina de Campos. Faculdade de Medicina de Campos, 2023. http://dx.doi.org/10.29184/anaisscfmc.v22023p52.
Full textLima, Nathália Oliveira, Nádilla Gonçalves Andrade, Laiza Bezerra Lima, Joelson Sousa Junior, and Gabriel Pereira Imolesi Barbosa. "POLINIZANDO O SABER: PROJETO LEVA EDUCAÇÃO AMBIENTAL PARA CRIANÇAS E JOVENS UTILIZANDO ABELHAS COMO MODELO EDUCACIONAL." In I Congresso Nacional On-line de Conservação e Educação Ambiental. Revista Multidisciplinar de Educação e Meio Ambiente, 2021. http://dx.doi.org/10.51189/rema/1805.
Full textBoschini, Fernanda, and Sueli Batista. "Desafios para a rede federal de educação profissional e tecnológica: um estudo a partir da criação e expansão dos Institutos Federais." In IX Simpósio Internacional Trabalho, Relações de Trabalho, Educação e Identidade. SITRE, 2022. http://dx.doi.org/10.47930/1980-685x.2022.1604.
Full textCunha, José, José Jr., Lívia Cunha, and Hermano Moura. "Melhoria de Processos de Software sob a Perspectiva dos Vieses Cognitivos: Uma Análise de Múltiplos Casos." In XI Simpósio Brasileiro de Sistemas de Informação. Sociedade Brasileira de Computação, 2015. http://dx.doi.org/10.5753/sbsi.2015.5825.
Full textCarvalho, Luiz Paulo, Flávia Maria Santoro, Jonice Oliveira, and Rosa Maria Costa. "Ética e Jogos, jogo ético e ética em jogo." In Anais Estendidos do Simpósio Brasileiro de Games e Entretenimento Digital. Sociedade Brasileira de Computação, 2021. http://dx.doi.org/10.5753/sbgames_estendido.2021.19752.
Full textVERDE, ANTONIO AUGUSTO GOES FERREIRA LIMA, and MARCOS ANTONIO CHAVES RICARTE. "ESTRATÉGIAS EMERGENCIAIS ADOTADAS PELAS INSTITUIÇÕES SUPERIORES BRASILEIRA FRENTE A PANDEMIA DO COVID-19." In 26º CIAED Congresso Internacional ABED de Educação a Distância. Associação Brasileira de Educação a Distância - ABED, 2020. http://dx.doi.org/10.17143/ciaed.xxviciaed.2020.54511.
Full textReports on the topic "Mer du Levant"
Nyström, Per, Marika Stenberg, Lennart Edsman, and Patrik Bohman. Flodkräfta och flodkräftodling i Sverige : en handbok baserad på erfarenheter. Institutionen för akvatiska resurser, Sveriges lantbruksuniversitet, 2023. http://dx.doi.org/10.54612/a.3io2b8ki32.
Full textAsztalos Morell, Ildikó, Isak Falk-Eliasson, and Robin Eriksson. Urfolksperspektiv på livsmedelsstrategin. SLU Future food, Swedish University of Agricultural Sciences, 2023. http://dx.doi.org/10.54612/a.5m806l8ijt.
Full textLarsson, Stefan, Alessandro Orio, Filip Svensson, Håkan Wennhage, and Jens Olsson. Indikatorrapportering för “Hållbart nyttjande av fisk- och skaldjursbestånd i kust och hav” : bedömningsåret 2022. Institutionen för akvatiska resurser, Sveriges lantbruksuniversitet, 2023. http://dx.doi.org/10.54612/a.1dtcvdo2tc.
Full textHellström, Lisa. Hur mår våra barn och unga? : Förändringar i barns och ungas hälsa över tid: en kunskapsöversikt. Malmö universitet; Malmö kommun, 2023. http://dx.doi.org/10.24834/isbn.9789178773794.
Full textAdill, Anders, Ingrid Bergman, Stefan M. Eiler, Per B. Holliland, and Carolina Åkerlund. Biologisk recipientkontroll vid Forsmarks kärnkraftverk : årsrapport för 2022. Institutionen för akvatiska resurser, Sveriges lantbruksuniversitet, 2023. http://dx.doi.org/10.54612/a.1ds9nbsbl6.
Full textBerg, Charlotte, Rie Henriksen, Anders Herlin, Ruben Hoffman, Magdalena Jacobson, Desirée Jansson, Linda Keeling, et al. Hållande av vaktel. SLU:s vetenskapliga råd för djurskydd, 2023. http://dx.doi.org/10.54612/a.3hlcu79vvb.
Full textRodriguez, Emily, Sigrid Jansson, Alexander Olsson, Anders Hansson, and Mathias Fridahl. Klimatansvar i Stockholms stad. Linköping University Electronic Press, November 2023. http://dx.doi.org/10.3384/report-199063.
Full textJärnland, Erik, Fredrik Garcia, and Elin Wihlborg. Kommunernas lägesbildsrapportering under Covid-19 pandemin: Ett medel för regional samverkan eller statlig styrning? Linköping University Electronic Press, January 2024. http://dx.doi.org/10.3384/dino-2023.1.
Full textAhammad, Ronju, and Francisco X. Aguilar. Socioekonomiska indikatorer för hållbart skogsbruk - och användning i svenska miljömålssystemet. SLU Future forests, Swedish University of Agricultural Sciences, 2024. http://dx.doi.org/10.54612/a.4s34ii4mn9.
Full textLarsson, Stefan, Filip Svensson, Håkan Wennhage, and Jens Olsson. Indikatorrapportering för “Hållbart nyttjande av fisk- och skaldjursbestånd i kust och hav” : bedömningsåret 2023. Department of Aquatic Resources, Swedish University of Agricultural Sciences, 2024. http://dx.doi.org/10.54612/a.1p05qqkdqa.
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