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Journal articles on the topic 'Panafricain'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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1

Mare, D. "Joseph ki-zerbo et le panafricanisme." Contemporary Journal of African Studies 6, no. 1 (2019): 59–75. http://dx.doi.org/10.4314/contjas.v6i1.4.

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Joseph Ki-Zerbo a mené sa vie entière dans le combat panafricaniste. Son parcours panafricain s’est consolidé à travers des rencontres à son initiative personnelle mais aussi grâce à des occasions avec les grands panafricanistes de renom comme le « prophète » Kwame Nkrumah, Amilcar Cabral, Patrice Lumumba, Julius Nyerere etc. Il arriva à joindre l’acte à la parole par exemple en allant prêter main forte à Sékou Touré en 1958, en ayant travaillé à exhumer le passé de l’africain. L’Afrique doit être libérée, et cette libération se fera obligatoirement de façon panafricaine ou elle n’aura jamais lieu. C’est pourquoi, l’Africain doit s’imprégner de son passé pour comprendre les réalités et les obstacles présents qui se posent à lui afin d’envisager les grandes lignes du combat panafricain pour un avenir meilleur. La lecture de l’engagement de Ki-Zerbo se veut une présentation d’un modèle phare pour les jeunes voués et engagés dans le sens du panafricanisme.

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2

Blade Babène, Frank. "L'ombre d'un rêve panafricain." Africultures 98, no. 2 (2014): 214. http://dx.doi.org/10.3917/afcul.098.0214.

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3

Mukeredzi, Tonderayi. "Passeport panafricain, au-delà des frontières." Afrique Renouveau 30, no. 2 (2016): 20–21. http://dx.doi.org/10.18356/e190b6c2-fr.

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4

GUEDJ, Pauline. "Africain, Akan, Panafricain et Afro-Américain." Civilisations, no. 58-1 (August 31, 2009): 73–92. http://dx.doi.org/10.4000/civilisations.1925.

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5

Renault, Matthieu. "Festival culturel panafricain d’Alger (7-8 juillet 2009)." Journal des anthropologues, no. 118-119 (December 1, 2009): 381–86. http://dx.doi.org/10.4000/jda.4194.

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6

Crosta, Suzanne. "Des désastres écologiques au rêve panafricain d’une Grande Muraille verte." International Journal of Francophone Studies 23, no. 3 (2020): 243–62. http://dx.doi.org/10.1386/ijfs_00020_1.

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Since the late twentieth century, African filmmakers have devoted themselves with tireless dedication and activism to environmental challenges that continue to alarm, even globally. Their lands are endangered, and their communities are severely affected in their living environment. There are major challenges, ever more urgent, about their ecosystems, but also about the neighbouring geographies and finally about the planet in general. Using a body of documentaries concerned with ecosystems on the continent, this study examines African filmmakers’ perspectives on ecosystem degradation in various African contexts while highlighting the ethics and aesthetics of their practices confronting the representation of a seemingly dystopian world. In response to the alarming discourses and desolate visions, this article underscores the filmmakers’ response to urgent ecological needs, and examines their activism in the search for green solutions in Africa.

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7

Balde, M. S., M. I. Buaro, O. K. Konstantinov, M. S. Diallo, E. Millimono, and M. Kulibali. "Trial of the new antivenin serum INSERP®PANAFRICAIN in the Republic of Guinea for the treatment of patients bitten by venomous snakes." Epidemiology and Infectious Diseases 21, no. 1 (2016): 36–40. http://dx.doi.org/10.17816/eid40896.

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Introduction The intoxication rate due to venomous snake bites in the population in the Republic of Guinea is 100-150 cases per 100 000 habitants with the mortality rate to 18% and represents a serious problem for public health services of the country. In the same time there is a big lack in antivenin sera supply. Nevertheless, the provision with antivenin serum against snake venom in the country is evidently not enough. Aim of research clinical trials of the efficiency and tolerance of a new polyvalent antivenin sera Inoserp® Panafricain against snake venom in comparison with the used previously serum Antivipmyn® Afrique. Methods There were treated 109 patients with pronounced symptoms of intoxication due to venomous snake bites. In the absence of hemolytic and neurologic symptoms they were intravenously administered the 1 dose (10 ml) of serum or 2 doses in the presence of mentioned symptoms. If situation so requires (in the absence of the positive effect, the occurrence of hemorrhage and neurological symptoms) this serum was re-administered 3, 6, 12 or 24 hours after the first injection. There was noted a status ofpatient and the presence of side effects after the application of this serum. Results All 109 patients have received an average of 1.1 doses (ampules) of serum. 108 patients (99%) recovered without consequences. No case of necrosis was observed. There was noted the 1 fatal case (0.9% of total patients). In 6 (5.5%) patients 10 minutes after administration of the serum there were noted side effects, but shortly they disappeared. The overall mortality rate in our experience was lower than in the testing of the similar serum Antivipmyn® Afrique, especially in patients who have not received antisera against the venom of snakes. Conclusion The efficacy and tolerability of the Inoserp® Panafricain serum were higher as mortality rate (0.9%) and side effects (5.5%) - lower in comparison with the serum Antivipmyn® Afrique. This experience has shown the perspectiveness of the use of serum Inoserp® Panafricain for the treatment of cases bitten by venomous snakes in Guinea.

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8

African Yearbook of International L, Editor. "PROTOCOLE A L’ACTE CONSTITUTIF DE L’UNION AFRICAINE RELATIF AU PARLEMENT PANAFRICAIN." African Yearbook of International Law Online / Annuaire Africain de droit international Online 20, no. 1 (2014): 546–62. http://dx.doi.org/10.1163/22116176-90000156.

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9

Lam, Absa, Mathilde Cabral, Aminata Touré, et al. "Évaluation de l’efficacité et la tolérance de Inoserp® Panafricain au Sénégal." Toxicologie Analytique et Clinique 31, no. 1 (2019): 18–29. http://dx.doi.org/10.1016/j.toxac.2018.12.008.

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10

Marcoux, Éric, and Michel Jébrak. "Plombotectonique des gisements du Maroc." BSGF - Earth Sciences Bulletin 192 (2021): 31. http://dx.doi.org/10.1051/bsgf/2021019.

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La synthèse de 240 analyses isotopiques du plomb, mesurées sur les gisements miniers marocains d’âges édiacarien à néogène appartenant à tous les domaines géotectoniques du Maroc autorise une réflexion globale sur la métallogénie du Maroc. Les compositions isotopiques varient grandement, de 17,738 (Bou Skour) à 18,905 (Draa Sfar) pour le rapport 206Pb/204Pb, et de 15,521 à 15,706 pour le rapport 207Pb/204Pb. La source du plomb des gisements étudiés se situe dans la croûte continentale supérieure, excepté pour ceux de l’Anti-Atlas (Bou Skour, Imiter…) et certains du Haut-Atlas (Azegour) à nette contribution du manteau. Les variations isotopiques relevées à l’échelle d’un district résultent soit de la présence de plusieurs événements hydrothermaux superposés sollicitant différentes sources locales comme à Tighza, soit d’un seul événement perturbé par la segmentation d’un bassin volcanosédimentaire, comme pour les amas sulfurés des Jebilet et Guemassa. À l’échelle du gisement (Draa Sfar, Bou Skour), les variations isotopiques résultent de la superposition de plusieurs événements hydrothermaux avec chacun leur propre plomb et métaux associés. Globalement, on peut distinguer trois générations de plomb incorporées successivement dans le socle géologique marocain par le magmatisme et/ou l’hydrothermalisme, caractérisées par leurs rapports 206Pb/204Pb : 17,74–17,90 (panafricain), 18,10–18,40 (hercynien) et 18,75–18,90 (alpin). Le plomb panafricain est présent dans l’Anti-Atlas, et très localement dans la Meseta (Bouznika), et se nourrit en partie du magmatisme mafique du Gondwana. Le plomb hercynien est le plus représenté et affiche une rupture définitive dans la source des métaux dès lors exclusivement crustale. Il envahit tous les domaines marocains, y compris l’Anti-Atlas, où il remobilise et se mélange avec le plomb panafricain. Le plomb alpin, plus discret, jalonne la large écharpe allant d’Agadir à Nador qui trace en surface le panache mantellique des Canaries et accompagne un magmatisme néogène qui peut aussi avoir agi comme simple moteur remobilisant le plomb hercynien, notamment pour former les gisements MVT de Touissit. Les plombs hercynien et alpin sont en partie responsables du rajeunissement des minéralisations néoprotérozoïques, comme à Bou Azzer ou Imiter. Le Maroc illustre le modèle de Sawkins avec un apport majeur du plomb lors du magmatisme fini-orogénique. Les résultats isotopiques plaident en faveur de remobilisations successives du plomb stocké dans des réservoirs primaires et secondaires avec des phénomènes d’héritage. Enfin le bon transfert de la signature isotopique du plomb des gisements aux gossans de surface, notamment pour les gisements stratiformes de sulfures polymétalliques de type Hajar, montre que la géochimie isotopique du plomb est un outil utilisable pour l’exploration minière au Maroc.

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11

Raschi, Nataša. "Sur la traduction du théâtre francophone africain : l’exemple de Werewere Liking." ALTERNATIVE FRANCOPHONE 1, no. 3 (2011): 79–86. http://dx.doi.org/10.29173/af9695.

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Nous concentrons ici notre attention sur la toute dernière production de Werewere Liking – Le Parler-Chanter et Médée – que nous avons traduite en italien. Auteur de pièces de théâtre, d’essais et de romans, mais aussi metteur en scène, peintre et écrivain, elle est originaire du Cameroun et, en 1985, a fondé à Abidjan (Côte d’Ivoire) un groupe de création artistique panafricain : la communauté du Village Ki-Yi. S’agissant d’œuvres créées en vue de la représentation scénique, plus aptes à être vues que lues, nous analysons les traits essentiels de ces textes, les multiples options offertes par la traduction et surtout les résultats obtenus.

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12

François, Isabelle. "Tshiyembe, Mwayila et Bukasa, Mayele. L’Afrique face à ses problèmes de sécurité et de défense. Paris, Institut Panafricain de Géopolitique, Coll. « Travaux et recherches de l’Institut Panafricain de Géopolitique », 1989, 263 p." Études internationales 21, no. 2 (1990): 437. http://dx.doi.org/10.7202/702685ar.

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13

Villeneuve, M. "Structure et evolution des bassins du Panafricain II dans la partie occidentale du craton ouest africain." Bulletin de la Société Géologique de France VI, no. 1 (1990): 155–65. http://dx.doi.org/10.2113/gssgfbull.vi.1.155.

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14

Lam, A., M. Cabral, A. Touré, M. Fall, A. Diouf, and J. P. Chippaux. "Evaluation de la prise en charge des envenimations au Sénégal : étude clinique de l’Inoserp® Panafricain." Toxicologie Analytique et Clinique 30, no. 3 (2018): 165–66. http://dx.doi.org/10.1016/j.toxac.2018.07.095.

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15

Madore, Frédérick. "‘Good Muslim, bad Muslim’ in Togo: religious minority identity construction amid a sociopolitical crisis (2017–2018)." Journal of Modern African Studies 59, no. 2 (2021): 197–217. http://dx.doi.org/10.1017/s0022278x21000094.

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AbstractIn Togo, the opposition movement behind the anti-government protests that broke out in 2017–2018 appears to reflect a greater role for Islam in politics. Tikpi Atchadam, leader of the Parti National Panafricain, was the preeminent figure in the movement, having built a solid grassroots base among his fellow Muslims. This article examines the unique role that Muslim leaders played in these protests, as well as the Faure Gnassingbé regime's strategic response. The ruling party made spurious claims against Muslim opponents, associating them with a dangerous wave of political Islam. I argue that by portraying Atchadam as the leader of a radical ethnic and religious movement with Islamist goals, Faure Gnassingbé and his supporters sought to weaken this emerging challenger and deter members of the public from backing calls for political change. The strategy also helped garner support from Western countries while simultaneously driving a wedge between Muslim community leaders.

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16

Dupont, P. L., H. Lapierre, M. Gravelle, and J. M. Bertrand. "Caractérisation du magmatisme Protérozoïque supérieur en Afrique de l'ouest et implications géodynamiques : des rifts intracratoniques au Panafricain?" Canadian Journal of Earth Sciences 24, no. 1 (1987): 96–109. http://dx.doi.org/10.1139/e87-008.

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The main petrological, mineralogical, and geochemical features of the metavolcanites belonging to the Late Proterozoic tectono-sedimentary units of southern Mauritanides (Termessé and Niokolo Koba – Koulountou) and western Hoggar, Algeria (Timesselarsine), permit a reconstruction of the geodynamic environment that controlled the evolution of the Pan-African ranges of western Africa. Flows and pyroclastic beds metamorphosed under greenschist-facies conditions are interbedded within detritic and carbonate platform sediments, suggesting an unstable environment in the vicinity of a continental margin.The association of oceanic tholeiites slightly enriched in LREE and basalts more enriched in TiO2, Zr, Nb, and LREE displaying alkalic affinities suggests intracontinental rifting succeeded by expansion. The lack of ultrabasic – basic complexes (oceanic paleosutures) in southern Mauritanides and their occurrence in the Hoggar suggest that the opening was bigger in the north than in the south.The later calc-alkalic sequences of the Niokolo Koba – Koulountou units are tectonically associated with the Termessé unit. In the Timesselarsine unit, calc-alkalic acid rocks coexist with the basic lavas previously mentioned. Thus, the closure of the rift related to a continental collision appears to be later in southern Mauritanides than in the Hoggar.

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17

Chachoua, Kamel. "2e Festival culturel panafricain d’Alger (1- 4 juillet 2009) Colloque international sur l’anthropologie africainePour une Anthropologie Sud/Sud ?" Journal des anthropologues, no. 118-119 (December 1, 2009): 375–80. http://dx.doi.org/10.4000/jda.4152.

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18

Elmadmad, Khadija. "LE DEUXIÈME CONCOURS PANAFRICAIN DE PROCÈS FICTIF DES DROITS DE L'HOMME (OUJDA, MAROC, 28 SEPTEMBRE ― 2 OCTOBRE 1996)." African Yearbook of International Law Online / Annuaire Africain de droit international Online 6, no. 1 (1998): 277–82. http://dx.doi.org/10.1163/221161798x00111.

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19

Beschea-Fache, Caroline. "Le Fespaco, une affaire d’État(s): festival panafricain de cinéma et de télévision de Ouagadougou, 1969-2009 par Colin Dupré." French Review 88, no. 2 (2014): 204–5. http://dx.doi.org/10.1353/tfr.2014.0016.

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20

Nickson, Patricia J. "L'Institut Panafricain de Santé Communautaire: A New Initiative in the Training of Health Professionals in Community Health in French Speaking Africa." Tropical Doctor 23, no. 2 (1993): 88–89. http://dx.doi.org/10.1177/004947559302300218.

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21

Chippaux, J. P., M. C. Baldé, É. Sessinou, M. Yéro Boiro, and A. Massougbodji. "Evaluation of a new polyvalent antivenom against snakebite envenomation (Inoserp® Panafricain) in two different epidemiological settings: Northern Benin and Maritime Guinea." Médecine et Santé Tropicales 25, no. 1 (2015): 56–64. http://dx.doi.org/10.1684/mst.2014.0413.

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22

Affaton, Pascal, Patrick Gaviglio, and André Pharisat. "Réactivation du craton ouest-africain au Panafricain : paléocontraintes déduites de la fracturation des grès néoprotérozoïques de Karey Gorou (Niger, Afrique de l’Ouest)." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 331, no. 9 (2000): 609–14. http://dx.doi.org/10.1016/s1251-8050(00)01445-2.

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23

Cherkaoui, Adil, and Ahmed Belgaid. "Les nouveaux défis des managers de proximité face à la décentralisation de la fonction RH au Maroc – Cas d’un groupe financier panafricain." Question(s) de management 32, no. 2 (2021): 43–68. http://dx.doi.org/10.3917/qdm.212.0043.

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24

Aitel, Fazia. "KHELLAS (Mériem), Le Premier Festival culturel panafricain. Alger 1969 : une grande messe populaire. Paris : L’Harmattan, 2014, 82 p. – ISBN 978-2-343-04344-9." Études littéraires africaines, no. 39 (2015): 206. http://dx.doi.org/10.7202/1033156ar.

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25

Ouazzani, Hassane, Andre Pouclet, Lakhlifi Badra, and Andre Prost. "Le volcanisme d'arc du massif ancien de l'ouest du Haut-Atlas occidental (Maroc), un temoin de la convergence de la branche occidentale de l'ocean panafricain." Bulletin de la Société Géologique de France 172, no. 5 (2001): 587–602. http://dx.doi.org/10.2113/172.5.587.

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26

Soulaimani, Abderrahmane, Mohamed Bouabdelli, and Alain Piqué. "The Upper Neoproterozoic-Lower Cambrian continental extension in the Anti-Atlas (Morocco)." Bulletin de la Société Géologique de France 174, no. 1 (2003): 83–92. http://dx.doi.org/10.2113/174.1.83.

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Abstract Introduction. – In the Anti-Atlas, south of Morocco (fig. 1), the Precambrian terrains are usually divided into several “series” (fig. 2) : the Paleoproterozoic (PI) is an old crystalline basement, at least Eburnean ; the Neoproterozoic (PII) is constituted by metasedimentary rocks, quartzites and limestones, indicative of a shelf, in which volcano-sedimentary and volcanic flows are intercalated, laterally grading to an ophiolitic complex along the Sirwa-Bou Azzer axis. These PII rocks have been deformed in the course of the Panafrican orogeny ; above the underlying upper Proterozoic terrains and in major unconformity on the Panafrican structures, the Saghro group (PII3) and Ouarzazate group (PIII) series are volcanic and volcano-clastic sequences, often considered as late-Panafrican molasses. Above them, the Tata group (Adoudounian), constituted by marine carbonates and siltstones, represents the earliest Cambrian. Recent structural and sedimentological observations Recent observations have been realized through all the Anti-Atlas, of which the present note gives only examples that are the most significant and easily accessible. They show that the PII3 conglomerates were not everywhere deposited around Panafrican paleoreliefs ; they often contain large bodies of quartzites embedded within the conglomerates (fig. 3). Clearly, the PII3 is an olistostrome at the base of the PIII détrital and volcanic series, which were deposited at the base of active faults. The development of these reliefs took place several tens of millions of years after the end of the Panafrican paroxysm and therefore the PII3 and the PIII are post-Panafrican deposits, unrelated to the Panafrican orogeny. Study of synsedimentary structures (folds, faults, progressive unconformities : fig. 4 to 7) reveals the extensive character of this faulting event that extends even in basal Cambrian. Between the PII3 series and PIII an angular unconformity due to tilting can exist, but we did not find there plicative structures clearly related to the compressive late-Panafrican « B2 » phase sometimes described in the litterature. In the western Anti-Atlas, the extension is pure, with a NW-SE direction ; it is N-S in the central Anti-Atlas and it is transtensive according to N070°E faults, en échelon between sinistral N110°E trending faults in the central-eastern Anti-Atlas. In the detail, nevertheless, the synsedimentary structures suggest slidings from raised zones that correspond to the future inliers (fig. 7). Magmatic and metallogenic activity This extension accompanies various events : (1) a marine transgression, from west to east ; (2) the emplacement of extrusive magmas, first calco-alkaline then tholeiitic ; (3) an hydrothermal activity responsible for the concentration of Co, Au, Cu, etc. These concentrations were in the past attributed to various episodes, from the pre-Panafrican extension to the Hercynian compression. In fact, they result from the circulation of hydrothermal solutions that deposited, in the superficial levels of the crust, products extracted from the PIII magmas or the PII Proterozoic serpentines. The circulations took place in the old compressive structures (e.g. the Panafrican foliation) reopened during the extensive episode described above. Discussion and conclusion : the late Proterozoic-early Cambrian rifting The crustal extension that affected the Anti-Atlas started during the late Proterozoic, after the end of the main Panafrican deformation. Its tectonic significance is discussed with regard to the Panafrican orogeny : either a late Panafrican extension, bracketed between two compressive deformations and possibly related to a thinning of the orogenic crust, or a post-Panafrican extension, unrelated to compressive phases, described as a synrift event. In the Anti-Atlas, it developed through late Proterozoic and early Cambrian times. It aborted at the end of the early Cambrian. Evidences of a comparable extension are found in northern Morocco, western Europe and as far in the Middle East, i.e. all along the northern margin of the paleo-Gondwana.

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Blum, Françoise. "Syndicalistes croyants et panafricains." Vingtième Siècle. Revue d'histoire 119, no. 3 (2013): 99. http://dx.doi.org/10.3917/ving.119.0099.

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Senut, Brigitte, Martin Pickford, and Dudley Wessels. "Panafrican distribution of Lower Miocene Hominoidea." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 325, no. 9 (1997): 741–46. http://dx.doi.org/10.1016/s1251-8050(97)89119-7.

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Villeneuve, Michel, Hervé Bellon, Abdelkrim El Archi, et al. "Événements panafricains dans l'Adrar Souttouf (Sahara marocain)." Comptes Rendus Geoscience 338, no. 5 (2006): 359–67. http://dx.doi.org/10.1016/j.crte.2006.02.008.

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30

Halen, Pierre. "PETIT (Pierre), Patrice Lumumba. La fabrication d’un héros national et panafricain. Préface de François de Callataÿ. Bruxelles : Académie Royale de Belgique, coll. L’Académie en poche, 2016, 145 p., ill. couleur – ISBN 978-2-8031-0526-7." Études littéraires africaines, no. 41 (2016): 232. http://dx.doi.org/10.7202/1037846ar.

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31

Connah, Graham. "Welcome back: The return of the Panafrican Congress." African Archaeological Review 13, no. 4 (1996): 261–65. http://dx.doi.org/10.1007/bf02126100.

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32

Frioux-Salgas, Sarah. "Voix panafricaines à Paris (1920-1950)." Hommes & migrations, no. 1332 (January 1, 2021): 135–41. http://dx.doi.org/10.4000/hommesmigrations.12273.

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33

HAILU, MEKONNEN. "Panafrican Centre for Emergency Preparedness and Response, Addis Ababa." Disasters 14, no. 2 (1990): 178–79. http://dx.doi.org/10.1111/j.1467-7717.1990.tb01061.x.

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34

Dakhlia, Jamil, and François Robinet. "Jeune Afrique, une expérience panafricaine. Entretien avec Béchir Ben Yahmed." Le Temps des médias 26, no. 1 (2016): 266. http://dx.doi.org/10.3917/tdm.026.0266.

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35

Baumann, A., M. El Chai, and F. Thiedig. "Panafrican granites from deep wells of the Murzuk Basin (Fezzan), western Libya." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1992, no. 1 (1992): 1–14. http://dx.doi.org/10.1127/njgpm/1992/1992/1.

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Lecomte, Claude Edouard Paul. "The Africa initiative and the Panafrican Conferences on Crystallography PCCr." Acta Crystallographica Section A Foundations and Advances 73, a2 (2017): C1394. http://dx.doi.org/10.1107/s2053273317081827.

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Baldy-Moulinier, Michel. "Compte rendu du 18e congrès de l'Association panafricaine des sciences neurologiques." Epilepsies 21, no. 1 (2009): 100. http://dx.doi.org/10.1684/epi.2009.0213.

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CHENEAU, Y. "Evolution de la peste bovine et stratégie de la campagne panafricaine." Revue Scientifique et Technique de l'OIE 4, no. 2 (1985): 403–25. http://dx.doi.org/10.20506/rst.4.2.196.

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39

Lara, Oruno D. "La Conférence Panafricaine de Londres. Un centenaire à commémorer, 1900-2000." Présence Africaine 163-164, no. 1 (2001): 103. http://dx.doi.org/10.3917/presa.163.0103.

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40

Honoré, Emmanuelle. "15e congrès de l’Association panafricaine d’archéologie, de préhistoire et disciplines associées." Afrique : Archeologie et Arts, no. 14 (December 15, 2018): 113–14. http://dx.doi.org/10.4000/aaa.1863.

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41

Ngangnou, A., and N. Zoyem. "Evaluation de la protection vaccinale contre la peste bovine au Cameroun. I. La province de l'Adamaoua." Revue d’élevage et de médecine vétérinaire des pays tropicaux 47, no. 1 (1994): 35–37. http://dx.doi.org/10.19182/remvt.9129.

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Dans le cadre de la campagne panafricaine de lutte contre la peste bovine, une enquête sérologique portant sur 5720 sérums a été menée dans la province de l'Adamaoua au Cameroun. La couverture immunitaire générale varie de 60 à 73 % dans les quatre départements visités. Il est conseillé de vacciner les animaux dès l'âge de 6 mois, de renouveler le matériel de vaccination, de remettre en état les parcs de contention et d'utiliser le sulfate de magnésium ou, à la rigueur, le sérum physiologique pour la reconstitution du vaccin lyophilisé.

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42

Nédélec, Anne, Jean-Louis Paquette, Jean-Luc Bouchez, Philippe Olivier, and Bruno Ralison. "Stratoid granites of Madagascar: structure and position in the Panafrican orogeny." Geodinamica Acta 7, no. 1 (1994): 48–56. http://dx.doi.org/10.1080/09853111.1994.11105258.

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43

Tairou, Mahaman Sani, Pascal Affaton, Jean-Pierre Gélard, Ramdane Aïté, and Bawoubadi Edèm Sabi. "Panafrican brittle deformation and palaeostress superposition in northern Togo (West Africa)." Comptes Rendus Geoscience 339, no. 13 (2007): 849–57. http://dx.doi.org/10.1016/j.crte.2007.08.001.

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44

Chorowicz, J., A. Emran, and E. M. Alem. "Tectonique et venues volcaniques en contexte de collision, exemple du massif néogène du Siroua (Atlas Marocain) : effets combinés d'une transformante et de la suture panafricaine." Canadian Journal of Earth Sciences 38, no. 3 (2001): 411–25. http://dx.doi.org/10.1139/e00-074.

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The Late Miocene Early Pliocene Siroua strato-volcano is made of particular hyperalkaline rocks. It lies between the High-Atlas and the Anti-Atlas, in a collisional zone related to the continental subduction of the African plate under the Moroccan Meseta. Our field observations and analyses of SPOT, Landsat-MSS, and DEM (digital elevation model) imagery have permitted mapping of faults, joints, and volcanic edifices. The elongate shape of volcanoes and linear clusters of adjacent edifices, together with their relationships with faults, show that magma ascent was favored by tectonic crustal scale open fractures, essentially tension fractures, tail-cracks, and open faults. These fractures, together with other nonvolcanic, narrow, NNE-striking troughs, provide valuable information on the regional deformation since the Late Miocene. The shorteningextension type strain, which is responsible for the open fractures, is situated near the Azdem transform, a zone of active faults striking NNE, parallel to the convergence trend. The transform links two segments of the "Accident Sud-Atlasique," which constitute the border between the Moroccan Meseta and the African plate. The magma seems to originate from the lithospheric mantle, but asthenospheric material had previously migrated upward along the Panafrican suture zone. This mixed magma finally was transferred to the surface as a result of the onset of the open fractures prior to fault motions. The Siroua volcanic activity results from the conjunction of (1) a Panafrican suture zone and (2) a zone of open fractures due to "strike-slip" strain near a local transform inside the area of collision.

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Delvoye, Adrien, Emmanuelle Honoré, and Chloé Capel. "14e Congrès de l’Association Archéologique Panafricaine de Préhistoire et Disciplines Associées (PANAF)." Afrique : Archeologie et Arts, no. 10 (January 1, 2014): 77–79. http://dx.doi.org/10.4000/aaa.249.

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Diop, Carmen. "Médias panafricains francophones et reproduction des rapports de pouvoir - Années 1980/1990." e-Migrinter, no. 10 (April 11, 2013): 61–78. http://dx.doi.org/10.4000/e-migrinter.481.

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Ouguergouz, Fatsah. "L’ORGANISATION PANAFRICAINE ET LA QUESTION DES DROITS DE L’HOMME : UN REGARD RETROSPECTIF." African Yearbook of International Law Online / Annuaire Africain de droit international Online 20, no. 1 (2014): 23–36. http://dx.doi.org/10.1163/22116176-90000130.

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Fabre, Jean, Ali Ait Kaci, Tayeb Bouima, and Alexis Moussine-Pouchkine. "Le cycle molassique dans le Rameau trans-saharien de la chaîne panafricaine." Journal of African Earth Sciences (and the Middle East) 7, no. 1 (1988): 41–55. http://dx.doi.org/10.1016/0899-5362(88)90052-8.

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Veall, Margaret-Ashley. "African archaeology without frontiers: papers from the 2014 PanAfrican Archaeological Association Congress." Azania: Archaeological Research in Africa 53, no. 1 (2018): 122–23. http://dx.doi.org/10.1080/0067270x.2018.1433595.

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MOURA, CANDIDO A. V., and HENRI E. GAUDETTE. "Evidence of brasiliano/panafrican deformation in the Araguaia belt: implication for Gondwana evolution." Revista Brasileira de Geociências 23, no. 2 (1993): 117–23. http://dx.doi.org/10.25249/0375-7536.1993232117123.

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