Auswahl der wissenschaftlichen Literatur zum Thema „Bougouni (Mali)“
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Zeitschriftenartikel zum Thema "Bougouni (Mali)":
Sogoba, Nafomon, Kyle Rosenke, Jennifer Adjemian, Sory Ibrahim Diawara, Ousmane Maiga, Moussa Keita, Drissa Konaté et al. „Lassa Virus Seroprevalence in Sibirilia Commune, Bougouni District, Southern Mali“. Emerging Infectious Diseases 22, Nr. 4 (April 2016): 657–63. http://dx.doi.org/10.3201/eid2204.151814.
Chappatte, André. „Night life in southern urban Mali: being a Muslimmaquisardin Bougouni“. Journal of the Royal Anthropological Institute 20, Nr. 3 (28.07.2014): 526–44. http://dx.doi.org/10.1111/1467-9655.12121.
Sidibé, Souleymane S., K. W. Coulibaly, Martin Dakouo, Z. Tarnagda, Amadou Sery, Mamadou Niang, K. Traoré, H. Nantoumé, Siaka Diarra und H. Seyni. „Fièvre Q chez les petits ruminants au Mali. Résultats d'une enquête sérologique“. Revue d’élevage et de médecine vétérinaire des pays tropicaux 66, Nr. 1 (01.01.2013): 11. http://dx.doi.org/10.19182/remvt.10144.
VANYUKOVA, Darya. „2022 Expedition to Mali“. Oriental Courier, Nr. 1 (2022): 86. http://dx.doi.org/10.18254/s268684310021414-3.
Sidibe, S., KW Coulibaly, A. Sery, M. Fofana, F. Sidibe und M. Kanoute. „Prévalence de la brucellose, chlamydiose et toxoplasmose chez les petits ruminants au Mali : résultats d'une enquête séro-épidemiologique“. Revue Malienne d'Infectiologie et de Microbiologie 13, Nr. 1 (01.05.2019): 1–9. http://dx.doi.org/10.53597/remim.v13i1.1298.
Keita, Sidiki, Koniba Keita, Mahamadou Coulibaly, Moussa Sissoko, Lamine Soumare, Oumar Sacko, Sekou Koumaré et al. „Peritonitis Management through Appendicular Perforation in the Department of Surgery Bougouni Hospital (Mali)“. Surgical Science 11, Nr. 12 (2020): 446–52. http://dx.doi.org/10.4236/ss.2020.1112046.
Traoré, Siaka Drissa, Moro Souley Sidibé, Kapoury Sanogo, Urbain Dembélé, Djigui Dembélé, M'Piè BENGALI und Kalifa Traoré. „EVALUATION OF THE EFFECTIVENESS OF THE CONTRIBUTION OF AGRICULTURAL LIME AND NATURAL PHOSPHATE OF TILEMSI (PNT) ON THE PRODUCTION OF COTTON AND CORN IN THE PRODUCTION SYSTEM OF FARMS IN THE MALI-SOUTH ZONE“. International Journal of Agriculture, Environment and Bioresearch 08, Nr. 03 (2023): 119–29. http://dx.doi.org/10.35410/ijaeb.2023.5833.
Mariam, D., TCA Bernadin und TM Inoussa. „Inventaire des vergers de mangues dans le cercle de Bougouni au Mali : Approche par Télédétection“. Journal of Applied Biosciences 66 (08.10.2013): 5095. http://dx.doi.org/10.4314/jab.v66i0.95007.
Traoré, N. K. „Etude des facteurs associés à la non compliance au traitement de masse ciblant les Schistosomiases dans le District Sanitaire de Bougouni, Bankass et Tominian“. Mali Santé Publique 10, Nr. 1 (24.07.2020): 71–78. http://dx.doi.org/10.53318/msp.v10i1.1666.
Traore, Kalifa, und Birhanu Zemadim Birhanu. „Soil Erosion Control and Moisture Conservation Using Contour Ridge Tillage in Bougouni and Koutiala, Southern Mali“. Journal of Environmental Protection 10, Nr. 10 (2019): 1333–60. http://dx.doi.org/10.4236/jep.2019.1010079.
Dissertationen zum Thema "Bougouni (Mali)":
Bertrand, Monique. „Question foncière et villes secondaires au Mali : les communes méridionales de Sikasso, Koutiala et Bougouni“. Paris 10, 1990. http://www.theses.fr/1990PA100116.
The investigations deal with the part of secondary towns in the territorial development of a west-African underdeveloped country on the one hand, and with the land question which confronts national institutional logics and local urban practices on the other hand. The first part analyses the deformations of normative domanial regulations : from the state to the southern communes, poor budgetary means are appearing at every levels of production of urban plots. The second part concerns the land markets. The selective offer of urban plots underlines the social stratifications in town. Market and property valorizations of these plots show close relations between speculative rents and patrimonial pressures on the land market. The third part confronts these different ambitions through occupational and migratory ways of town insertion. The family and the duration of residence determine social solvencies which bypass or consolidate economic solvencies. The fourth part considers historical implications of urban conflicts about land. New personal relationships develop between local communes and the state of Mali. The conclusion qualifies sizing effects between towns in the land and property market. Taken in a largest geographical comparison, the links between rents and patrimonies request new investigations about economic, social and political competitions which are spreading in Malian society
Chappatte, Andre. „Walking an earthly path : everyday Islam in Bougouni, a town of southwest Mali“. Thesis, SOAS, University of London, 2013. http://eprints.soas.ac.uk/15627/.
Sanogo, Séko. „Pegmatites lithinifères (Li-Cs-Ta) et roches plutoniques de Bougouni (Sud du Mali, Craton Ouest Africain) : approches pétrographiques, structurales, géochimiques et géochronologiques“. Electronic Thesis or Diss., Université de Lille (2022-....), 2022. https://pepite-depot.univ-lille.fr/ToutIDP/EDSMRE/2022/2022ULILR083.pdf.
The Bougouni region in southern Mali is well known for the ore body lithium-bearing pegmatites and aplites. Lithium is currently a strategic element in view of the growing need for this raw material. The lithiniferous pegmatites are thus among the most sought-after deposits for lithium.The study area, located SE of Bamako (Mali), belongs to the southern part of the West African Craton. The various rocks in this area were formed during the Birimian crustal growth events, during the Eburnean oOrogeny, between ca. 2200 and 1800 Ma. The formations encountered are metavolcano sedimentary and plutonic rocks, mostly granitoid (tonalite to two-mica monzogranite), structured in a NNE-SSW direction by the existence of large shear zones. The dykes are intrusive in these host rocks, which occur in the form of decimeter to decameter thick dykes ranging from aplitic to pegmatitic facies. The emplacement in a brittle domain coupled with the low metamorphic grade of the enclosing metasediments indicate a dyke emplacement in the upper continental crust.The Bougouni province has about 100 Li-rich dykes (Li2O > 1.00 wt% of total rock). Spodumene, the main lithium-bearing mineral phase (Li2O = 8 wt%), represents between 5 and 30 vol.% of the rock, accompanied by alkali feldspar, plagioclase, quartz and a small quantity of muscovite and biotite. In addition to, 100 Li-poor dykes (Li2O < 0.05 wt%) that are characterized by the same mineralogical assemblage as the lithium-rich dykes except for spodumene, which is replaced by garnet.Concerning geochronology, U-Pb ages on zircons for all granitoids (granodioritic to granitic facies with two micas) range between 2100 ± 14 and 2136 ± 19 Ma. These ages are in agreement with the ages of other plutonic formations ranging between 2080 and 2120 Ma on the Birimian scale. The U-Pb ages on magmatic apatites of the dykes are between 2070 - 2000 Ma. Comparison of the geochronological data with other pegmatites of the Birimian allow us to define the period ca. 2070 - 2000 Ma as the period of establishment of the pegmatitic dykes (notably the LCT family pegmatites) of the Birimian. This late- to post-Orogenic period would represent the final stage of paleoproterozoic magmatism in the Boulé-Mossi domain.Concerning major and trace elements geochemistry, the absence of a continuous geochemical evolution from granitoids to dykes does not allow to explain the pegmatitic fluids as the most evolved terms of the granitoids. This conclusion is in agreement with the geochronological data that show a much too large age difference between these formations to be genetically related. Concerning the dykes, although they are contemporaneous, the differences in geochemical signature do not allow to explain that they could have evolved from a single parent melt. However, it is very likely that the melts that gave rise to both types of dykes may have been derived from the melting of the same type of metapelitic protolith.In sum, the field, petrographic, geochronological and geochemical data do not provide a genetic link between the Bougouni dykes and granitoids. The two dyke facies are formed from two distinct melts derived from a single protolith. The difference in mineralogical and geochemical composition, particularly in Li, between the Li-rich and Li-poor dykes could be explained by the role of fluids of sedimentary origin that may have percolated and interacted with the source? host rocks and/or the pegmatitic melts, allowing the enrichment of certain fluids in mobile elements such as lithium
Bücher zum Thema "Bougouni (Mali)":
Togola, Dasse. Les organizations d'auto-promotion féminine et le développement de la filière fonio dans la zone de Bougouni au Mali. Arlington, VA: Winrock International, 2002.
Buchteile zum Thema "Bougouni (Mali)":
„Prologue“. In Knowing by Ear, 1–9. Duke University Press, 2024. http://dx.doi.org/10.1215/9781478059028-001.
Konferenzberichte zum Thema "Bougouni (Mali)":
Pujol, Magali, und Anne Battani. „Natural hydrogen occurrence in Bougou-1 well (Mali): geological accumulation or ongoing generation, insights from stable isotopes and noble gas tracing“. In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11436.
Zhao, Hongwen, Ernest A. Jones, Rajput Seemant Singh, Hasnol Hady B. Ismail und Seng WahTan. „The Hydrogen System in the Subsurface: Implications for Natural Hydrogen Exploration“. In ADIPEC. SPE, 2023. http://dx.doi.org/10.2118/216710-ms.
Fuad, M. I. Ahmad, H. Zhao, M. S. Jaya und E. A. J. Jones. „Rock Physics Modeling of Hydrogen-Bearing Sandstone: Implications for Natural Hydrogen Exploration and Storage“. In SPE Annual Technical Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/214789-ms.