Conselho Nacional de Pesquisa e Desenvolvimento Científico e Tecnológico - CNPq / The Propriá, Amparo do São Francisco and Fazenda Alvorada stocks are intrusive in the eastern part of the Macururé Domain and cut the regional orientation. These stocks present similar geological and petrographic features and are essentially constituted by quartz monzonites and porphyritic granites. In these plutons biotite is the predominant mafic mineral and hornblende occurs in some enclaves. Plagioclase crystals exhibit path zoning indicating important instabilities during crystallization. The accessory minerals in these rocks are apatite, zircon, titanite, opaque minerals. In the Propriá and Amparo do São Francisco the stocks the microgranular mafic enclaves are abundant. The crystallization age of the Propriá stock is 615 ± 6 Ma (U-PbSHRIMP). The geochemical data indicate that these stocks correspond to magmatism potassium, orogenic and arc signature and positioned in a post-collision set. / Os stocks Propriá, Amparo do São Francisco e Fazenda Alvorada são intrusivos na parte leste do Domínio Macururé e truncam as orientações regionais. Estes corpos apresentam feições geológicas e petrográficas semelhantes e são essencialmente constituídos por quartzo monzonitos e granitos porfiríticos. Nestes plutons a biotita é o mineral máfico predominante e a hornblenda ocorre em alguns enclaves. Os cristais de plagioclásio exibem forte zoneamento indicando instabilidades importantes durante a cristalização. Os minerais acessórios nestas rochas são apatita, zircão, titanita, minerais opacos. Nos stocks de Propriá e Amparo do São Francisco enclaves máficos microgranulares são abundantes. A idade de cristalização do Stock Propriá é de 615 ± 6 Ma (U-PbSHRIMP). Os dados geoquímicos indicam que estes stocks correspondem a magmatismo potássico, orogênico e com assinatura de arco e posicionados em período pós-colisional. / São Cristóvão, SE

Submitted by Fabio Sobreira Campos da Costa (fabio.sobreira@ufpe.br) on 2016-08-12T12:30:57Z No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Tese de Doutorado Josemar Guerra.pdf: 4223686 bytes, checksum: 5ef7d536e636cc8daf52f5ee42c401f1 (MD5) / Made available in DSpace on 2016-08-12T12:30:58Z (GMT). No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Tese de Doutorado Josemar Guerra.pdf: 4223686 bytes, checksum: 5ef7d536e636cc8daf52f5ee42c401f1 (MD5) Previous issue date: 2015-10-15 / FINEP / ANP / PRH28 / Os derivados de petróleo são largamente empregados na geração de energia em todo o mundo. Por serem constituídos por diversos componentes, seus derivados podem ser empregados como matéria-prima em várias áreas industriais. No processamento do petróleo e no uso de seus derivados identificam-se inúmeras possibilidades de contaminação ao meio ambiente. Os resíduos líquidos gerados nas indústrias petroquímicas possuem diferentes composições químicas que inclui óleos e graxas, benzeno, tolueno e metais pesados, tais como níquel, cádmio, cobre e chumbo. Diante disso, as indústrias buscam, cada vez mais, ajustar os processos existentes através da adoção de procedimentos que visam diminuir a geração de resíduo e uma maior remoção de elementos tóxicos dos efluentes. Assim, este trabalho estudou a utilização de argilas esmectitas in natura e tratadas como adsorventes no processo de adsorção para remoção de poluentes orgânicos e de íons metálicos presentes em efluentes gerados nas indústrias de petroquímicas. A argila esmectita foi empregada no processo de adsorção dos compostos orgânicos benzeno e tolueno e no processo de troca catiônica para a remoção dos íons de metais pesado Cu+2 e Pb+2 como um processo de pós-tratamento para efluentes de refinaria. A partir do tratamento químico da argila esmectita policatiônica (argila chocolate) in natura com carbonato de sódio foi alcançada uma boa troca de íons de cálcio e magnésio por íons de sódio. Com o tratamento observou-se um aumento do número de íons trocáveis de 81,34 meq/100g para 89,39 meq/100g. Pode-se considerar que as argilas apresentam uma estrutura em que os poros são classificados como mesoporosos. Os experimentos de adsorção e de troca catiônica foram realizados em batelada empregando as argilas sódicas como adsorventes no estudo cinético e de equilíbrio. Os resultados obtidos a partir do modelo de equilíbrio de Langmuir-Freundlich indicaram que a argila sódica apresentou capacidade adsortiva perante o benzeno e o tolueno de 7,28mg/g e 7,39mg/g, respectivamente. Para os íons Cu+2 e Pb+2 foi aplicado o modelo de troca Catiônica o qual indicou uma capacidade de 0,99mg/g e 1,10mg/g para os íons Cu+2 e Pb+2, respectivamente. Além disso, o comportamento das análises cinética mostrou que as constantes cinéticas obtidas para o benzeno e tolueno apresentaram os valores de 0,0016 L/mg.min e 0,019 L/mg.min, respectivamente. Para os íons Cu+2 e Pb+2 em argila sódica as constantes cinéticas foram de 0,049 L/mg.min e 0,063 L/mg.min, respectivamente. / The oil derivatives are widely used in power generation throughout the world. For be constituted of several components, their derivatives can be used as raw materials in various industrial areas. In the oil processing and in the use of their derivatives are identified numerous possibilities for contamination to the environment. Liquid wastes generated in the petrochemical industries have different chemical compositions that include oils and greases, benzene, toluene, and heavy metals such as nickel, cadmium, copper and lead. Before that, the industries has been seeking, increasingly, adjust the existing processes by adopting procedures to reduce the generation of waste and to reach a greater removal of toxic elements effluent. This work has studied the use of smectite clays in natura and treated as adsorbents in the adsorption process for removing organic pollutants and metal ions present in wastewater generated in the petrochemical industries. The smectite clay was used in the adsorption of organic compounds benzene and toluene and the cation exchange process for the removal of heavy metal ions Cu+2 and Pb+2 as a post-treatment process for refinery effluents. From the chemical treatment of chocolate clay in natura with sodium carbonate has been achieved a good exchange of calcium and magnesium ions for sodium ions. With treatment there was an increase in the number of exchangeable ions of 81.34 meq/100g to 89.39 meq/100g. It can be considered that the clays have a structure in which the pores are classified as mesoporous. The adsorption and cation exchange experiments were conducted in batch mode using the sodium clays as adsorbents in the kinetic and equilibrium study. The results obtained from the Langmuir-Freundlich equilibrium model indicated that sodium clay adsorptive capacity presented to the benzene and toluene 7,28mg.g-1 and 7,39mg/g, respectively. For Cu+2 and Pb+2 ions was applied to the ion exchange model which indicated a capacity of 0,99mg.g-1 and 1,10mg.g-1 for Cu+2 and Pb+2 ions, respectively. Moreover, the behavior of the kinetic analysis showed that the kinetic constants obtained for benzene and toluene showed values of 0.0016 L.mg-1.min-1 and 0.019 L.mg-1.min-1 respectively. For Cu+2 and Pb+2 ions in sodium clay the kinetic constants were 0.049 L.mg-1.min-1 and 0.063 L.mg-1.min-1, respectively.

Os depósitos de tipo Cu-Au (Mo) pórfiro de Água Rica e Bajo de la Alumbrera, NW argentino, estão geneticamente associados às atividades do Complexo Vulcânico Farallón Negro, no Mioceno. Estes depósitos de classe mundial estão inseridos no contexto geotectônico dos Andes Centrais, Província Geológica das Serras Pampeanas Ocidentais e são do tipo Cu-Au (Mo) pórfiro, embora o depósito de Água Rica possua uma série de características epitermais e uma fase de enriquecimento supergênico. Estudos isotópicos e geocronologia de alta resolução foram propostos para os dois depósitos, objetivando investigar a fonte da mineralização e a influência crustal em sua gênese, além de idades para os pórfiros de Água Rica. Os isótopos de Pb mostram que as amostras de rocha total de Bajo de la Alumbrera são menos radiogênicas, com valores de razões muito próximos e apresentam-se menos radiogênicas do que as amostras de rocha total de Água Rica. As amostras de rocha total de Água Rica mostram maior dispersão, mas de certo modo alguma relação com o material analisado (pirita, ou rocha total). As amostras de pirita, de ambos os depósitos apresentam valores de razões similares, o que permite agrupá-las. As composições isotópicas de Pb em sulfetos e em rochas hospedeiras para os depósitos de Água Rica e Bajo de la Alumbrera indicaram que, apesar da diferença nas litologias presentes nos dois depósitos, os valores obtidos são próximos e muito homogêneos. As amostras de sulfetos de Bajo de la Alumbrera apresentam razões \'ANTPOT.206 Pb\'/ \'ANTPOT.204 Pb\', \'ANTPOT.207 Pb\'/ \'ANTPOT.204 Pb\' e \'ANTPOT.208 Pb\'/ \'ANTPOT.204 Pb\' muito próximas das razões de rocha total, porém com discreto enriquecimento em Pb radiogênico. As amostras de sulfetos de Água Rica apresentam distribuição pouco mais variável, no entanto, observa-se que as amostras de pirita de diorito e pirita do metarenito encaixante ficam próximas entre si e próximas das razões de pirita de Bajo de la Alumbrera Isto pode ser interpretado como fonte e condições de formação similar para estes sulfetos. Os isótopos de Sr e Nd obtidos e combinados com dados da literatura podem sugerir mais evidências na fonte dos magmas e fluidos para estes depósitos, onde as rochas foram divididas em grupos por afinidades isotópicas. Percebe-se que há rochas de padrão juvenil, incorporadas durante a orogenia Andina, mas também há rochas que indicam a presença de contaminação crustal, não homogênea, com variações nos valores de épsilon Nd(t) positivos e negativos. Idades de U-Pb em zircão SHRIMP-IIe nos pórfiros Trampeadero e Quebrada Seca, do depósito de Água Rica, apresentaram idades de 6,20±0,16 Ma e 5,66±0,22 Ma, respectivamente. Estas idades indicam um intervalo tempo muito curto, de cerca de 0,54 Ma, entre as intrusões que contém as mineralizações de maior teor e sendo as primeiras idades obtidas para as intrusões de Água Rica, por meio de datação por U-Pb SHRIMP em zircão. Estas idades sugerem que as intrusões associadas a mineralizações do depósito Água Rica são as mais jovens das que ocorrem na área do Complexo Farallón Negro. Uma isócrona Re-Os obtida em pirita para o depósito de Água Rica de 6,4±2,8 Ma é condizente com a história evolutiva deste depósito. Esta idade, combinada com a idade U-Pb em zircão condiz com a principal fase magmática ocorrida neste depósito e que é tida como a fase principal da mineralização. Com base nos dados, sugere-se que a gênese do depósito de Água Rica ocorreu concomitantemente aos estágios magmáticos finais de Bajo de la Alumbrera, e que esta marca as idades mais jovens para as rochas do Complexo Vulcânico Farallón Negro. Além disso, a participação crustal foi significativa durante a gênese desses depósitos, com uma componente maior no depósito de Água Rica, devido a maior interação dos fluidos magmáticos e mineralizantes com o embasamento Paleozoico. Com base neste estudo, indicamos que em zonas de subducção com baixo ângulo de mergulho, os depósitos minerais gerados podem apresentar maior interação com fluidos crustais do que aqueles em áreas de com placa de alto ângulo. / The Agua Rica and Bajo de la Alumbrera Cu-Au (Mo) porphyry-type deposits, NW Argentina, are genetically associated with the Farallón Negro Volcanic Complex, Miocene age. These world-class deposits of Bajo de la Alumbrera and Agua Rica, located into the tectonic context of the Central Andes, Geological Province of the Sierras Pampeanas, are Cu-Au (Mo) porphyry-type, although the Agua Rica deposit has a number of epithermal features and a supergene enrichment phase. Isotopic studies and high-resolution geochronology were carried out for the two deposits, aiming to investigate the source of the mineralization and crustal influence in its genesis, and ages for the Agua Rica porphyries. Pb isotopes show that the whole-rock samples from Bajo de la Alumbrera are less radiogenic than those from Agua Rica, with close ratio values. The whole-rock samples from Agua Rica show higher dispersion compared to Bajo de la Alumbrera. The pyrite samples from both deposits present similar ratios, which allows grouping them. The Pb isotopic compositions of sulfides and host rocks for the Agua Rica deposit and Bajo de la Alumbrera indicated that, despite the difference in the lithology present in the two deposits, the values obtained are close and very homogeneous. Sulfide samples from Bajo de la Alumbrera show ratios of \'ANTPOT.206 Pb\'/ \'ANTPOT.204 Pb\', \'ANTPOT.207 Pb\'/ \'ANTPOT.204 Pb\' and \'ANTPOT.208 Pb\'/ \'ANTPOT.204 Pb\' very close to the whole-rock ratios, but with a slight enrichment in radiogenic Pb. Sulfide samples from Agua Rica present variable distribution, however, the pyrite samples from diorite and from metasandstone present ratios close to the pyrite from Bajo de la Alumbrera. This ratios similarity could be interpreted as similar conditions and sources to these sulfides. The Sr and Nd isotopes obtained and combined with literature data may suggest more evidence on the source of magmas and fluids for these deposits. Rocks with juvenile pattern, incorporated during the Andean orogeny, are one group observed, but there are also rocks that indicate the presence of crustal contamination, not homogeneous, with variations in Epsilon Nd(t) positive to negative. U-Pb SHRIMP-IIe zircon ages in the porphyries Trampeadero and Quebrada Seca, from the Agua Rica deposit, presented ages of 6.20 ± 0.16 Ma and 5.66 ± 0.22 Ma, respectively. These ages indicate a short time interval between these intrusions, of about 0.54 Ma, and represent the youngest ages obtained for Agua Rica by U-Pb SHRIMP zircon. A Re-Os isochron obtained in pyrite to the Agua Rica deposit of 6.4 ± 2.8 Ma is consistent with the evolution of this deposit. This age, combined with the U-Pb SHRIMP zircon ages matches the main magmatic phase and shows that the main mineralization phase is coeval to the intrusions. Based on these data, it is suggested that the genesis of the Agua Rica deposit was coeval to the last magmatic stages of Bajo de la Alumbrera, and this marks the youngest ages to the Farallón Negro Volcanic Complex rocks. In addition, the crustal participation was significant in the genesis of these deposits, with a major component in the Agua Rica deposit, because the fluids interaction with the Paleozoic basement. Based on this study, we indicated that in flat-subduction zones, the mineral deposits generated present more significant interaction with the crustal fluids than those normal subduction zones.

A presente dissertação apresenta uma investigação sobre a evolução tectono-metamórfica da Formação São Tomé, uma das unidades metassedimentares pertencente ao Grupo Rio Doce, no Orógeno Araçuaí. Essa unidade, de origem pelítica, ocorre em uma faixa com direção geral aproximadamente N-S, com vergência para NE, contrária ao cráton São Francisco neste setor do orógeno. Possui como litotipo principal quartzo-mica xisto, com proporções variadas de granada, estaurolita, sillimanita e plagioclásio. Duas fases deformacionais estão registradas através de uma foliação continua S1 do tipo clivagem de fratura e uma foliação S2 de clivagem de crenulação. As relações texturais indicam que parte das fases minerais se cristalizaram tanto durante o evento deformacional como em condições ausentes de tensão deviatórica, e registro de condições de pico metamórfico de 6 kbar e 650 °C. Os dados geocronológicos foram obtidos em monazita por meio de datações Th-UPb em microssonda eletrônica. Foram identificadas três populações distintas: (i) A população mais antiga de 641±32 Ma, 614±39 Ma e 607±47 Ma, a qual pode representar grãos detríticos de corpos ígneos, não mais aflorantes, relacionados a um possível estagio pré-colisional ou, tratar-se de monazitas metamórficas formadas em um primeiro evento térmico; (ii) População com idades intermediárias entre 560±32 Ma e 559±29 Ma, compatíveis com as idades do ápice metamórfico regional; (iii) População mais jovem de idades entre 501±28 Ma e 491±34 Ma, condizentes com a formação concomitante à geração dos corpos ígneos tardios. Ainda que não esteja esclarecido se essas idades estão relacionadas a eventos metamórficos distintos ou são reflexo da baixa taxa de resfriamento do orógeno, os três grupos de monazita com idades distintas estão bem estabelecidos. / The present dissertation presents an investigation on the tectono-metamorphic evolution of the São Tomé Formation, one of the metasedimentary units belonging to the Rio Doce Group, in the Araçuaí Orogen. This unit, of pelitic origin, occurs in a band with general direction approximately N-S, with vergence for NE, contrary to the São Francisco craton in this sector of the orogen. It has quartz-mica schist as main lithotype, with varying proportions of grarnet, staurolite, sillimanite and plagioclase. Two deformational phases are recorded through a continuous foliation S1 of the fracture cleavage type and a foliation S2 of crenulation cleavage. The textural relations indicate that part of the mineral phases crystallized both during the deformational event and in conditions absent of deviatore voltage, and record of metamorphic peak conditions of 6 kbar and 650 ° C. The geochronological data were obtained in monazite by means of Th-U-Pb dating in electron microprobe. Three distinct populations were identified: (i) The oldest population of 641 ± 32 Ma, 614 ± 39 Ma and 607 ± 47 Ma, which may represent detrital grains of igneous bodies, no longer outcrops, related to a possible pre- collisional or, being metamorphic monazites formed in a first thermal event; (ii) Populations with intermediate ages between 560 ± 32 Ma and 559 ± 29 Ma, compatible with regional metamorphic apex ages; (iii) Younger population between 501 ± 28 Ma and 491 ± 34 Ma, consistent with the formation concomitant with the generation of late igneous bodies. Although it is unclear whether these ages are related to distinct metamorphic events or are reflective of the low orogenic cooling rate, the three monazite groups of different ages are well established.

Located in the south of the Moroccan Sahara, the Adrar Souttouf Massif is the northern continuation of the Mauritanides at the western margin of the West African Craton. The massif itself exhibits a complex polyphase geologic history and contains four geologically different, SSW-NNE trending main units named from west to east: Oued Togba, Sebkha Gezmayet, Dayet Lawda, Sebkha Matallah. They are thrusted over each other in thin-skinned nappes with local windows of the discordantly overlain Archaean Reguibat basement. The eastern margin of the massif is bordered by the Tiris and Tasiast-Tijirit areas of the Reguibat Shield as well as its (par-) autochthonous Palaeozoic cover sequence, termed Dhloat Ensour unit. More than 5.500 U-Th-Pb age determinations and over 1.000 Hf isotopic measurements on single zircon grains from igneous, metamorphic, and sedimentary rocks of all the massifs units and its vicinity have yet been obtained. Most of the zircons were studied with respect to their morphological features. This method improves the accuracy of provenance studies by detecting varying zircon morphologies in space and time. These data are accompanied by U-Th-Pb age determinations on apatite as well as rutile. Together, they allow proposing a model of the geologic evolution of this poorly mapped area for the last 635 Ma. A combination of the obtained data with extensive zircon age databases of the surrounding cratons and terranes facilitates continental-scaled palaeogeographic reconstructions. Regarding the geologic evolution of the Adrar Souttouf Massif, the assembly of the first units began prior to 635 Ma. Although containing all the major zircon age and Hf-isotope populations of the West African Craton as well as some Mesoproterozoic grains, the Sebkha Gezmayet unit lies to the west of the Dayet Lawda unit of oceanic island arc composition. Hence, the Sebkha Gezmayet unit must have been rifted away from the craton prior to the formation of the oceanic unit within the West African Neoproterozoic Ocean at about 635 Ma. Recently published Hf and zircon age data of this unit suggest that the island arc was derived from a juvenile mantle source. Subsequently, the accretion of precursors of the Oued Togba and Sebkha Gezmayet units as well as a partial obduction of the oceanic Dayet Lawda unit and the Neoproterozoic sediments of a foreland basin (Sebkha Matallah unit) onto the Reguibat Shield took place. Peak metamorphism in the obducted oceanic rocks was reached at about 605 Ma. Magmatism in the western units between 610 and 570 Ma suggests on-going tectonic activity. The Early and Middle Cambrian is characterised by the erosion of the Ediacaran orogen and deposition of thick sedimentary sequences at the Sebkha Matallah unit, which acted as foreland basin. These sediments show a mostly West African zircon record with only some Mesoproterozoic grains provided by the westernmost parts of the massif. Initial rifting of the Oued Togba and Sebkha Gezmayet units from the remaining areas presumably occurred during the Late Cambrian. Coeval granitoid intrusions occurred on both sides of the rift. The two rifted units were likely involved to the polyphased Appalachian orogenies, which is emphasised by Devonian magmatism. Thus, and with respect to the isotopic data, the Oued Togba unit is interpreted to be of Avalonia affinity, while the Sebkha Gezmayet unit can likely be linked to Meguma. The units which remained at the West African Craton underwent intense sediment recycling during the entire Ordovician to Devonian times. Final accretion of all units and formation of the current massif was achieved during the Variscan-Alleghanian orogeny. This was accompanied by magmatism in the Sebkha Gezmayet unit and intense metamorphism of the Reguibat basement, whose zircons often show lower discordia intercepts of Carboniferous or Permian age. The post-Variscan period is characterised by erosion of the orogen and subjacent alternating cycles of sedimentation and deflation. The Adrar Souttouf Massifs importance for palaeogeographic reconstructions is given by the striking differences in the zircon age and Hf-isotope record of its westernmost Oued Togba unit and the remaining area. The results obtained from the Oued Togba unit resemble the published data of the Avalonia type terranes including prominent Mesoproterozoic, Ediacaran-Early Cambrian, as well as Early Devonian age populations. Many Mesoproterozoic zircons, which are exotic for the West African Craton prior to 635 Ma, form a ca. 1.20 to 1.25 Ga age peak that is an excellent tracer for detrital provenance studies and source craton identification of the sedimentary rocks. This is also valid for some sedimentary samples that do not show ages younger than 700 Ma, but large quantities of Mesoproterozoic zircon. These rocks can be correlated to similar sediments in Mauritania and W-Avalonia and are thought to be of pre-pan-African", i.e. pre-Ediacaran or even pre-Cryogenian age. They may give direct insights to the source area in Early to Mid Neoproterozoic times. Accordingly, comparison with published data of Amazonia and Baltica, allows setting up new hypotheses for the pre-Ediacaran history of the Avalonian type terranes. Lacking of magmatism in Amazonia between ca. 1200 and ca. 1300 Ma favours Baltica as source craton for the Avalonian terranes and requires a new point of view for the Neoproterozoic palaeogeography.

No description available.

No description available.

Located in the south of the Moroccan Sahara, the Adrar Souttouf Massif is the northern continuation of the Mauritanides at the western margin of the West African Craton. The massif itself exhibits a complex polyphase geologic history and contains four geologically different, SSW-NNE trending main units named from west to east: Oued Togba, Sebkha Gezmayet, Dayet Lawda, Sebkha Matallah. They are thrusted over each other in thin-skinned nappes with local windows of the discordantly overlain Archaean Reguibat basement. The eastern margin of the massif is bordered by the Tiris and Tasiast-Tijirit areas of the Reguibat Shield as well as its (par-) autochthonous Palaeozoic cover sequence, termed Dhloat Ensour unit. More than 5.500 U-Th-Pb age determinations and over 1.000 Hf isotopic measurements on single zircon grains from igneous, metamorphic, and sedimentary rocks of all the massifs units and its vicinity have yet been obtained. Most of the zircons were studied with respect to their morphological features. This method improves the accuracy of provenance studies by detecting varying zircon morphologies in space and time. These data are accompanied by U-Th-Pb age determinations on apatite as well as rutile. Together, they allow proposing a model of the geologic evolution of this poorly mapped area for the last 635 Ma. A combination of the obtained data with extensive zircon age databases of the surrounding cratons and terranes facilitates continental-scaled palaeogeographic reconstructions. Regarding the geologic evolution of the Adrar Souttouf Massif, the assembly of the first units began prior to 635 Ma. Although containing all the major zircon age and Hf-isotope populations of the West African Craton as well as some Mesoproterozoic grains, the Sebkha Gezmayet unit lies to the west of the Dayet Lawda unit of oceanic island arc composition. Hence, the Sebkha Gezmayet unit must have been rifted away from the craton prior to the formation of the oceanic unit within the West African Neoproterozoic Ocean at about 635 Ma. Recently published Hf and zircon age data of this unit suggest that the island arc was derived from a juvenile mantle source. Subsequently, the accretion of precursors of the Oued Togba and Sebkha Gezmayet units as well as a partial obduction of the oceanic Dayet Lawda unit and the Neoproterozoic sediments of a foreland basin (Sebkha Matallah unit) onto the Reguibat Shield took place. Peak metamorphism in the obducted oceanic rocks was reached at about 605 Ma. Magmatism in the western units between 610 and 570 Ma suggests on-going tectonic activity. The Early and Middle Cambrian is characterised by the erosion of the Ediacaran orogen and deposition of thick sedimentary sequences at the Sebkha Matallah unit, which acted as foreland basin. These sediments show a mostly West African zircon record with only some Mesoproterozoic grains provided by the westernmost parts of the massif. Initial rifting of the Oued Togba and Sebkha Gezmayet units from the remaining areas presumably occurred during the Late Cambrian. Coeval granitoid intrusions occurred on both sides of the rift. The two rifted units were likely involved to the polyphased Appalachian orogenies, which is emphasised by Devonian magmatism. Thus, and with respect to the isotopic data, the Oued Togba unit is interpreted to be of Avalonia affinity, while the Sebkha Gezmayet unit can likely be linked to Meguma. The units which remained at the West African Craton underwent intense sediment recycling during the entire Ordovician to Devonian times. Final accretion of all units and formation of the current massif was achieved during the Variscan-Alleghanian orogeny. This was accompanied by magmatism in the Sebkha Gezmayet unit and intense metamorphism of the Reguibat basement, whose zircons often show lower discordia intercepts of Carboniferous or Permian age. The post-Variscan period is characterised by erosion of the orogen and subjacent alternating cycles of sedimentation and deflation. The Adrar Souttouf Massifs importance for palaeogeographic reconstructions is given by the striking differences in the zircon age and Hf-isotope record of its westernmost Oued Togba unit and the remaining area. The results obtained from the Oued Togba unit resemble the published data of the Avalonia type terranes including prominent Mesoproterozoic, Ediacaran-Early Cambrian, as well as Early Devonian age populations. Many Mesoproterozoic zircons, which are exotic for the West African Craton prior to 635 Ma, form a ca. 1.20 to 1.25 Ga age peak that is an excellent tracer for detrital provenance studies and source craton identification of the sedimentary rocks. This is also valid for some sedimentary samples that do not show ages younger than 700 Ma, but large quantities of Mesoproterozoic zircon. These rocks can be correlated to similar sediments in Mauritania and W-Avalonia and are thought to be of pre-pan-African", i.e. pre-Ediacaran or even pre-Cryogenian age. They may give direct insights to the source area in Early to Mid Neoproterozoic times. Accordingly, comparison with published data of Amazonia and Baltica, allows setting up new hypotheses for the pre-Ediacaran history of the Avalonian type terranes. Lacking of magmatism in Amazonia between ca. 1200 and ca. 1300 Ma favours Baltica as source craton for the Avalonian terranes and requires a new point of view for the Neoproterozoic palaeogeography.

Cette enquête épidémiologique porte sur l'impact sanitaire de la décharge de Mbeubeuss, réceptacle de l'ensemble des déchets ménagers et industriels de Dakar (Sénégal), sur la population résidant à proximité. Les déchets, stockés sans être recouverts, sont source de pollution atmosphérique et des sols, notamment par le plomb et le cadmium. Les répercussions sanitaires sont d'autant plus préoccupantes que de nombreux riverains de cette décharge sont directement ou indirectement exposés. L'objectif de cette étude était de déterminer, après caractérisation chimique des échantillons de sol et de particules atmosphériques, l'imprégnation de la population (enfants et adultes) à ces deux métaux et de rechercher leur éventuel impact sur la fonction rénale. Nos résultats ont mis en évidence des teneurs atmosphériques et telluriques en plomb et en cadmium plus élevées sur le site de la décharge (teneurs 20 à 80 fois plus élevées que celles de la zone témoin). L'imprégnation saturnine, déterminée au travers des plombémies, plomburies et des marqueurs biologiques d'effet (PPZ, AlaU), de même que les teneurs sanguines et urinaires en cadmium étaient significativement plus importantes chez les individus résidant au voisinage de la décharge. La production excessive d'espèces réactives de l'oxygène induite par cette imprégnation s'est traduit par une diminution du système de défenses antioxydantes (SOD, GPx, Sélénium, GSH) et une peroxydation lipidique (MDA) accrue chez les sujets exposés. En outre, les variations de certains des marqueurs sensibles et spécifiques de néphrotoxicité (concentrations urinaires élevées en protéines totales, en RBP et en CC16 ; et augmentation des activités GSTα et LDH) suggèrent l'apparition de signes discrets et précoces d'altération de la fonction rénale chez les individus résidant à proximité de la décharge. L'exposition aux émissions de la décharge de Mbeubeuss constitue donc une véritable source de risques pour l'environnement et la santé des populations environnantes. Cette étude pourrait sans doute contribuer à conscientiser les acteurs de la santé sur les risques liés à cette décharge et à placer ces problèmes environnementaux, qui constituent un nouveau défi pour les pays pauvres, au cœur des futurs programmes de développement. / This case-control study dealt with adverse health effects on the population living near Mbeubeuss landfill in Dakar (Senegal). All household and industrial waste arising from Dakar are stored in this open landfill without being covered and are therefore possible sources of air pollution and soil contamination by heavy metals, especially Pb and Cd. Health impacts are of particular concern since many of the neighboring residents of this discharge are directly or indirectly exposed. The objective of this study was to determine Pb and Cd concentrations in both environment and humans, and to evaluate possible renal function alteration within the adult and child populations. Our results showed that lead and cadmium concentrations of soils and atmosphere were higher in the landfill (20 to 80 times) than those of the control area. The lead impregnation, evaluated through the blood and urine lead levals, and the biomarkers of exposure (PPZ, ALAU) as well as blood and urine cadmiums levels, were significantly higher in the subjects neighboring the landfill. Excessive production of reactive oxygen species induced by the metal impregnation conducted in exposed subjects to a decrease in antioxidant defense system (SOD, GPx, Selenium, GSH) and an increase in lipid peroxidation (MDA). Moreover, changes in several sensitive and specific markers of nephrotoxicity (high urinary concentrations of total protein, RBP and CC16, as well as GSTα and increased activities) suggested the occurence of discrete and early signs of impaired renal function for the landfill neighboring population. Exposure to emissions from the Mbeubeuss landfill is therefore a source of risk for the environment and the health of people who live and/or work within it. This study could undoubtedly help to raise awareness of landfill-related health risks amoung stakeholders, and to place these environmental problems, wich constitute a new challenge for poor countries, at the heart of future development programs.

Världen står inför ett stort vattenförsörjningsproblem som måste lösas – så många som 884 miljoner människor använder idag potentiellt förorenade vattenkällor till sitt dricksvatten. Denna rapport fokuserar på ett av de drabbade länderna som är Uganda. Syftet med projektet är att undersöka vilket/vilka av de fem olika ugandiska växterna; Erythrina abyssinica, Musa spp, Cyperus papyrus, Imperata cylindrica och Coffea canephora som är mest lämplig för rening av kadmium- och blykontaminerat grundvatten. Katjonbyteskapaciteten bestäms genom laboration. Analyser kring växtmaterialen görs med hjälp av litteraturstudier och intervjuer med en doktorand från Uganda. M. spp visar sig ha klart högst katjonbyteskapacitet och finns även i form av mycket avfall, därför anses denna vara det mest lämpliga materialet för rening. Lösningen skulle kunna implementeras i samhället med ett filter gjort av växtmaterial, om vidare forskning görs. / The world is facing a major water supply problem to solve, as many as 884 million people currently use potentially polluted water sources for their drinking water. This report focuses on one of the affected countries, which is Uganda. The project aims to examine which of the five different Ugandan plants; Erythrina abyssinica, Musa spp, Cyperus papyrus, Imperata cylindrica and Coffea canephora that is the most suitable for purification of cadmium- and lead contaminated groundwater. The cation exchange capacity is determined by laboratory experiment. Literature studies and interviews with a Ugandan postgraduate student are used for the analysis of the plant materials. M. spp has the highest cation exchange capacity and contributes with a lot of waste material; therefore it is considered the most suitable material for purification. The solution could be implemented in the community with a filter made of plant material, if further research is done.