“Germes de grandeza”: Antônio Ladislau Monteiro Baena e a descrição de uma província do Norte durante a formação do Império brasileiro (1823-1850)

O objetivo desta dissertação é analisar o conjunto da obra do português Antônio Ladislau Monteiro Baena, bem como sua atuação militar na província do Pará nas primeiras décadas do século XIX. Através da descrição física e política da província paraense, Antônio Baena forneceu dados estatísticos de uso político para o Império brasileiro. O escritor e militar Baena, a serviço do Império, viveu e escreveu em um momento ímpar para o Brasil e para o antigo Grão-Pará. Sua obra reúne e traduz uma série de dados que ajudarão a compor a tensa ligação entre as províncias do norte com as do sul do Brasil. É a partir de sua obra intitulada Ensaio Corográfico sobre a Província do Pará, publicada em 1839, que o presente estudo envereda pela escrita comprometida do autor e dos seus principais apontamentos sobre a riqueza em potencial da província, embasada na variedade e na virtude de seus produtos naturais. Ademais, a análise atenta para outras produções de Antônio Baena, cujo tema principal era a província do Pará, constantes na Revista do Instituto Histórico e Geográfico Brasileiro e publicadas no cenário imperial. Estas produções acabam por inserir-se nos debates do referido Instituto e no contexto de formação política do Império brasileiro.

Cooperação e conflito entre britânicos e portugueses na Ásia. Dos primeiros contactos em Bombaim (c.1600-1740)

A aquisição da ilha de Bombaim pela coroa inglesa e a consequente convivência fronteiriça com o Estado da Índia constituiu uma novidade relacional e diplomática entre os poderes português e britânico, não só no Índico como em todo o espaço ultramarino. Esta nova situação projectou a recentemente forjada e renovada aliança anglo-portuguesa para um diferente plano, até então não experienciado. De facto, o acordo de 1661 estipulou que o Estado da Índia entregasse parte do seu território a uma coroa europeia, o que significava uma mudança no seu paradigma de actuação e a partilha de fronteiras comuns com um vizinho europeu, “consentido” e aliado. A isto adicionava-se o facto da população residente em Bombaim, constituída por uma forte comunidade de grandes foreiros portugueses e jesuítas, passar a estar sujeita aos dictames da coroa inglesa. Todos estes pressupostos constituíram uma novidade para o Estado da Índia e para os seus súbditos e exigiram, necessariamente, uma adaptação no modo de interacção com tão próximo vizinho. O mesmo se terá passado com os oficiais britânicos, numa primeira fase da coroa (1665-1668) e doravante da East India Company, para quem o domínio territorial no espaço asiático constituía uma experiência nova. Esta realidade tão próxima entre as duas potências europeias originou, necessariamente, a eclosão de problemas e tensões entre as duas estruturas de poder. Será a partir desta conjuntura sugestiva que procuraremos compreender como o entendimento anglo-português na Europa foi transposto e gerido na esfera ultramarina, através da análise do caso paradigmático de Bombaim. A gestão da aliança naquele espaço assumiu contornos específicos e de difícil administração, pois a distância ditava uma maior autonomia decisória das autoridades de Goa e Bombaim, nem sempre em consonância com as directrizes europeias. A interacção na região de Bombaim e espaços adjacentes foi pautada pela flexibilidade e, por isso, caracterizou-se por momentos de antagonismo, cooperação e conflito aberto. Nestes “encontros de (in)conveniência”, ambos os lados procuraram tirar partido das dinâmicas conjunturais da política indiana, o mesmo aplicando-se no sentido inverso, adaptando-se alinhamentos e rupturas consoante os interesses imediatos. Bombaim foi, assim, singular no relacionamento anglo-português na Ásia, o que não implica que não se procure compreender as ressonâncias da interação entre portugueses e britânicos noutros espaços do subcontinente indiano (como Madrasta) ou contrapor os modos de actuação da EIC noutros locais (como Cochim). Na dissertação em curso, propomos efectuar um estudo de longo tempo, que analise de forma sistemática a transversal as dinâmicas relacionais entre britânicos e portugueses desde a introdução britânica na Ásia até à perda portuguesa da Província

Escravidão na Vila do Príncipe, província do Rio Grande do Norte (1850/1888)

This dissertation presents a study on the slave population of Vila do Príncipe, from 1850 to 1888, based on the judicial and notarial collection of hand written documents as well as on the Reports of Presidents of the Province of Rio Grande do Norte. The issue that drives the research relates to the reproduction of slavery in a region of cattle breeding colonization. Therefore, the research aims to understand how in a peripheral socio-economic place (in Vila do Príncipe, cattle breeding Seridó) after the prohibition of the African slave trade, the slave relationships subsisted and structured themselves. In the sense, the research analyzed the dynamics of socio-economic slave units and their relationship with space, ownership structure and the slave family.

Escravos em ação na Comarca do Príncipe - Província do Rio Grande do Norte (1870-1888)

The aim of this research is to study the actions of slaves in Comarca do Príncipe, Rio Grande do Norte (1870/1888). Considering the space as a relevant category in the subservient relationship, we investigate how negotiations about the captivity conditions and freedom took place in the domain of this province. The slaves are considered as subjects, who fought for better living conditions in the captivity and who sometimes practiced criminal offenses to achieve freedom. To analyze their actions in the socio-economic environment of the province, we resort to different types of sources. They are: civil and criminal processes, reports from the president of Rio Grande do Norte, the census of 1872, a newspaper called O Assuente, the Livro do Fundo de Emancipação do Município de Príncipe (1873-1886) (The Emancipation Book of Príncipe city) and Imperial Laws. We used the following steps to analyze the data obtained from these sources: the compilation, reading, paleographic transcription, classification of the data according to the thematic, analysis and comparison of information and statistic quantification, submitting empirical data to the discussion built according to the historiographies debates about this subject

Litogeoquímica E aspectos Petrogenéticos dos basaltos da Província Magmática do Paraná na porção centro-norte do Estado de São Paulo

The petrographic and geochemical characterization of flood basalts of Serra Geral Formation are here presented. The investigated areas are situated in four different regions of São Paulo state: Jaú, Ribeirão Preto, Franca and Fernandópolis. They represent almost the total area of outcrops of basalts in the São Paulo State. The petrographical data reveals that these rocks are constituted mainly by plagioclase (30-40%), pyroxenes, augite and pigeonita (20-30%) and magnetite (5-15%), and show a intergranular texture and its varieties intersertal, hialophitic and pilotaxitic. The geochemical data show a basic and tholeiitic affinity of the studied basalts, with high-Ti content (TiO2 > 1.8%), typical of the northern region of Paraná Basin. Three different magma-types were recognized: Paranapanema, Urubici and Pitanga. The first magma-type is concentrated in the Fernandópolis region, the second in the Franca region, and the Pitanga occurs in the Ribeirão Preto and Jaú regions. The distribution patterns of these magma-types and the detailed study of geochemical data showed that they are, probably, generated by a melting of a continental lithospheric mantle.

Geologia, petrografia e geoquímica das associações TTGs e Leucogranodioritos do extremo norte do Domínio Rio Maria, Província Carajás

O mapeamento geológico realizado à sudeste de Água Azul do Norte/PA, porção norte do Domínio Rio Maria, aliado aos dados petrográficos e geoquímicos permitiram a individualização de associações TTGs e leucogranodioritos. Nesta região, os trabalhos de mapeamento foram realizados apenas em escala regional o que possibilitou a extrapolação da área de ocorrência de rochas similares ao Tonalito Caracol e rondhjemito Mogno. Os TTGs estudados foram individualizados em duas unidades com base no conteúdo de minerais máficos, concentrações de epidoto magmático e no grau de saussuritização (descalcificação) do plagioclásio em: (1) Epidoto-Biotita Tonalito e; (2) Biotita Trondhjemito. Em geral, são rochas que apresentam foliação definida pelo bandamento composicional, localmente pode ser perturbada por dobras e bandas de cisalhamento. Suas características geoquímicas são compatíveis com os TTGs arqueanos do grupo de alto Al2O3, sendo ainda relativamente pobres em elementos ferromagnesianos, com padrões ETRP moderado a fortemente fracionados e anomalias de Eu discretas. As diferenças nas razões La/Yb e anomalia de Eu, possibilitou a discriminação de três grupos distintos de rochas: Os TTGs pertencentes ao grupo de alto La/Yb e Sr/Y são similares às rochas do Trondhjemito Mogno, descritos no Domínio Rio Maria. Estas rochas incluem a maioria das amostras da unidade Biotita Trondhjemito. No caso dos TTGs com médio a baixo La/Yb e Sr/Y quando comparadas com as rochas do Domínio Rio Maria possuem forte correlação com o Tonalito Caracol. Estes grupos são compostos principalmente pela unidade Epidoto-Biotita Tonalito, incluindo também amostras isoladas do Biotita Trondhjemito. Com base nos critérios utilizados acima, os leucogranodioritos da área foram divididos em dois grupos: Biotita Granodiorito e Leucogranodiorito. As rochas do Biotita Granodiorito possuem ampla ocorrência espacial na porção oeste da área, relações de campo mostram que são intrusivas nos granitoides TTGs. Os dados geoquímicos apontam que o Biotita Granodiorito possui padrões de ETR fortemente fracionados, com alta razão La/Yb (33 – 186) e anomalia de Eu positiva (1,11 < Eu/Eu* < 3,26), enquanto os leucogranodioritos mostram padrões levemente fracionados, com moderadas razões La/Yb (24,7 – 34,7) e anomalia de Eu ausente (Eu/Eu*= 1,03). Os diagramas de Harker para elementos maiores e traços não favorecem uma ligação genética por processo de cristalização fracionada entre o Biotita Granodiorito e as associações TTGs, uma vez que apresentam trends de evolução distintos, indicando portanto que as condições de sua gênese e diferenciação foram bem diferentes, tampouco por fusão parcial de uma fonte TTG, pelo fato de não apresentar significante anomalia negativa de Eu, bem como por exibir padrões similares de fracionamento de ETR em relação aos TTGs, atestando que essas rochas provavelmente não foram oriundas de magmas precursores desses TTGs.

"Do alto da colina" - a província do Rio Grande do Norte, o comércio, os rios Potengi e Jundiaí e o complexo comercial do Guarapes 1850 - 1900

The commercial complex Guarapes was during the second half of the nineteenth century most commercial street of Rio Grande do Norte province. In that time frame, you can see its flourishing as one of the central places of trade in the province in 1850, and its subsequent abandonment in 1900. This thesis aims to investigate, in its first part, the paths that help to understand, as the context of the expansion of global markets in the second half of the nineteenth century enabled the conditions for the emergence of the commercial complex. However, trade relations established in this province through the commercial complex, even participating in this global environment, reserved particular characteristics in their social and trade relations, as if dealing with a peripheral province, we look at the uniqueness of the relationship occurred in this space. In the second part, we seek to understand the importance that the rivers Potengi and Jundiaí had to install the commercial complex Guarapes in the second half of the nineteenth century. As the geographical position in relation to rivers, enabled this space became flow zone and confluence of goods distributed to the various parts of the interior of the province. We also monitor the process that made these rivers leave the role of mobility and transport relations in this space, giving way the railways and roads shooting. In the third part, we seek to understand the commercial complex Guarapes in focus. Analyzing their spatial distribution on the landscape, and how the spatial organization held at the same time traces of the Brazilian patriarchy exposed by Gilberto Freyre, but also "modern" features, due to the increase of a new culture inserted material in the province. We also seek to understand elements of material culture that was the environment of the complex, and how these materials are important sources for understanding this society under study. We treat from the biggest to the smallest fragments without hierarchize them. Understanding that, the study associated the written sources and materials provide a gain in understanding of everyday these people who lived in that area of the complex in the second half of the nineteenth century.

Vigilância Epidemiológica de Doenças Infecciosas de Origem Bacteriana na Província do Cuanza-Norte

seguinte trabalho teve como objetivo a pesquisa da vigilância epidemiológica das doenças infecciosas de origem bacteriana na província do Cuanza-Norte em Angola. Todos os resultados foram obtidos a partir da base de dados da Direção Provincial de Saúde do Cuanza-Norte em Ndalatando, onde foram recolhidos os dados relativos aos doentes com Febre Tifóide e Tuberculose de 2010-2014, sendo estas, as doenças bacterianas predominantes na província. Os dados recolhidos demonstram valores elevados relativos à pesquisa de Tuberculose e Febre Tifóide, tendo sido estudados casos de prevalência das doenças relacionadas com a idade, sexo e origem do município. Destaca-se a faixa etária de indivíduos com menos de 20 anos para o caso da Febre Tifóide e idades superiores aos 20 anos para a Tuberculose. Os municípios mais afectados para o caso da Febre Tifóide são Lukala, Bolongongo, Banga, Quikulungo, e Ngonguembo. Para o caso da Tuberculose são mais afectados os municípios de Gongembo, Banga, Quiculungo e Bolongongo, uma vez que são municípios em situação instável com uma escassa vigilância sanitária. No tempo húmido (chuvoso), os meses de Março e Abril se distinguiram com maiores taxas de prevalência de febre tifóide e no tempo seco (frio), os meses de Junho, Julho e Agosto se distinguiram com maiores taxas de prevalência de tuberculose durante este estudo. A análise dos resultados permite afirmar que se registou, durante os cinco (5) anos deste estudo, uma tendência crescente para a tuberculose e uma tendência decrescente para a Febre Tifóide. A prevalência é, ainda, muito elevada em ambos os casos, sendo, por isso, necessário agir rapidamente - aplicando as respetivas medidas de vigilância sanitária que haja um maior controlo efetivo e sustentável de doenças bacterianas negligenciadas e melhor acompanhamento dos doentes.

Caracterização da estruturação espacial dos povoamentos da epifauna do litoral rochoso do distrito de Mercúfi. província de Cabo Delgado (Norte de Moçambique), com uso de Sistema de Informação Geográfica: distribuição, abundância, diversidade e conservação

Dissertação de mest. em Estudos Marinhos e Costeiros, Faculdade de Ciências do Mar e do Ambiente, Univ. do Algarve, 2002

O papel do inapem no fomento do empreendedorismo na provincia do Kwanza Norte-Angola

Dissertação de Mestrado apresentada ao Instituto de Contabilidade e Administração do Porto para a obtenção do grau de Mestre em Empreendedorismo e Internacionalização, sob orientação de Celsa Maria Carvalho Machado e Adalmiro Álvaro Malheiro de Castro Andrade Pereira

Capital social e luta simbólica : o caso da Red Puna : uma experiência territorial de articulação social na província de Jujuy , Argentina

Na década de 1990 a noção de capital social alcançou ampla influência no âmbito das políticas públicas, aparecendo como uma nova alternativa para a promoção do desenvolvimento. Na esfera acadêmica, contudo, ainda não existe consenso sobre a conceitualização e as implicações desta nova noção nos processos sociais em geral. Por um lado, encontra-se a abordagem normativista, inspirada nos trabalhos de Putnam, que vê o capital social como um recurso utilizado pelas sociedades que contribui para melhorar a sua eficiência, promovendo o desenvolvimento econômico e melhorando o desempenho institucional e, conseqüentemente, ampliando o bem-estar social. Por outro lado, Bourdieu entende o capital social como uma das formas em que se expressa o poder, o qual é utilizado pelos agentes nas suas estratégias de reprodução. Este trabalho adota a perspectiva teórica de Bourdieu e tem por objetivo estudar o papel do capital social no processo de formação de uma organização social. Para isto, estuda-se a formação da Red Puna que é uma organização de segundo grau que articula diferentes organizações sociais nas regiões de Puna e Quebrada de Humahuaca, situadas no norte da Argentina. O método de pesquisa adotado é o qualitativo, sendo a técnica utilizada o de estudo de caso Entre as principais conclusões da pesquisa salienta-se a diversidade de usos que os agentes fazem do capital social, constituindo-se em aspecto-chave nas estratégias de reprodução social adotadas e nas relações de poder utilizadas nas suas lutas simbólicas.

Arcabouço geofísico, isostasia e causas do magmatismo cenozóico da província Borborema e de sua margem continental (Nordeste do Brasil)

The Borborema Province (BP) is a geologic domain located in Northeastern Brazil. The BP is limited at the south by the São Francisco craton, at the west by the Parnaíba basin, and both at the north and east by coastal sedimentary basins. Nonetheless the BP surface geology is well known, several key aspects of its evolution are still open, notably: i)its tectonic compartmentalization established after the Brasiliano orogenesis, ii) the architecture of its cretaceous continental margin, iii) the elastic properties of its lithosphere, and iv) the causes of magmatism and uplifting which occurred in the Cenozoic. In this thesis, a regional coverage of geophysical data (elevation, gravity, magnetic, geoid height, and surface wave global tomography) were integrated with surface geologic information aiming to attain a better understanding of the above questions. In the Riacho do Pontal belt and in the western sector of the Sergipano belt, the neoproterozoic suture of the collision of the Sul domain of the BP with the Sanfranciscana plate (SFP) is correlated with an expressive dipolar gravity anomaly. The positive lobule of this anomaly is due to the BP lower continental crust uplifting whilst the negative lobule is due to the supracrustal nappes overthrusting the SFP. In the eastern sector of the Sergipano belt, this dipolar gravity anomaly does not exist. However the suture still can be identified at the southern sector of the Marancó complex arc, alongside of the Porto da Folha shear zone, where the SFP N-S geophysical alignments are truncated. The boundary associated to the collision of the Ceará domain of the BP with the West African craton is also correlated with a dipolar gravity anomaly. The positive lobule of this anomaly coincides with the Sobral-Pedro II shear zone whilst the negative lobule is associated with the Santa Quitéria magmatic arc. Judging by their geophysical signatures, the major BP internal boundaries are: i)the western sector of the Pernambuco shear zone and the eastern continuation of this shear zone as the Congo shear zone, ii) the Patos shear zone, and iii) the Jaguaribe shear zone and its southwestern continuation as the Tatajuba shear zone. These boundaries divide the BP in five tectonic domains in the geophysical criteria: Sul, Transversal, Rio Grande do Norte, Ceará, and Médio Coreaú. The Sul domain is characterized by geophysical signatures associated with the BP and SFP collision. The fact that Congo shear zone is now proposed as part of the Transversal domain boundary implies an important change in the original definition of this domain. The Rio Grande do Norte domain presents a highly magnetized crust resulted from the superposition of precambrian and phanerozoic events. The Ceará domain is divided by the Senador Pompeu shear zone in two subdomains: the eastern one corresponds to the Orós-Jaguaribe belt and the western one to the Ceará-Central subdomain. The latter subdomain exhibits a positive ENE-W SW gravity anomaly which was associated to a crustal discontinuity. This discontinuity would have acted as a rampart against to the N-S Brasiliano orogenic nappes. The Médio Coreaú domain also presents a dipolar gravity anomaly. Its positive lobule is due to granulitic rocks whereas the negative one is caused by supracrustal rocks. The boundary between Médio Coreaú and Ceará domains can be traced below the Parnaíba basin sediments by its geophysical signature. The joint analysis of free air anomalies, free air admittances, and effective elastic thickness estimates (Te) revealed that the Brazilian East and Equatorial continental margins have quite different elastic properties. In the first one 10 km < Te < 20 km whereas in the second one Te ≤ 10 km. The weakness of the Equatorial margin lithosphere was caused by the cenozoic magmatism. The BP continental margin presents segmentations; some of them have inheritance from precambrian structures and domains. The segmentations conform markedly with some sedimentary basin features which are below described from south to north. The limit between Sergipe and Alagoas subbasins coincides with the suture between BP and SFP. Te estimates indicates concordantly that in Sergipe subbasin Te is around 20 km while Alagoas subbasin has Te around 10 km, thus revealing that the lithosphere in the Sergipe subbasin has a greater rigidity than the lithosphere in the Alagoas subbasin. Additionally inside the crust beneath Sergipe subbasin occurs a very dense body (underplating or crustal heritage?) which is not present in the crust beneath Alagoas subbasin. The continental margin of the Pernambuco basin (15 < Te < 25 km) presents a very distinct free air edge effect displaying two anomalies. This fact indicates the existence in the Pernambuco plateau of a relatively thick crust. In the Paraíba basin the free air edge effect is quite uniform, Te ≈ 15 km, and the lower crust is abnormally dense probably due to its alteration by a magmatic underplating in the Cenozoic. The Potiguar basin segmentation in three parts was corroborated by the Te estimates: in the Potiguar rift Te ≅ 5 km, in the Aracati platform Te ≅ 25 km, and in the Touros platform Te ≅ 10 km. The observed weakness of the lithosphere in the Potiguar rift segment is due to the high heat flux while the relatively high strength of the lithosphere in the Touros platform may be due to the existence of an archaean crust. The Ceará basin, in the region of Mundaú and Icaraí subbasins, presents a quite uniform free air edge effect and Te ranges from 10 to 15 km. The analysis of the Bouguer admittance revealed that isostasy in BP can be explained with an isostatic model where combined surface and buried loadings are present. The estimated ratio of the buried loading relative to the surface loading is equal to 15. In addition, the lower crust in BP is abnormally dense. These affirmations are particularly adequate to the northern portion of BP where adherence of the observed data to the isostatic model is quite good. Using the same above described isostatic model to calculate the coherence function, it was obtained that a single Te estimate for the entire BP must be lower than 60 km; in addition, the BP north portion has Te around 20 km. Using the conventional elastic flexural model to isostasy, an inversion of crust thickness was performed. It was identified two regions in BP where the crust is thickened: one below the Borborema plateau (associated to an uplifting in the Cenozoic) and the other one in the Ceará domain beneath the Santa Quitéria magmatic arc (a residue associated to the Brasiliano orogenesis). On the other hand, along the Cariri-Potiguar trend, the crust is thinned due to an aborted rifting in the Cretaceous. Based on the interpretation of free air anomalies, it was inferred the existence of a large magmatism in the oceanic crust surrounding the BP, in contrast with the incipient magmatism in the continent as shown by surface geology. In BP a quite important positive geoid anomaly exists. This anomaly is spatially correlated with the Borborema plateau and the Macaú-Queimadas volcanic lineament. The integrated interpretation of geoid height anomaly data, global shear velocity model, and geologic data allow to propose that and Edge Driven Convection (EDC) may have caused the Cenozoic magmatism. The EDC is an instability that presumably occurs at the boundary between thick stable lithosphere and oceanic thin lithosphere. In the BP lithosphere, the EDC mechanism would have dragged the cold lithospheric mantle into the hot asthenospheric mantle thus causing a positive density contrast that would have generated the main component of the geoid height anomaly. In addition, the compatibility of the gravity data with the isostatic model, where combined surface and buried loadings are present, together with the temporal correlation between the Cenozoic magmatism and the Borborema plateau uplifting allow to propose that this uplifting would have been caused by the buoyancy effect of a crustal root generated by a magmatic underplating in the Cenozoic

A história do intemperismo na Província Borborema Oriental, Nordeste do Brasil: implicações paleoclimáticas e tectônicas

Until some years ago, weathering geochronology was primarily based on the K-Ar and 40Ar/39Ar dating of supergene minerals. Recent advances in the analysis of supergene goethite by the (U-Th)/He method expanded the number of suitable minerals for such purpose, as well as the time of application for weathering geochronology. This study represents the first systematic approach in Brazil, combining both the 40Ar/39Ar e (U-Th)/He methodologies to improve the knowledge on the weathering and the age of nonfossiliferous sediments. Supported by geologic and geomorphologic correlations, we identified different types of weathering profiles occurring in the interior and coastal areas of northeastern Brazil. These profiles were correlated to main regional geomorphological domains: the Borborema Plateau , the Sertaneja Depression , and the Coastal Cuestas and Plains, and respective planation surfaces, which study is fundamental to understand the landscape evolution of the northern portion of the eastern Borborema Province. The depth and stratigraphic organization of the weathering profiles in each of the geomorphological domains permitted to establish that: (i) the profiles on the highlands that cap the Borborema Surface are deeper (up to 100 m) and can be considered as typical lateritic profiles; (ii) on the lowlands that form the Sertaneja Surface , the weathering profiles are shallow and poorly developed (2-5 m deep); (iii) the profiles along the coastal area are moderately developed (up to 25 m deep), and are characterized by thick saprolites and mottle zones. Aiming to establish the timing of the evolution of northeastern Brazil, we studied 29 weathering profiles representing distinct topographic levels of the Borborema Province, from the highlands to the coast, through the analysis of 248 grains of supergene manganese oxides using laser step-heating 40Ar/39Ar geochronology. Additionally, we applied the (U-Th)/He method in 20 weathering profiles, by dating 171 grains of supergene iron oxides and hydroxides. Geochronological results for 248 grains of manganese oxides analyzed by the 40Ar/39Ar method indicate that the weathering profiles in the study area record the history of weathering from the Oligocene to the Pleistocene, with ages in the order of 31.4 ± 1.0 Ma to 0.8 ± 0.4 Ma. Dating of 171 grains of goethite by the (U-Th)/He method yielded ages ranging from 43.2 ± 4.3 Ma to 0.8 ± 0.1 Ma, suggesting the weathering processes last from the Eocene to the Pleistocene. The precipitation of supergene goethite in this interval confirms the age of the weathering processes identified from the manganese oxides record. 105 goethite grains from 8 different occurrences of the Barreiras Formation were dated by the (U-Th)/He method. Five grains collected from the cement in the Barreiras Formation sandstones, in the Lagoa Salgada and Rio do Fogo coastal cuestas, yielded ages of 17.6 ± 1.8 Ma, 17.3 ± 1.7 Ma, 16.3 ± 1.6 Ma, 16.2 ± 1.6 Ma and 13.6 ± 1.4 Ma. Results of 69 goethite grains from authigenic pisoliths collected in 7 different localities also yielded concordant ages, varying from 17.8 ± 1.8 to 7.5 ± 0.8 Ma. Results obtained from 31 detrital grains are concordant in 3 distinct localities (Lagoa Salgada, Praia da Garças e Ponta Grossa); they vary in the range of 43.2 ± 4.3 to 21.6 ± 2.2 Ma, and indicate that the maximum age for the Barreiras Formation deposition is around 22 Ma. 40Ar/39Ar results for 15 manganese oxides grains associated with the Barreiras Formation weathering profiles, in 3 different localities, vary from 13.1 ± 0.9 to 7.7 ± 0.4 Ma, in the same range of ages obtained by the (U-Th)/He method. The systematic application of the 40Ar/39Ar and (U-Th)/He methods, respectively for manganese oxides and goethites, show that the Barreiras Formation sediments were already deposited since ca. 17 Ma, and that the weathering processes were active until ca. 7 Ma ago. The ages obtained from manganese oxides collected in the Cenozoic basalts (Macau Formation) also reveal a weathering history between 19 and 7 Ma, pointing to hot and humid conditions during most of the Miocene. 40Ar/39Ar ages yielded by manganese oxides associated with the Serra do Martins Formation vary from 14.1 ± 0.4 to 10.5 ± 0.3 Ma. On the other hand, (U-Th)/He ages from iron oxides/hydroxides collected in the Serra do Martins Formation mesas vary from 20.0 ± 2.0 to 5.5 ± 0.6 Ma, indicating that those sediments are older than 20 Ma. 40Ar/39Ar and (U-Th)/He results produced in this study are in agreement with paleoclimatic interpretations based on stable isotopes and clay index values measured in the Atlantic Ocean sediments, validating the use of weathering geochronology to investigate paleoclimatic variations. The direct dating of the Barreiras Formation permitted, for the first time, confident inferences on the age of the brittle deformation recorded by this sedimentary unit in the Rio Grande do Norte and Ceará states. The first event, syn-deposition, occurred during the early Miocene; an younger event, related to the post-depositional deformation of the Barreiras Formation, is associated with tectonic activity from the very early Miocene to the Holocene. In agreement with data from other areas, results obtained in this study reveal that the depth and complexity of the weathering profiles reflect the time of exposition of such areas to the weathering agents close to the surface. However, there is no clear relationship between ages vs. altitude. The depth and the stratigraphic organization of weathering profiles in northeastern Brazil, contrary to the southeastern Brazil pattern, do not vary toward the coast. In our study area, field observations reveal the presence of ancient, thick and complex lateritic profiles preserved in the sedimentary mesas on the Borborema Plateau, as younger, narrow and incipient ones occur in the dissected areas. Geochronological results obtained for these profiles yielded older ages on the high altitudes, and younger ages in the lowlands, suggesting the scarp retreatment is the most reliable model to explain the regional landscape evolution. However, in the coastal lowlands, the relatively older ages obtained indicate that more complexes processes were involved in the modeling of the local relief

Geologia, Geocronologia, Geoquímica e Petrogênese das Rochas Ígneas Cretácicas da Província Magmática do Cabo e suas Relações com as Unidades Sedimentares da Bacia de Pernambuco (NE do Brasil)

The area studied forms a thin NNE-directed belt situated south of Recife town (Pernambuco state), northeastern Brazil. Geologically, it comprises the Pernambuco Basin (PB), which is limited by the Pernambuco Lineament to the north, the Maragogi high to the south and the Pernambuco Alagoas massif to the west, all of them with Precambrian age. This thesis reports the results obtained for the Cabo Magmatic Province (CMP), aiming the characterization of the geology, stratigraphy, geochronology, geochemistry and petrogenesis of the Cretaceous igneous rocks presented in the PB. The PB is composed of the Cabo Formation (rift phase) at the base (polymictic conglomerates, sandstones, shales), an intermediate unit, the Estiva Formation (marbles and argillites), and, at the top, the Algodoais Formation (monomictic conglomerates, sandstones, shales). The CMP is represented by trachytes, rhyolites, pyroclastics (ignimbrites), basalts / trachy-andesites, monzonites and alkali-feldspar granite, which occur as dykes, flows, sills, laccoliths and plugs. Field observations and well descriptions show that the majority of the magmatic rocks have intrusive contacts with the Cabo Formation, although some occurrences are also suggestive of synchronism between volcanism and siliciclastic sedimentation. 40Ar/39Ar and zircon fission tracks for the magmatic rocks indicate an average age of 102 r 1 Ma for the CMP. This age represents an expressive event in the province and is detected in all igneous dated materials. It is considered as a minimum age (Albian) for the magmatic episode and the peak of the rift phase in the PB. The 40Ar/39Ar dates are about 10-14 Ma younger than published palynologic ages for this basin. Geochemically, the CMP may be divided in two major groups; i) a transitional to alkaline suite, constituted by basalts to trachy-andesites (types with fine-grained textures and phenocrysts of sanidine and plagioclase), trachytes (porphyrytic texture, with phenocrysts of sanidine and plagioclase) and monzonites; ii) a alkaline suite, highly fractionated, acidic volcano-plutonic association, formed by four subtypes (pyroclastic flows ignimbrites, fine-to medium-grained rhyolites, a high level granite, and later rhyolites). These four types are distinguished essentially by field aspects and petrographic and textural features. Compatible versus incompatible trace element concentrations and geochemical modeling based on both major and trace elements suggest the evolution through low pressure fractional crystallization for trachytes and other acidic rocks, whereas basalts / trachy-andesites and monzonites evolved by partial melting from a mantle source. Sr and Nd isotopes reveal two distinct sources for the rocks of the CMP. Concerning the acidic ones, the high initial Sr ratios (ISr = 0.7064-1.2295) and the negative HNd (-0.43 to -3.67) indicate a crustal source with mesoproterozoic model ages (TDM from 0.92 to 1.04 Ga). On the other hand, the basic to intermediate rocks have low ISr (0.7031-0.7042) and positive HNd (+1.28 to +1.98), which requires the depleted mantle as the most probable source; their model ages are in the range 0.61-0.66 Ga. However, the light rare earth enrichment of these rocks and partial melting modeling point to an incompatible-enriched lherzolitic mantle with very low quantity of garnet (1-3%). This apparent difference between geochemical and Nd isotopes may be resolved by assuming that the metasomatizing agent did not obliterate the original isotopic characteristics of the magmas. A 2 to 5% partial melting of this mantle at approximately 14 kbar and 1269oC account very well the basalts and trachy-andesites studied. By using these pressure and temperatures estimates for the generation of the basaltic to trachy-andesitic magma, it is determined a lithospheric stretching (E) of 2.5. This E value is an appropriated estimate for the sub-crustal stretching (astenospheric or the base of the lithosphere?) region under the Pernambuco Basin, the crustal stretching probably being lower. The integration of all data obtained in this thesis permits to interpret the magmatic evolution of the PB as follows; 1st) the partial melting of a garnet-bearing lherzolite generates incompatible-enriched basaltic, trachy-andesitic and monzonitic magmas; 2nd) the underplating of these basaltic magmas at the base of the continental crust triggers the partial melting of this crust, and thus originating the acidic magmas; 3rd) concomitantly with the previous stage, trachytic magmas were produced by fractionation from a monzonitic to trachy-andesitic liquid; 4th) the emplacement of the several magmas in superficial (e.g. flows) or sub-superficial (e.g. dykes, sills, domes, laccoliths) depths was almost synchronically, at about 102 r 1 Ma, and usually crosscutting the sedimentary rocks of the Cabo Formation. The presence of garnet in the lherzolitic mantle does not agree with pressures of about 14 kbar for the generation of the basaltic magma, as calculated based on chemical parameters. This can be resolved by admitting the astenospheric uplifting under the rift, which would place deep and hot material (mantle plume?) at sub-crustal depths. The generation of the magmas and their subsequent emplacement would be coupled with the crustal rifting of the PB, the border (NNE-SSW directed) and transfer (NW-SE directed) faults serving as conduits for the magma emplacement. Based on the E parameter and the integration of 40Ar/39Ar and palynologic data it is interpreted a maximum duration of 10-14 Ma for the rift phase (Cabo Formation clastic sedimentation and basic to acidic magmatism) of the PB

Evolução morfotectônica do maciço estrutural pereiro, província Borborema

The Northeast relief was described by the Pediplanation Model. This action discards the theoretical basis of post-Cretaceous tectonic evolution of the landscape. Through this model the Massif Pereiro - MP, Borborema Province, was established as part of the Tablelands Area Residual Sertanejos. The present work aims to establish the post- Cretaceous morphotectonic evolution of the MP by geomorphological and geological mapping using Geographic Information System, Remote Sensing and dating of sediments by Single Aliquot Regenerative-dose (SAR). The MP is contained in the core semi-arid, annual precipitation of 600-800 mm / year. The MP is NE-SW, is limited by Shear Zone Jaguaribe (ZCJ) and Portalegre Shear Zone (ZCPa), the same attitude, and crossed by several other shear zones. These shear zones show evidence of brittle Cenozoic reactivation, mostly as normal faults and shallow crustal level. The Quaternary sedimentation around the MP focuses on fault escarpments in a general pattern cascade, where ages decrease from the summits of the steep foothills. The ages of 51 sediment samples indicate a correlation with global climate following pulses: Last Interestadial-UI, the Last Glacial Maximum - LGM and the transition Pleistocene / Holocene, while the latter focus on 18 of 51 samples dated. This study also finds evidence of a new quaternary basin, here called Merejo Basin. Through these results it is concluded that no evidence of post-Cretaceous tectonic evolution of morphological MP, as their retreat along the fault scarps, invariably following the trend of the shear zones. The erosion of cliffs in large time scale is controlled by weakness zones generated by faults on the other hand the erosion of cliffs in short time, with the formation of deposits and colluvial horizons pedogenizados, has climate control. It was also found that in the study area there is a preponderance of past and current tectonic erosion processes on the morphological evolution