Solos do campo experimental da Embrapa Algodão, em Patos-PB: levantamento detalhado e potencial edáfico.

2002

Avaliação institucional : impactos no currículo dos cursos de licenciatura plena das faculdades integradas de patos - pb

O presente trabalho dissertativo objetivou levantar e descrever os impactos causados pela Avaliação Institucional do MEC no âmbito do currículo dos cursos superiores de Licenciatura Plena, tomando-se como objeto empírico de verificação as Faculdades Integradas de Patos – FIP. Em linhas gerais, o referido trabalho evidencia o histórico da avaliação institucional brasileira, identificando os modelos avaliativos: PAIUB, ENC e SINAES, levando-se em consideração as ideias conceituais de teóricos, como: Leite (1997), Brito (2006), Buarque (2005), Dias Sobrinho (2000), Balzan (2005), Catani (1997), Gadotti (2005), Trindade (1999), dentre outros. Apresenta a organização curricular dos Cursos de Licenciatura Plena das Faculdades Integradas de Patos que são: Geografia, História, Letras e Pedagogia, identificando cada curso a partir de sua matriz curricular, destacando a proposta do Plano de Desenvolvimento Institucional e do Plano Pedagógico Institucional da IES. Por último, mostra os resultados da pesquisa de campo que foi desenvolvida a partir da aplicação de questionários direcionados aos segmentos dos Docentes, Coordenadores de Curso, Coordenações Acadêmicas e Membros da Comissão Própria de Avaliação das FIP. Com base nos resultados da pesquisa de campo, os Cursos de Licenciatura Plena das FIP nesta última década, sofrerem e vem sofrendo os impactos das avaliações institucionais do MEC. Tais impactos configuramse a partir de perspectivas mais positivas do que negativas, pois estes cursos desde que começaram a participar do processo avaliativo do MEC, que se veem envolvidos em processos de auto-avaliação, tanto interno como externo, apresentando melhorias significativas.

Estudo de águas subterrâneas com métodos elétricos na região do semi-árido de Patos - Pb

O Nordeste do Brasil, em particular a região semi-árida do Estado da Paraíba, é muito castigada pelos períodos de grandes estiagens e escassez de recursos hídricos. A água de superfície não supre a demanda da região, portanto, a busca de água subterrânea e sua exploração é uma constante nos programas dos Governos Federal e Estadual. Nesta região, ocorrem geralmente apenas aquíferos aluviais rasos e aquíferos nas fraturas do embasamento cristalino. Tradicionalmente, as fraturas no cristalino são prospectados através de estudos aerofotogramétricos e geoestruturais, com média de 30% de furos secos. O dimensionamento dos aquíferos aluviais é feito através de perfurações sistemática do subsolo, que é uma metodologia muito demorosa e cara. O objetivo deste trabalho é mostrar que o emprego de métodos geofísicos, especialmente os métodos geoelétricos, são eficazes e econômicos para localizar e avaliar áreas promissoras de água subterrânea, tanto nos aquíferos aluviais como nos cristalinos. Neste trabalho, foram aplicados o convencional método da eletroresistividade e o método eletromagnético, ainda pouco usado na prospecção de água subterrânea, em três áreas selecionadas na região semi-árida de Patos - Pb, sendo duas representantes dos aquíferos aluviais e uma representante dos aquíferos cristalinos. Nos aquíferos aluviais, foi determinada a profundidade até o embasamento cristalino através de sondagens elétricas verticais (SEVs), e os respectivos limites laterais foram mapeados com perfilagens de eletroresistividade. Os resultados das SEVs são coerentes com as profundidades obtidas pelas sondagens mecânicas de confirmação mostrando, assim, a aplicabilidade desta metodologia na pesquisa deste tipo de aquífero. No aquífero cristalino, inicialmente determinou-se a orientação geral das zonas fraturadas do embasamento cristalino pela técnica modificada da sondagem elétrica vertical (SEV Radial) e, em seguida, a localização exata em planta das mesmas foram determinadas com perfilagens de eletroresistividade e eletromagnéticas no sistema horizontal coplanar nas frequências 880 Hz e 2640 Hz. Os resultados dos dois métodos utilizados foram satisfatórios, porém, a perfilagem eletromagnética é mais rápida, necessita de menos mão de obra, reduzindo assim os custos de prospecção de água subterrânea no embasamento cristalino.

Ensino jurídico e cidadania : uma investigação acerca do PRAJUR (Núcleo de Prática Jurídica) das faculdades integradas de PATOS (FIP)

Esta dissertação aborda o tema do ensino jurídico e cidadania e da função social do Núcleo de Prática Jurídica(PRAJUR) da FIP-Faculdades Integradas de Patos-PB. Para analisar o ensino jurídico e cidadania do PRAJUR/FIP, parte-se da Resolução nº 09/2004/MEC que sucedeu a Portaria nº 1.886/94/MEC, onde instituiu a implantação de escritórios jurídicos em todos os cursos de Direito, na busca de melhor delinear o conhecimento prático dos acadêmicos. Os objetivos da pesquisa foram: descrever que através do conhecimento tem-se uma forma de diminuir a distância entre os níveis sociais e um caminho à buscar cidadania pela educação, refletir sobre o acesso à justiça como um direito de cidadania e analisar a função social do PRAJUR/FIP no acesso à justiça. A coleta dos dados foi realizada através de bibliografia, doutrina, dados documentais e aplicação de questionários. A dissertação foi organizada de forma a contemplar educação jurídica e efeitos práticos no exercício da cidadania onde no primeiro capítulo discorre-se sobre a educação e suas transversalidades aplicáveis atualmente na sociedade. No segundo capítulo abordou-se além da função social do PRAJUR/FIP no acesso à justiça, apresenta-se os dados coletados junto aos educadores em forma de entrevista do PRAJUR/FIP, e em forma de pesquisa dados coletados de exalunos e usuário. Finalmente, no terceiro capítulos aborda-se a evolução dos cursos de Direito e a formação acadêmica do educando.

Avaliação escolar no ensino superior de letras: entre o discurso e a prática

O objeto desta pesquisa é a avaliação da aprendizagem, tendo como foco central a análise dos discursos e práticas dos professores de Cursos de Licenciatura de Letras. Este estudo foi desenvolvido com docentes de duas instituições de ensino superior do interior do estado da Paraíba, localizado no nordeste brasileiro. O objetivo geral deste estudo é: analisar as semelhanças, diferenças e contradições resultantes da comparação entre os discursos e o que se pratica na avaliação da aprendizagem dos professores de Letras do Ensino Superior de uma instituição de ensino superior particular de Patos/PB e os de uma pública de Catolé do Rocha/PB. Esta foi uma pesquisa qualitativa com uma amostra de cinco docentes de cada estabelecimento de ensino superior, somando-se dez ao todo. Foram feitas entrevistas com perguntas abertas e fechadas, cujas respostas tiveram uma análise de conteúdo, e o resultado desta foi confrontado com os dados da observação das práticas de sala de aula dos professores da amostra. Constatou-se que há casos de professores que têm discursos diferentes da sua prática de avaliação da aprendizagem. Há também problemas de interação entre docentes e discentes em relação à avaliação da aprendizagem que aumentam o índice de reprovação do alunado, o que poderia ser evitado. No entanto, de modo geral há um compromisso com a qualidade de ensino dos docentes entrevistados. Os autores e teóricos que inspiraram esta pesquisa foram: Wachowicz (2000), Castanho (2000), Berbel (2001), Sacristán e Gómez (1998), Hoffman (1996 e 2003), Luckesi (1994), Vasconcelos (2000) e Villas Boas (2000), entre outros.

Prevalence of leptospirosis in dairy goats in the semiarid region of Paraiba state

Higino S.S.S., Alves C.J., Santos C.S.A.B., Vasconcellos S.A., Silva M.L.C.R., Brasil A.W.L., Pimenta C.L.R.M. & Azevedo S.S. 2012. [Prevalence of leptospirosis in dairy goats in the semiarid region of Paraiba state.] Prevalencia de leptospirose em caprinos leiteiros do semiarido paraibano. Pesquisa Veterinaria Brasileira 32(3):199-203. Universidade Federal de Campina Grande, Centro de Saude e Tecnologia Rural, Unidade Academica de Medicina Veterinaria, Av. Universitaria s/n, Patos, PB 58700-970, Brazil. E-mail: sergio.azevedo@pq.cnpq.br This study aimed to determine the prevalence of positive dairy goat herds and seropositive animals for leptospirosis in the semiarid region of Paraiba state, Brazil. Sampling was designed to determine the prevalence of positive herds (foci) and seropositive animals for leptospirosis. A total of 975 serum samples were collected from goats of 110 dairy herds in the Monteiro municipality, Western Cariri microregion of Paraiba. For the serological diagnosis of leptospirosis the microscopic agglutination test (MAT) was carried out using 24 Leptospira spp. serovars as antigens. A herd was considered positive when existed at least one seropositive animal. The prevalence of positive herds and seropositive animals were 43.6% (95% CI = 34.2-53.4%) and 8.7% (95% CI = 58.7-12.9%) respectively. The most frequent serovars in goats were Autumnalis (1.74%; 95% CI = 0.97-3.09%), Sentot (1.71%; 95% CI = 0.82-3.52%) and Whitcomb (1.39%; 95% CI = 0.65-2.93%), and by herd, serovars Autumnalis (10.9%; 95% CI = 5.8-18.3%), Whitcomb (8.2%; 95% CI = 3.8-15.0%) and Sentot and Patoc (7.3%; 95% CI = 3.2-13.8%) were the most frequent. It is suggested that leptospirosis is spread in goats in the region, and that there is need to implement control and preventive measures in order to reduce infection and economic losses, and to avoid possible transmission of infection to humans.

Epidemiological characterization and risk factors associated with leptospirosis in the brazilian semiarid

Alves C. J., Alcino J. F., Farias A. E. M., Higino S. S. S., Santos F. A., Azevedo S. S., Costa D. F. & Santos C. S. A. B. 2012. [Epidemiological characterization and risk factors associated with leptospirosis in the brazilian semiarid.] Caracterizacao epidemiologica e fatores de risco associados a leptospirose em ovinos deslanados do semiarido brasileiro. Pesquisa Veterinaria Brasileira 32(6): 523-528. Universidade Federal de Campina Grande, Centro de Sa de e Tecnologia Rural, Unidade Academica de Medicina Veterinaria, Av. Universitaria s/n(o), Patos, PB 58700-970, Brazil. E-mail: clebertja@uol.com.br The aim of this investigation was to determine the herd-level and animal-level prevalence of leptospirosis in sheep from the semiarid of Paraiba State, Northeast Brazil, as well as to identify risk factors. Blood samples were collected from 1,275 sheep from 117 flocks in 19 counties in the Sertao mesoregion, Paraiba. For the serological diagnosis of leptospirosis the microscopic agglutination test (MAT) using 24 Leptospira spp. serovars as antigens was carried out. Of the 117 flocks studied 33 (28.20%) presented at least one seropositive sheep, and of the 1,275 animals 69 (5.41%) were seropositive with titers ranging from 100 to 3,200. Reactant serovars were Autumnalis (49.30%), Andamana (27.53%), Sentot (17.39%), Whitcomb (4.34%) and Australis (1.44%). Herd size > 48 sheep (odds ratio = 2.26; 95% CI = 1.33-5.07; p = 0.021) and participation in animal exhibits (odds ratio = 9.05; 95% CI = 0.96-85.71; p = 0.055) were identified as risk factors. The need was suggested for studies on the isolation of the agent, characterization of its pathogenicity and its economic impact on sheep flocks of the region, and sanitary control in sheep agglomerations was recommended.

Seroprevalence and risk factors associated with Chlamydophila abortus infection in dairy goats in the Northeast of Brazil

Santos C.S.A.B., Piatti R.M., Azevedo S.S., Alves C.J., Higino S.S.S., Silva M.L.C.R., Brasil A.W.L. & Gennari S.M. 2012. Seroprevalence and risk factors associated with Chlamydophila abortus infection in dairy goats in the Northeast of Brazil. Pesquisa Veterinaria Brasileira 32(11):1082-1086. Unidade Academica de Medicina Veterinaria, Centro de Sa de e Tecnologia Rural, Universidade Federal de Campina Grande, Av. Universitaria s/n, Bairro Santa Cecilia, Patos, PB 58700-970, Brazil. E-mail: sergio.azevedo@pq.cnpq.br Few data are available on the prevalence and risk factors of Chlamydophila abortus infection in goats in Brazil. A cross-sectional study was carried out to determine the flock-level prevalence of C. abortus infection in goats from the semiarid region of the Paraiba State, Northeast region of Brazil, as well as to identify risk factors associated with the infection. Flocks were randomly selected and a pre-established number of female goats >= 12 mo old were sampled in each of these flocks. A total of 975 serum samples from 110 flocks were collected, and structured questionnaire focusing on risk factors for C. abortus infection was given to each farmer at the time of blood collection. For the serological diagnosis the complement fixation test (CFT) using C. abortus S26/3 strain as antigen was performed. The flock-level factors for C. abortus prevalence were tested using multivariate logistic regression model. Fifty-five flocks out of 110 presented at least one seropositive animal with an overall prevalence of 50.0% (95%; CI: 40.3%, 59.7%). Ninety-one out of 975 dairy goats examined were seropositive with titers >= 32, resulting in a frequency of 9.3%. Lend buck for breeding (odds ratio = 2.35; 95% CI: 1.04-5.33) and history of abortions (odds ratio = 3.06; 95% CI: 1.37-6.80) were associated with increased flock prevalence.

Quantificação de metais (Al, Fe, Mn, Pb, Zn e Cu) nos sedimentos do sistema estuarino das Ilhas de Tinharé-Boipeba (Bahia - Brasil)

O sistema estuarino das Ilhas de Tinharé-Boipeba está inserido na região do Baixo Sul baiano (Bahia Brasil), costa nordeste brasileira, e conectam-se com o oceano através de três saídas principais, Morro de São Paulo, Boipeba e Barra dos Carvalhos. Informações relacionadas à presença de metais no sedimento são quase inexistentes para a região. Nestes estuários foram coletadas 40 amostras de sedimento, onde analisou-se a concentração de metais (Al, Cu, Fe, Mn, Pb e Zn) através da extração com água-régia, segundo o protocolo do material de referência BCR-701 (RAURET et al., 2001). Baixas concentrações de metais foram registradas nas proximidades das saídas para o mar e no Canal de Garapuá e Rio Grande. Altas concentrações, porém praticamente dentro dos valores de referência na CONAMA 344/04, foram registradas no Rio Una, na maior parte do Rio Cairu, Rio das Almas, em quase todas as estações, no braço leste do Rio Cairu e na porção intermediária do Rio dos Patos. As concentrações dos metais (mg.kg1) apresentaram valores entre os seguintes intervalos, Al (3,57 x 104 a 3,19 x 102), Cu (1,02 x 102 a 0,35), Fe (4,33 x 104 a 2,05 x 102), Mn (1,44 x 103 a 2,73), Pb (6,67 x 101 a 2,66) e Zn (5,08 x 102 a 3,18). Através da análise estatística ACP (Análise dos Componentes Principais) e dos gráficos de correlação entre a granulometria do sedimento (areia, silte e argila) e os metais, observou-se maiores concentrações de metais com o aumento do percentual de silte e diminuição do percentual de areia. Também se identificou uma forte correlação entre a ocorrência do fósforo e a presença de metais. Acredita-se que a principal espécie química em questão seja o fosfato (PO43 ou P2O5) que é uma base dura, onde a ligação com os metais se dá pelo oxigênio, sendo o caráter iônico relevante. Não foi identificada uma correlação entre a presença de metais e a argila, fato atribuído ao baixo teor dessa granulometria para todas as amostras do estudo e a composição da argila desses estuários

Precambrian history of the Zona Transversal of the Borborema Province, NE Brazil: Insights from Sm-Nd and U-Pb geochronology

The Borborema Province has three major subprovinces. The northern subprovince lies north of the Patos shear zone and is comprised of Paleoproterozoic cratonic basement with Archean nuclei, plus overlying Neoproterozoic supracrustal rocks and Brasiliano plutonic rocks. The central subprovince occurs between the Patos and Pernambuco shear zones and is mainly comprised of the Zona Transversal. The southern subprovince occurs between the Pernamabuco shear zone and the Sao Francisco craton and is comprised of a tectonic collage of various blocks, terranes, or domains ranging in age from Archean to Neoproterozoic. This report focuses on the Zona Transversal, especially on Brasiliano rocks for which we have the most new information. Paleoproterozoic gneisses with ages of 2.0-2.2 Ga occur discontinuously throughout the Zona Transversal. The Cariris Velhos suite consists of metavolcanic, metasedimentary, and metaplutonic rocks yielding U-Pb zircon ages of 995-960 Ma. This suite is mainly confined to a 100 km wide belt that extends for more than 700 km within the Alto Pajeu terrane. Sm-Nd model ages in metaigneous rocks cluster about 1.3-1.6 Ga, indicating that older crust was involved in genesis of their magmas. Brasiliano supracrustal rocks dominate the Pianco-Alto Brigida terrane, and they probably also constitute significant parts of the Alto Pajeu and Rio Capibaribe terranes. They are only slightly older than early stages of Brasiliano plutonism, with detrital zircon ages at least as young as 620 Ma; most T(DM) ages range from 1.2 to 1.6 Ga. Brasiliano plutons range from ca. 640 to 540 Ma, and their T(DM) ages range from 1.2 to 2.5 Ga. Previous workers have shown significant correlations among U-Pb ages, Sm-Nd model ages, petrology, and geochemistry, and we are able to reinforce and extend these correlations. Stage I plutons formed 640 -610 Ma and have T(DM) ages less than 1.5 Ga. Stage 11 (610-590 Ma) contains few plutons, but coincides with the peak of compressional deformation, metamorphism, and formation of migmatites. Stage III plutons (590 to ca. 575 Ma) have older T(DM) ages (ca. 1.8-2.0 Ga), as do Stage IV plutons (575 to ca. 550 Ma; T(DM) from 1.9 to 2.4 Ga). Stage III plutons formed during the transition from compressional to transcurrent deformation, while Stage IV plutons are mainly post-tectonic. Stage V plutons (550-530 Ma) are commonly undeformed (except along younger shear zones) and have A-type geochemistry. The five stages have distinct geochemical properties, which suggest that the tectonic settings evolved from early, arc-related magma-genesis (Stage I) to within-plate magma-genesis (Stage V), with perhaps some intermediate phases of extensional environments. (C) 2011 Elsevier Ltd. All rights reserved.

The Serido Group of NE Brazil, a late Neoproterozoic pre- to syn-collisional basin in West Gondwana: insights from SHRIMP U-Pb detrital zircon ages and Sm-Nd crustal residence (T-DM) ages

The Serido Group is a deformed and metamorphosed metasedimentary sequence that overlies early Paleoproterozoic to Archean basement of the Rio Grande do Norte domain in the Borborema Province of NE Brazil. The age of the Serido Group has been disputed over the past two decades, with preferred sedimentation ages being either Paleoproterozoic or Neoproterozoic. Most samples of the Serido Formation, the upper part of the Serido Group, have Sm-Nd T-DM ages between 1200 and 1600 Ma. Most samples of the Jucurutu Formation, the lower part of the Serido Group, have T-DM ages ranging from 1500 to 1600 Ma; some basal units have T-DM ages as old as 2600 Ma, reflecting proximal basement. Thus, based on Sm-Nd data, most, if not all, of the Serido Group was deposited after 1600 Ma and upper parts must be younger than 1200 Ma.Cathodoluminescence photos of detrital zircons show very small to no overgrowths produced during ca. 600 Ma Brasiliano deformation and metamorphism, so that SHRIMP and isotope dilution U-Pb ages must represent crystallization ages of the detrital zircons. Zircons from meta-arkose near the base of the Jucurutu Formation yield two groups of ages: ca. 2200 Ma and ca. 1800 Ma. In contrast, zircons from a metasedimentary gneiss higher in the Jucurutu Formation yield much younger ages, with clusters at ca. 1000 Ma and ca. 650 Ma. Zircons from metasedimentary and metatuffaceous units in the Serido Formation also yield ages primarily between 1000 and 650 Ma, with clusters at 950-1000, 800, 750, and 650 Ma. Thus, most, if not all, of the Serido Group must be younger than 650 Ma. Because these units were deformed and metamorphosed in the ca. 600 Ma Brasiliano fold belt during assembly of West Gondwana, deposition probably occurred ca. 610-650 Ma, soon after crystallization of the youngest population of zircons and before or during the onset of Brasiliano deformation.The Serido Group was deposited upon Paleoproterozoic basement in a basin receiving detritus from a variety of sources. The Jucurutu Formation includes some basal volcanic rocks and initially received detritus from proximal 2.2-2.0 Ga (Transamazonian) to late Paleoproterozoic (1.8-1.7 Ga) basement. Provenance for the upper Jucurutu Formation and all of the Serido Formation was dominated by more distal and younger sources ranging in age from 1000 to 650 Ma. We suggest that the Serido basin may have developed as the result of late Neoproterozoic extension of a pre-existing continental basement, with formation of small marine basins that were largely floored by cratonic basement (subjacent oceanic crust has not yet been found). Immature sediment was initially derived from surrounding land; as the basin evolved much of the detritus probably came from highlands to the south (present coordinates). Alternatively, if the Patos shear zone is a major terrane boundary, the basin may have formed as an early collisional foredeep associated with south-dipping subduction. In any case, within 30 million years the region was compressed, deformed, and metamorphosed during final assembly of West Gondwana and formation of the Brasiliano-Pan African fold belts. (C) 2003 Elsevier B.V. All rights reserved.

U Pb and Sm Nd geochronologic studies of the eastern Borborema Province, Northeastern Brazil: initial conclusions

The Borborema Province of NE Brasil comprises the central part of a wide Pan-African-Brasiliano orogenetic belt that formed as a consequence of late Neoproterozoic convergence and collision of the São Luis-West Africa craton and the São Francisco-Congo-Kasai cratons. New Sm Nd and U Pb results from the eastern part of this province help to define the basic internal architecture and pre-collisional history of this province, with particular emphasis on delineating older cratonic terranes, their fragmentation during the Mesoproterozoic, and their assembly into West Gondwana during the Pan African-Brasiliano orogeny at ca. 600 Ma. The region can be divided into three major geotectonic domains: a) Rio Piranhas-Caldas Brandão massif, with overlying Paleoproterozoic to Neoproterozoic supracrustal rocks, north of the Patos Lineament; b) the Archean to Paleoproterozoic São Francisco craton (SFC) to the south; and c) a complex domain of Paleoproterozoic to Archean basement blocks with several intervening Mesoproterozoic to Neoproterozoic fold belts in the center (south of Patos Lineament and north of SFC). The northern and central domains comprise the Borborema Province. Archean basement gneiss and Transamazonian granulite of northern SFC are exposed in the southern part of the central domain, underlying southern parts of the Sergipano fold belt. Basement in the Rio Piranhas massif appears to consist mostly of Transamazonian (2.1 to 2.2 Ga) gneissic rocks; Nd model ages (TDM) of ca. 2.6 Ga for 2.15 Ga gneisses indicate a substantial Archean component in the protoliths to these gneisses. The Caldas Brandão massif to the east yields both Transamazonian and Archean U Pb zircon and Nd (TDM) ages, indicating a complex architecture. Metasedimentary rocks of the Jucurutu Formation yield detrital zircons with original crystallization ages as young as 1.8 Ga, indicating that these rocks may be late Paleoproterozoic and correlate with other ca. 1.8 Ga cratonic supracrustal rocks in Brazil such as the Roraima Group and Espinhaço Group. Most metavolcanic and pre-Brasiliano granitic units of the Sergipano (SDS), Pajeú-Paraíba (SPP), Riacho Pontal (SRP), and Piancó-Alto Brígida (SPAB) fold belts in the central domain formed ~ 1.0 ± 0.1 Ga, based on U Pb ages of zircons. Nd model ages (TDM) for these same rocks, as well as Brasiliano granites intruded into them and large parts of the Pernambuco-Alagoas massif, are commonly 1.3-1.7 Ga, indicating that rocks of the fold belts were not wholly derived from either older (> 2.1 Ga) or juvenile (ca. 1.0 Ga) crust, but include mixtures of both components. A simple interpretation of Brasiliano granite genesis and the Nd data implies that there is no Transamazonian or Archean basement underlying large parts of these fold belts or of the Pernambuco-Alagoas massif. An exception is a belt of syenitic Brasiliano plutons (Syenitoid Line) and host gneisses between SPAB and SPP that clearly has a Transamazonian (or older) source. In addition, there are several smaller blocks of Archean to Transamazonian gneiss that can be defined within and among these fold belts. These blocks do not appear to constitute a continuous basement complex, but appear to be isolated older crustal fragments. Our data support a model in which ca. 1.0 Ga rifting was an important tectonic and crust-forming event along the northern edge of the São Francisco craton. Our data also show that significant parts of the Borborema Province are not remobilized Transamazonian to Archean crust, but that Mesoproterozoic crust is a major feature of the Province. There are several small remnants of older crust within the area dominated by Mesoproterozoic crust, suggesting that the rifting event created several small continental fragments that were later incorporated into the Brasiliano collisional orogen. We cannot at present determine if the Rio Piranhas-Caldas Brandão massifs and the older crustal blocks of the central domain were originally part of the São Francisco craton or whether some (or all) of them came from more exotic parts of the Proterozoic Earth. Finally, our data have not yet revealed any juvenile terranes of either Transamazonian or Brasiliano age. © 1995.

New insights into Crustal Contributions to Large-volume Rhyolite Generation in the Mid-Tertiary Sierra Madre Occidental Province, Mexico, revealed by U Pb Geochronology

Voluminous (≥3·9 × 105 km3), prolonged (∼18 Myr) explosive silicic volcanism makes the mid-Tertiary Sierra Madre Occidental province of Mexico one of the largest intact silicic volcanic provinces known. Previous models have proposed an assimilation–fractional crystallization origin for the rhyolites involving closed-system fractional crystallization from crustally contaminated andesitic parental magmas, with <20% crustal contributions. The lack of isotopic variation among the lower crustal xenoliths inferred to represent the crustal contaminants and coeval Sierra Madre Occidental rhyolite and basaltic andesite to andesite volcanic rocks has constrained interpretations for larger crustal contributions. Here, we use zircon age populations as probes to assess crustal involvement in Sierra Madre Occidental silicic magmatism. Laser ablation-inductively coupled plasma-mass spectrometry analyses of zircons from rhyolitic ignimbrites from the northeastern and southwestern sectors of the province yield U–Pb ages that show significant age discrepancies of 1–4 Myr compared with previously determined K/Ar and 40Ar/39Ar ages from the same ignimbrites; the age differences are greater than the errors attributable to analytical uncertainty. Zircon xenocrysts with new overgrowths in the Late Eocene to earliest Oligocene rhyolite ignimbrites from the northeastern sector provide direct evidence for some involvement of Proterozoic crustal materials, and, potentially more importantly, the derivation of zircon from Mesozoic and Eocene age, isotopically primitive, subduction-related igneous basement. The youngest rhyolitic ignimbrites from the southwestern sector show even stronger evidence for inheritance in the age spectra, but lack old inherited zircon (i.e. Eocene or older). Instead, these Early Miocene ignimbrites are dominated by antecrystic zircons, representing >33 to ∼100% of the dated population; most antecrysts range in age between ∼20 and 32 Ma. A sub-population of the antecrystic zircons is chemically distinct in terms of their high U (>1000 ppm to 1·3 wt %) and heavy REE contents; these are not present in the Oligocene ignimbrites in the northeastern sector of the Sierra Madre Occidental. The combination of antecryst zircon U–Pb ages and chemistry suggests that much of the zircon in the youngest rhyolites was derived by remelting of partially molten to solidified igneous rocks formed during preceding phases of Sierra Madre Occidental volcanism. Strong Zr undersaturation, and estimations for very rapid dissolution rates of entrained zircons, preclude coeval mafic magmas being parental to the rhyolite magmas by a process of lower crustal assimilation followed by closed-system crystal fractionation as interpreted in previous studies of the Sierra Madre Occidental rhyolites. Mafic magmas were more probably important in providing a long-lived heat and material flux into the crust, resulting in the remelting and recycling of older crust and newly formed igneous materials related to Sierra Madre Occidental magmatism.