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.

Rheological behavior of binary aqueous solutions of poly(ethylene glycol) of 1500 g·mol-1 as affected by temperature and polymer concentration

The rheological behavior of poly(ethylene glycol) of 1500 g·mol -1(PEG1500) aqueous solutions with various polymer concentrations (w = 0.05, 0.10, 0.15, 0.20 and 0.25) was studied at different temperatures (T = 283.15, 288.15, 293.15, 298.15 and 303.15) K. The analyses were carried out considering shear rates ranging from (20 to 350) s-1, using a cone-and-plate rheometer under controlled stress and temperature. Classical rheological models (Newton, Bingham, Power Law, Casson, and Herschel-Bulkley) were tested. The Power Law model was shown suitable to mathematically represent the rheological behavior of these solutions. Well-adjusted empirical models were derived for consistency index variations in function of temperature (Arrhenius-type model; R2 > 0.96), polymer concentration (exponential model; R2 > 0.99) or the combination of both (R 2 > 0.99). Additionally, linear models were used to represent the variations of behavior index in the functions of temperature (R2 > 0.83) and concentration (R2 > 0.87). © 2013 American Chemical Society.

Density, Refractive Index, Apparent Specific Volume, and Electrical Conductivity of Aqueous Solutions of Poly(ethylene glycol) 1500 at Different Temperatures

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Rythmes de construction et de destruction des édifices volcaniques de point chaud : l'example des Iles Canaries (Espagne)= Ritmos de construcción y destrucción en islas volcánicas asociadas a puntos calientes : La Islas Canarias (España)

Tesis Universidad Paris 1 Panthéon - Sorbone (France) y Universidad de Las Palmas de Gran Canaria, 2002. Precede al título Laboratoire de Géographie Physique UMR 8591 CNRS Meudon

Evaluación del factor peso inferior a 1500 gramos al nacer como indicador de riesgo para la hipoacusia neurosensorial en el programa de cribaje universal de la hipoacusia infantil del Complejo Hospitalario Universitario Insular Materno Infantil de Gran Canaria durante el periodo 2007-2010

Programa de doctorado: Avances en Traumatología, Medicina del Deporte y Cuidados de Heridas.

La vision de l'Espagne de la preimère moitié du XIXe siècle dans la Géographie Universelle de Conrad Malte-Brun

[FR] Grande figure de la géographie française —et européenne— du premier quart du XIXe siècle, Conrad Malte-Brun laisse une oeuvre scientifique écrite considérable, dont une vaste Géographie universelle qui marqua alors son époque, rééditée à de multiples reprises durant plus de 50 ans. Contrairement à Élisée Reclus, autre grande figure de la seconde moitié du XIXe siècle, les écrits de Malte-Brun demeurent mal connus, sinon mésestimés. Or, à travers le fil conducteur que représente le chapitre de sa Géographie universelle consacré à l’Espagne, nous avons pour objectif de montrer que son auteur a su dépasser la simple dimension descriptive caractérisant nombre de textes géographiques de son époque pour introduire une réelle dimension explicative. Rien que pour cela, il mérite très largement, à notre sens, d’être redécouvert…

Recent changes in subsurface temperature and salinity in the Canary region

[EN]Based on hydrographic sections carried out during the last decade in the Canary region at 29° 10′N, we show that there has been a statistically significant rise in temperature and salinity on isobars between 1500 and 2300 db. The maximum increase, found at 1600 db, is occurring at a rate of 0.29°C and 0.047 per decade. Isobaric change decomposition into changes on neutral surfaces and changes due to the vertical displacement of the isoneutrals was performed. Results reveal that the lower part of North Atlantic Central Water (NACW) cooled and freshened on neutral surfaces, suggesting changes in the freshwater fluxes at the outcropping region. However, the signal in deep waters (1500–2300 db) was principally due to a downward displacement of the isoneutrals, although water mass modification is observed in the range of Mediterranean Water (MW) influence.

La institución parroquial a través de los registros contables del señorío episcopal de la Villa de Agüimes (1500-1860)

[ES]Con el trabajo de investigación que presentamos tratamos de abordar la organización y gestión administrativa de la institución parroquial a través del estudio y análisis de los libros contables, la normativa aplicada, correspondencia y demás documentos relacionados con la administración de la parroquia, con el objeto de poner de manifiesto su estructura organizativa, el método contable aplicado, los cambios organizativos y su incidencia en los registros contables.