Mineralogia e química dos sedimentos de fundo do médio e baixo Madeira e de seus principais tributários: Amazonas - Brasil

O objetivo deste trabalho foi investigar a variação composicional e mineralógica dos sedimentos de fundo transportados pelos grandes rios da Amazônia, com nascentes nos Andes provenientes de rochas cratônicas. O estudo foi realizado com base em análises granulométricas, mineralógicas e químicas, incluindo isótopos de Pb, no rio Madeira e seus tributários. O conjunto de dados mostra que os sedimentos de fundo do rio Madeira são granulométrica, mineralógica e quimicamente distintos de seus principais tributários. Os sedimentos do rio Madeira são mais arenosos; têm maior quantidade de quartzo; menor conteúdo de Al2O3, Fe2O3, K2O, MgO, Na2O, PF, TiO2, P2O5, MnO e elementos-traço; e a maturidade aumenta de montante para jusante. Dentre os sedimentos dos tributários, os rios Machado e secundariamente o rio Marmelos são os que mais se aproximam da composição dos sedimentos do rio Madeira, enquanto que o Jamari com sedimentos com maior proporção de TiO2, Zr, Y, Nb, Ga, Hf, U, Ta e ETR, é o mais distinto. Apesar do ambiente de intenso intemperismo e erosão, em condições tropicais úmidas, a que estão submetidas as rochas drenadas pela bacia do rio Madeira, os valores das razões Th/Co, Th/Pb, Th/Yb, Al/Pb, Zr/Co e a composição isotópica de Pb indicam fontes distintas para os sedimentos de fundo estudados. Os sedimentos do rio Madeira são provenientes, principalmente, de rochas máficas, enquanto que os sedimentos de seus tributários têm como fonte essencialmente rochas félsicas.

Efecte de l'estrès estructual sobre l'emissió estimulada (laseig) en capes epitaxials de KY0.8Yb0.2(WO4)2 i KLu0.8Yb0.2(WO4)2 crescudes sobre substractes de KY(WO4)2 i KLu(WO4)2

Projecte de recerca elaborat a partir d’una estada a la State University of New York a Stony Brook, EEUU, a l’agost i setembre del 2008. S’ha demostrat com està relacionada la diferència en el rendiment de lasejat de dos mostres altament dopades amb iterbi (20 at. %) de capes epitaxials de KY(WO4)2 (KYW) dopat amb Yb crescut sobre un substrat de KYW i de KLu(WO4)2 (KLuW) dopat amb Yb crescut sobre un substrat de KLuW, respectivament, amb la presència de estrès estructural en les capes epitaxials, investigat per Topografia de Feix Blanc de Raig X de Sincrotró. A partir dels resultats obtinguts, queda clar que les mostres que mostren una quantitat d'estrés estructural més gran, les epitaxies de KYW dopat amb Yb crescudes sobre substrats de KYW, duen a una eficiència més petita durant el lasejat, permetent establir una correlació directa entre l'existència i la magnitud d'aquest estrès estructural i la pèrdua del rendiment làser en aquestes capes epitaxial, que per altra banda, des del punt de vista espectroscòpic són equivalents.

Detection and Characterization of Rotavirus G and P Types from Children Participating in a Rotavirus Vaccine Trial in Belém, Brazil

This study sought the characterization of rotaviruses in a trial with a tetravalent rhesus-human rotavirus vaccine in Belém, Brazil in children who received three doses of vaccine or placebo in the 1st, 3rd and 5th months of life. Rotavirus electropherotypes, subgroups, G serotypes, G, [P] and [P],G genotypes were determined in 93.3%, 95.9%, 93.3%, 73.3%, 95.5% and 92.2% of isolates, respectively. Serotypes G1, G2 and G4 were detected in 58.9%, 30% and 4.4% of the cases, respectively. Rotavirus genotype G5 was detected for the first time in Northern region in 4.4% of the infections. Rotavirus genotypes P[8], P[4], P[6] and P[8+6] were detected in 54.5%, 26.7%, 12.2%, and 2.2% of the cases, respectively. The predominant genotypes were P[8],G1 and P[4],G2 with 53% and 26.6% of the infections, respectively. Unusual strains accounted for 20.5% including P[4],G1, P[6],G1, P[6],G4, P[6],G5, P[8],G2, P[8],G5. Mixed infections involving P[8+6],G2 and P[8+6],G1 were also noted. The neonatal P[6] strains associated with diarrhea were detected among children aged 9-24 months. To our knowledge, this study represents the first in Brazil to analyse, on molecular basis, rotavirus genotypes from children participating in a rotavirus vaccine trial. These results are of potential importance regarding future rotavirus vaccination strategies in Brazil.

Insights into shallow magmatic processes in large silicic magma bodies: the trace element record in the Fish Canyon magma body, Colorado

Highly evolved rhyolite glass plus near-solidus mineral assemblages in voluminous, dacitic, crystal-rich ignimbrites provide an opportunity to evaluate the late magmatic evolution of granodiorite batholiths. This study reports laser-ablation ICP-MS analyses of trace element concentrations in feldspars, hornblende, biotite, titanite, zircon, magnetite, and interstitial glass of the crystal-rich Fish Canyon Tuff. The high-silica rhyolite glass is characterized by relatively high concentrations of feldspar-compatible elements (e.g., 100 ppm Sr and 500 ppm Ba) and low concentrations of Y (< 7 ppm) and HREE (&SIM; 1 ppm Yb), hence high LREE/HREE (Ce/Yb > 40) compared to many well-studied high-silica rhyolite glasses and whole-rock compositions. Most minerals record some trace element heterogeneities, with, in particular, one large hornblende phenocryst showing four- to six-fold core-to-rim increases in Sr and Ba coupled with a decrease in Sc. The depletions of Y and HREE in the Fish Canyon glass relative to the whole-rock composition (concentrations in glass &SIM; 30% of those in whole rocks) reflect late crystallization of phases wherein these elements were compatible. As garnet is not stable at the low-P conditions at which the Fish Canyon magma crystallized, we show that a combination of modally abundant hornblende (&SIM; 4%) + titanite (&SIM; 0.5-1%) and the highly polymerized nature of the rhyolitic liquid led to Y and HREE depletions in melt. Relatively high Sr and Ba contents in glass and rimward Sr and Ba increases in euhedral, concentrically zoned hornblende suggest partial feldspar dissolution and a late release of these elements to the melt as hornblende was crystallizing, in agreement with textural evidence for feldspar (and quartz) resorption. Both observations are consistent with thermal rejuvenation of the magma body prior to eruption, during which the proportion of melt increased via feldspar and quartz dissolution, even as hydrous and accessory phases were crystallizing. Sr/Y in Fish Canyon glass (13-18) is lower than the typical ``adakitic'' value (> 40), confirming that high Sr/Y is a reliable indicator of high-pressure magma generation and/or differentiation wherein garnet is implicated.

Estudi de les addicions de Michael i aza-Michael. I, Catalitzades per lantànids. II, Catalitzades per un nou organocatalitzador suportat en nanopartícules d'or

Aquesta memòria es centra en un gran tema de la química orgànica que és la catàlisi asimètrica de les addicions de Michael. Més concretament, en aquest treball s’estudia la enantioselectivitat que proporcionen dos lligand en qüestió, un d’ells basat en metalls i l’altre organocatalític, en unes reaccions de Michael. Així doncs, s’estudiaren dos tipus de sistemes. El primer cas és l’addició de Michael entre 2-tert-butoxicarbonil-1-indanona i tres acceptors de Michael diferents com són la metilvinilcetona, el Nacriloïloxazolidinona i l’azodicarboxilat de di-tert-butil, catalitzat per combinacions de metalls lantànids (majoritariament Yb) amb lligands quirals de tipus pybox. La segona part de la memòria es centra en l’estudi d’enantioinducció que proporciona un nou organocatalitzador en les addicions de Michael esmentades en l’apartat anterior. Aquest catalitzador està format pel derivat de la cincona 11-(9-mercaptononiltio)-10,11-dihidrocinconina suportat en nanopartícules d’or.

The variability of peridotite composition across a mantle shear zone (Lanzo massif, Italy): interplay of melt focusing and deformation

In this paper we present new data on the spatial variability of peridotite composition across a kilometer-scale mantle shear zone within the Lanzo massif (Western Alps, Italy). The shear zone separates the central from the northern part of the massif. Plagioclase peridotite shows gradually increasing deformation towards the shear zone, from porphyroclastic to mylonitic textures in the central body, while the northern body is composed of porphyroclastic rocks. The peridotite displays a large range of compositions, from fertile peridotite to refractory harzburgite and dunite. Deformed peridotites (proto-mylonite and mylonites) tend to be compositionally more homogeneous and fertile than weakly deformed peridotites. The composition of most plagioclase peridotites show rather high and constant (Ce/Yb) (N) ratios, and Yb (N) that cannot be explained by any simple melting model. Instead, refertilization modeling, consisting of melt increments from spinel peridotite sources, particularly with E-MORB melt, reasonably reproduces the plagioclase peridotite whole rock composition. Combined with constraints from Ce-Nb and Ce-Th systematics, we speculate that peridotites such as those from Lanzo record pervasive refertilization processes in the thermal boundary layer. In this scenario, mantle shear zones might act as important areas of melt focusing in the upper mantle that separates the thermal boundary layer from the conductively cooled mantle.

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@ . Euripidis tragoediae septendecim ex quibus quaedam habent commentaria ; et sunt hae : ecuba, Orestes Phoenisse Medea, Hippolytus, Alcestis, Andromache. Supplices, Iphigenia im Aulide. Iphigenia in Tauris, Rhesus, Troades, Bacchae, Cyclops, Heraclidae, Helena, Ion

Numérisation partielle de reliure

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