La chloritisation supergène zincifère des phlogopites de Canoas (PR, Brésil)

Dans l'altération superficielle de la mine de Pb-Zn-Ba de Canoas, les chlorites apparaissent en pseudomorphose des phlogopites avec un faciès et une composition tout à fait particuliers et sont très fortement zincifères (de 15 à 20% ZnO). Cette chlorite se substitue aux phlogopites du gisement. La chloritisation supergène est transitoire, avec une altération de la chlorite en smithsonite. La chlorite zincifère, (Zn3,48Mg5,11Fe3,71Al0,48Ti0,08)(Si5,67Al2,33)O26(OH)16, est de genèse et de compostion différentes de celles de la baileychlore. (Résumé d'auteur

Jarosita e plumbojarosita nos gossans do distrito mineiro de Canoas (PR)

Jarosites and plumbojarosites in gossans related to Pb-Zn mineralization in the Canoas District are described. They are always associated with goethite and in minor extent with hematite. Some crystals show zoning with a core of jarosite and a rim of plumjarosite. Others are rather homogeneous with intermediate composition. In the general formula AB3(SO4)2(OH)6, A sites are occupied by K and Pb and B sites by Fe, Al and Zn. A and B sites are often incompletely filled. A sites generally show excess of charge. B sites show deficiency. Jarosites and plumbojarosites are secondary minerals formed by sulfur, iron and lead derived from the weathering of sulphides, and potassium from the gangue mineral orthoclase. The jarosite-goethite association in gossans percolated by meteoric waters is thermodynamically unstable. It persists due to the sluggishness of the transformation of the jarosite into goethite. Thus, the Canoas jarosites are transitory Pb bearing phases. In the mature gossans Pb is associated only with the oxyhydroxides. (Résumé d'auteur

The lateritic ore deposits of Brazil

Au Brésil, les mécanismes d'altération supergène ont conduit à la formation d'un épais recouvrement latéritique sur environ 65 % de la surface totale; dans des conditions particulières, l'accumulation de certains métaux dans ce manteau peut atteindre le stade économique. La latéritisation des diverses roches mères, tout à fait spécifiques de chaque type de gisement, est intervenue pour l'essentiel au Tertiaire, pendant des épisodes de stabilité tectonique auxquels correspondent des surfaces d'aplanissement généralisées. Le rôle des facteurs lithologiques, climatiques et morpho-tectoniques dans le mécanisme de genèse des gisements latéritiques est discut

Transitions of cardio-metabolic risk factors in the Americas between 1980 and 2014

Describing the prevalence and trends of cardiometabolic risk factors that are associated with non-communicable diseases (NCDs) is crucial for monitoring progress, planning prevention, and providing evidence to support policy efforts. We aimed to analyse the transition in body-mass index (BMI), obesity, blood pressure, raised blood pressure, and diabetes in the Americas, between 1980 and 2014

Combination of searches for heavy spin-1 resonances using 139 fb−1 of proton-proton collision data at √s = 13 TeV with the ATLAS detector

A combination of searches for new heavy spin-1 resonances decaying into diferent pairings of W, Z, or Higgs bosons, as well as directly into leptons or quarks, is presented. The data sample used corresponds to 139 fb−1 of proton-proton collisions at √s = 13 TeV collected during 2015–2018 with the ATLAS detector at the CERN Large Hadron Collider. Analyses selecting quark pairs (qq, bb, tt¯, and tb) or third-generation leptons (τν and τ τ ) are included in this kind of combination for the frst time. A simplifed model predicting a spin-1 heavy vector-boson triplet is used. Cross-section limits are set at the 95% confdence level and are compared with predictions for the benchmark model. These limits are also expressed in terms of constraints on couplings of the heavy vector-boson triplet to quarks, leptons, and the Higgs boson. The complementarity of the various analyses increases the sensitivity to new physics, and the resulting constraints are stronger than those from any individual analysis considered. The data exclude a heavy vector-boson triplet with mass below 5.8 TeV in a weakly coupled scenario, below 4.4 TeV in a strongly coupled scenario, and up to 1.5 TeV in the case of production via vector-boson fusion

Search for non-resonant Higgs boson pair production in final states with leptons, taus, and photons in pp collisions at √s = 13 TeV with the ATLAS detector

A search is presented for non-resonant Higgs boson pair production, targeting the bbZZ, 4V (V = W or Z), V V τ τ , 4τ , γγV V and γγτ τ decay channels. Events are categorised based on the multiplicity of light charged leptons (electrons or muons), hadronically decaying tau leptons, and photons. The search is based on a data sample of proton-proton collisions at √s = 13 TeV recorded with the ATLAS detector during Run 2 of the Large Hadron Collider, corresponding to an integrated luminosity of 140 fb−1. No evidence of the signal is found and the observed (expected) upper limit on the cross-section for non-resonant Higgs boson pair production is determined to be 17 (11) times the Standard Model predicted cross-section at 95% confidence level under the background-only hypothesis. The observed (expected) constraints on the HHH coupling modifier, κλ, are determined to be −6.2 < κλ < 11.6 (−4.5 < κλ < 9.6) at 95% confidence level, assuming the Standard Model for the expected limits and that new physics would only affect κλ

Searches for exclusive Higgs boson decays into D⁎γ and Z boson decays into D0γ and Ks0γ in pp collisions at √s = 13 TeV with the ATLAS detector

Searches for exclusive decays of the Higgs boson into D⁎γ and of the Z boson into D0γ and Ks0γ can probe flavour-violating Higgs boson and Z boson couplings to light quarks. Searches for these decays are performed with a pp collision data sample corresponding to an integrated luminosity of 136.3 fb−1 collected at s=13TeV between 2016–2018 with the ATLAS detector at the CERN Large Hadron Collider. In the D⁎γ and D0γ channels, the observed (expected) 95% confidence-level upper limits on the respective branching fractions are B(H→D⁎γ)&lt;1.0(1.2)×10−3, B(Z→D0γ)&lt;4.0(3.4)×10−6, while the corresponding results in the Ks0γ channel are B(Z→Ks0γ)&lt;3.1(3.0)×10−6