Narrativas de violências praticadas por parceiros íntimos contra mulheres

Foi realizada uma pesquisa com mulheres de 15 a 49 anos moradoras de uma área de vulnerabilidade social da capital brasileira para conhecer os discursos femininos sobre suas vivências de violências praticadas por parceiros íntimos. Foi utilizada uma abordagem qualitativa e técnica do Discurso do Sujeito Coletivo. Durante entrevistas realizadas em seus domicílios no período de fevereiro a julho de 2007, 195 mulheres narraram, episódios de violências sofridas ao longo da vida. As entrevistas geraram 32 Discursos do Sujeito Coletivo que foram construídos a partir de 395 expressões-chaves agrupadas em sete blocos temáticos: i) Engenharia das VPI (N = 114; 58,5%); ii) Histórias de estupro de vulneráveis (N = 77; 39,5%); iii) Violências silenciosas ou silenciadas (N = 43; 22%); iv) Anos potenciais de vida sofrida (N = 43; 22%); v) Um novo tempo, apesar dos pesares (N = 39; 20%); vi) E por falar em violências (N = 35; 18%); vii) A violência é uma linguagem (N = 34; 17,4%). Três discursos do bloco de maior prevalência, intitulado "A engenharia das VPI", são apresentados integralmente neste trabalho. As narrativas das violências reveladas mostram a intensidade da vulnerabilidade e das agressões sofridas pelas mulheres e a existência de múltiplas dinâmicas violentas nos relacionamentos íntimo-afetivos.

Present bounds on new neutral vector resonances from electroweak gauge boson pair production at the LHC

Several extensions of the standard model predict the existence of new neutral spin-1 resonances associated with the electroweak symmetry breaking sector. Using the data from ATLAS (with integrated luminosity of L = 1.02 fb(-1)) and CMS (with integrated luminosity of L = 1.55 fb(-1)) on the production of W+W- pairs through the process pp --> l(+)l(-)' is not an element of(T), we place model independent bounds on these new vector resonances masses, couplings, and widths. Our analyses show that the present data exclude new neutral vector resonances with masses up to 1-2.3 TeV depending on their couplings and widths. We also demonstrate how to extend our analysis framework to different models with a specific example.

Constraining anomalous Higgs boson interactions

The recently announced Higgs boson discovery marks the dawn of the direct probing of the electroweak symmetry breaking sector. Sorting out the dynamics responsible for electroweak symmetry breaking now requires probing the Higgs boson interactions and searching for additional states connected to this sector. In this work, we analyze the constraints on Higgs boson couplings to the standard model gauge bosons using the available data from Tevatron and LHC. We work in a model-independent framework expressing the departure of the Higgs boson couplings to gauge bosons by dimension-six operators. This allows for independent modifications of its couplings to gluons, photons, and weak gauge bosons while still preserving the Standard Model (SM) gauge invariance. Our results indicate that best overall agreement with data is obtained if the cross section of Higgs boson production via gluon fusion is suppressed with respect to its SM value and the Higgs boson branching ratio into two photons is enhanced, while keeping the production and decays associated to couplings to weak gauge bosons close to their SM prediction.

Using AMS combined with mineral shape preferred orientation analysis to understand the emplacement fabrics of the Apiai gabbro-norite (Ribeira Belt, SE Brazil)

The Apiai gabbro-norite is a massive fine-grained Neoproterozoic intrusion emplaced in a core of synformal structure that deforms low-grade marine metasedimentary rocks of the Ribeira Belt of south-eastern Brazil. The lack of visible magmatic layering or any internal fabric has been a major limitation in deciding whether the emplacement occurred before or after the regional folding. To assist in the tectonic interpretations, we combine low-field anisotropy of magnetic susceptibility (AMS) and silicate shape preferred orientation (SPO) to reveal the internal structure of the mafic intrusion. Magnetic data indicate a mean susceptibility of about 10(-2) SI and a mean anisotropy degree (P) of about 1.08, essentially yielded by titanomagnetite. The magnetic and silicate foliations for P >= 1.10 are parallel to each other, while the lineations tend to scatter on the foliation plane, in agreement with the dominant oblate symmetry of the AMS and SPO ellipsoids. For lower P values, the magnetic and silicate fabrics vary from coaxial to oblique, and for P <= 1.05, their shapes and orientations can be quite distinct. The crystal size distribution (CSD) of plagioclase for P > 1.05 is log linear, in agreement with a bulk simple crystallisation history. These results combined show that for a strong SPO, corresponding to a magnetic anisotropy above 1.10, AMS is a reliable indicator of the magmatic fabric. They indicate that the Apiai gabbro-norite consists of sill-like body that was inclined gently to the north by the regional folding.