https://ri.ufs.br/jspui/handle/riufs/955 Mon, 07 Sep 2026 04:07:40 GMT 2026-09-07T04:07:40Z https://ri.ufs.br/jspui/handle/riufs/25981 Título: Epidemiological aspects and spatial distribution of human and canine visceral leishmaniasis in an endemic area in northeastern Brazil Autor(es): Campos, Roseane; Santos, Márcio; Tunon, Gabriel; Cunha, Luana; Magalhães, Lucas; Moraes, Juliana; Ramalho, Danielle; Lima, Sanmy; Pacheco, José Antônio; Lipscomb, Michael; Jesus, Amélia Ribeiro de; Almeida, Roque Pacheco de Sun, 01 Jan 2017 00:00:00 GMT https://ri.ufs.br/jspui/handle/riufs/25981 2017-01-01T00:00:00Z https://ri.ufs.br/jspui/handle/riufs/25735 Título: Petrologia do Granito Chasqueiro, região de Arroio Grande, sudeste do Escudo Sul-Rio-Grandense Autor(es): Vieira, Daniel Triboli; Koester, Edinei; Bertotti, Anelise Losangela Abstract: Chasqueiro Granite comprises an 400 km2 N50ºEtrend elongated body located at the southernmost portion of the eastern Sul-Rio-Grandense Shield. It consists of monzo to syenogranite, light gray and leucocratic porphyritic texture with megacrystals K-feldspar in a coarse equigranular hypidiomorphic matrix, composed of quartz, K-feldspar, plagioclase, biotite, hornblende, opaque minerals and accessories. The modal megacrystals reach proportions between 30.0 and 60.0%, and range from 4 to 8 cm, with mafic minerals of the matrix showing a subvertical magmatic foliation and a tectonic foliation prominent in the borders marked by intense ductile deformation and protomylonite generation. Another important aspect of the Granite Chasqueiro is the obiquitous presence of microgranular mafic enclaves of dioritic composition in the granite, having different shapes and sizes. The Chasqueiro Granite is high-K calc alkaline, metaluminous to slightly peraluminous and characterized by a narrow SiO2 variation, with characteristic signature of granites generated in post-collisional tectonic setting. Geochronological analyzes obtained by the U-Pb method (LA-ICP-MS) and isotope geochemistry of Lu-Hf zircon data (LA-ICP-MS) presenting, respectively, crystallization age 574 ± 3 Ma and negative εHf, which suggest a granite relationship with deformational event D2 and supporting a magmatic crustal sources with subordinate mantle component. Tue, 01 Mar 2016 00:00:00 GMT https://ri.ufs.br/jspui/handle/riufs/25735 2016-03-01T00:00:00Z https://ri.ufs.br/jspui/handle/riufs/25118 Título: Predicting frequency distribution and influence of sociodemographic and behavioral risk factors of Schistosoma mansoni infection and analysis of co-infection with intestinal parasites Autor(es): Rollemberg, Carla Virginia Vieira; Silva, Marilia Matos Bezerra Lemos; Rollemberg, Karla C.; Amorim, Fábio Jorge Ramalho de; Lessa, Nayanna Mendes Neves; Santos, Marcos D. S.; Souza, Acacia Maria Barros; Melo, Enaldo Vieira de; Almeida, Roque Pacheco de; Silva, Angela Maria da; Werneck, Guilherme Loureiro; Santos, Mario Adriano dos; Almeida, José Antonio Pacheco de; Jesus, Amélia Maria Ribeiro de Thu, 01 Jan 2015 00:00:00 GMT https://ri.ufs.br/jspui/handle/riufs/25118 2015-01-01T00:00:00Z https://ri.ufs.br/jspui/handle/riufs/24398 Título: Mechanical properties of epoxy resin based on granite stone powder from the Sergipe fold-and-thrust belt composites Autor(es): Gonçalves, Jorge Antônio Vieira; Campos, Diego Adalberto Teles; Oliveira, Gislane de Jesus; Rosa, Maria de Lourdes da Silva; Macêdo, Marcelo Andrade Wed, 01 Jan 2014 00:00:00 GMT https://ri.ufs.br/jspui/handle/riufs/24398 2014-01-01T00:00:00Z