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A set of 12 samples of acid rock types Palmas (ATP) and Chapecó (ATC) was used to determine the chemical composition of plagioclase and pyroxene by electron microprobe, with the purpose to get information about the pressure and temperature of crystallization of these rocks. The results show that the pyroxene of ATP rocks (3,2 ± 1,2 kbar, max = 5,1 kbar and 1028 ± 38°C) were formed under pressure conditions higher than those ATC (1,8 ± 0,9 kbar, max = 3,4 kbar and 995 ± 26oC). However, the pressures obtained from plagioclase showed higher pressures for ATC (3.2 ± 1 kbar, max = 6,4 kbar and 1033 ± 12°C) than ATP (1,9 ± 1 kbar, max = 4,8 kbar and 1043 ± 5°C), suggesting that the crystallization of rocktype ATP began with the formation of pyroxene and plagioclase almost simultaneously at a depth of around 17 km while the ATC, began with the crystallization of plagioclase at a depth of about 21 km (assuming a gradient of 3,3 kbar/km). The geothermometry of plagioclase allow us to calculate the concentration of water from about 1 ± 0,3% H2O for both acid rock types. Additional calculations allow us to get the depth of water exsolution of magmatic liquid at 30m below the surface. Although the data are still preliminary and insufficient to model the extrusion of these rocks, they point out to an effusion mechanism of a partially fluidized magma by volatile, which would spread to large areas with small friction with the surface that would increased with the increase of viscosity caused by the loss of volatile and decreasing of temperature, developing coherent structures as lava flows.

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In assisted reproduction, the selection of gametes to achieve better clinical outcomes is a crucial task of embryologists. The quality of the oocyte is a key factor in female fertility, reflecting the intrinsic potential of gamete development, and has a vital role not only in conception but also in subsequent embryonic development. Oocyte dysmorphisms are classified into two types: cytoplasmic, including the presence of granules and/or cytoplasmic inclusions (vacuoles, refractive bodies, and aggregates of the endoplasmic reticulum), and extracytoplasmic (changes in the shape of the oocyte, the zona pellucida, the space perivitelline changes and the polar body). Variations in oocyte morphology may occur due to factors such as the age of women, genetic problems and changes in the hormonal environment to which the oocyte is exposed in ovarian hyperstimulation. The classification of oocyte morphology and its correlation with embryo development and pregnancy rates are controversial in the literature. Several studies show no association between oocyte dysmorphisms and the results of in vitro fertilization, while others report an association between oocyte morphology and embryo development. These differences in the results can be explained by the use of different morphological criteria due to a lack of standardization of oocyte evaluation. © Todos os direitos reservados a SBRA - Sociedade Brasileira de Reprodução Assistida.

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