Designing a model for development of women sports with an emphasis on sports as a social phenomenon: What do we need?

Despite the development of sports in Iran, women's sports have not yet been able to achieve a desirable position. The development components and their necessary contexts and backgrounds must be identified to achieve the development of women sports. The aim of this study was to present a model for development of women's sports in Iran which was conducted through qualitative research method with the fundamental-exploratory nature. The data were collected by snowball sampling method based on deep interviews, which were coded and analysed according to grounded theory with a constructive approach. The results showed that the development of women's sports involves three components: environmental, structural, and behavioural. Furthermore, there was an intimate relationship between all the developmental contexts. Also, Peripheral components were identified as a large-scale context but structural components as facilitating contexts for development. The results also indicated to achieve women Sports development, suitable contexts are needed and the most important one is Cultural-Social context. Based on the results, necessary actions for the development of women's sport should be taken through the establishment of proper policies, determination of appropriate structures, and provision of favourable environments and contexts

Geothermometry obtained from the calcite twin and fluid inclusions in barite (Irankuh Pb-Zn deposit, Southwest of Isfahan)

The Irankuh mining district is located 20 km southwest of Isfahan and is geologically situated in Sanandaj - Sirjan zone and the lower Cretaceous sequence of Isfahan-Malayer ore mineralization area. The ore minerals are emplaced in the faulted contact of Jurassic shale and Cretaceous carbonates and include pyrite, galena, sphalerite, calcite, barite, dolomite, quartz as well as minor marcasite, smithsonite, cerussite, gypsum, malachite, hematite and goethite. The mineralization is mainly occurred as hydrothermal veins and veinlets associated with fractures and faults, suggesting the deposit is likely to be of epigenetic type. A comparison between geothermometric results obtained from calcite twins and fluid inclusions showed a similar temperature range for the mineralization (less than 170ºc). Fluid inclusion studies indicate the temperature, salinity and density ranges of 80-166ºc, 5.39-20.94 wt.% NaCl and 0.95-1.12, respectively. The obtained data share many similarities with those of the MVT deposit

Mineralization and geochemical studies in the Kalchouyeh occurrence, southwest of Naein

Kalchouyeh area in southwest of Naein is located in the Urumieh-Dokhtar volcano-plutonic belt. Mineralization occurred mainly as disseminations and veinlets hosted by trachy-andesite and pyroxene andesites. For mineralogy, alteration, fluid inclusion and geochemical studies, the two major mineralized zones: A (larger vein) from the north-northwest and B (smaller vein) from the east-southeast of the area were sampled. Alteration studies revealed that the main alteration assemblages are silicification and propylitic. The ore minerals are chalcopyrite, galena, pyrite, bornite, chalcocite, covellite, goethite, malachite, azurite, cerussite and cuprite with quartz, calcite and barite as the main gangues. Fluid inclusion studies demonstrated that salinity and homogenization temperatures were 0.38-4.23 and 0.166-9.188 wt% NaCl and 175-252°C and 250-324°C at the A and B veins, respectively. Rare Earth Element (REE) plots show negative slopes that is one of the features for calc-alkaline magmas. La/Y is higher than 1 showing that mineralizing fluids were neutral to basic. According to the data, direction of ore-bearing fluids movement was determined to be from east-southeast toward north-northwest (from B to A veins(, approximate site of mineralization center is located adjacent to smaller vein and the mineralization is epithermal in type

The effects of Urtica dioica hydroalcoholic extract on the propylthiouracil induced hypothyroidism in rat

Introduction: Hypothyroidism is an important endocrine disorder determined by some depressed symptoms. Urtica dioica (Urticaceae) is a medicinal plant which has been traditionally used for treatment of a wide range of decreased functions of different organs. In the current study, we aimed to evaluate the effect of hydroalcoholic extract of aerial parts of U. dioica on thyroid hormones in propylthiouracil (PTU)-induced hypothyroidism in rats. Methods: Forty-two male Wistar rats were randomly divided into 7 groups including control, PTU, different doses of Urtica dioica hydroalcoholic extract (UDHAE) treated and levothyroxine treated groups. The animals in various groups received water (control group) or water containing 0.1% W/V PTU and then injected saline (control group) or 25, 50, 100, 150 mg/kg UDHAE, respectively for 4 weeks. Positive control group was fed levothyroxine 0.5 mg/kg during the PTU treatment. Then, the blood samples were collected and the levels of thyroxine (T4), triiodothyronine (T3), free triiodothyronine (FT3) and thyroid-stimulating hormone (TSH) measured via the Elisa method. Results: The data showed that PTU decreased the blood level of thyroid hormones but increased TSH, significantly. The 50 or 100 mg/kg doses of UDHAE remarkably increased the blood level of T3 and FT3. The 50 mg/kg doses of UDHAE increased the blood level of T4. None of the UDHAE doses showed significant change in the TSH levels. 25 and 150 mg/kg doses of UDHAE did not change the PTU- diminished level of thyroid related hormones. Conclusion: The findings suggest that 50 mg/kg dose of UDHAE has stimulatory effect on thyroid gland function and raises plasma T3 & T4 & FT3 levels. UDHAE at the dose of 50 or 100 mg/kg could enhance blood level of T3 and FT3 perhaps by increase in T4 to T3 transformation. Higher doses of UDHAE could not increase the level of these hormones probably due to the presence of inhibitory materials