In the Cheshmeh-Bid district of Khajeh-Jamali ophiolitic massifs (Southern Iran), mantle peridotites are intruded by abundant pyroxenite dykes. A few these dykes remarkable for occurrence native copper associated with development a metasomatic reaction zone. The progressively reacted, from their margins towards center, an amphibole + antigorite selvage, followed centimeter-thick clinopyroxene a...

This study, carried out in tailings from two sediment-hosted stratiform copper deposits the Lublin-Głogów Copper District Poland (Kupferschiefer-type deposit) and Zhezkazgan (cupriferous sandstone-type Kazakhstan, analysed mineralogy of copper, zinc, lead minerals as related to metal accumulation sediments. Microscopic study reflected light SEM–EDS (Scanning Electron Microscope—Energy Dispersiv...

The use of geometallurgical modelling is becoming common in the design a concentrator plant and during its operational phase. Predictive aims to define optimized process parameters for accommodate variability ore feed characteristics. main objective this study simulate metallurgical response distinct unit types their blends using kinetic models derived from experimental flotation tests. Kinetic...

Little is known about the production of ruby red copper stained glasses from Medieval and Renaissance periods apart fact that colour due to presence small metallic nanoparticles tin, most common reducing agent used in glass since 19th century, not present. In fact, very few workshops Europe were able make historical times, they kept it secret, so little how was obtained. These exported througho...

The Baranyevskoe Au-Ag epithermal deposit of low-sulfidation (LS) type is located on the Kamchatka Peninsula in Neogene-Quaternary Central Volcanic Belt, where Au-bearing quartz veins are usually accompanied by veinlet stockworks. Two economic associations typical deposit. first corresponds to gold-pyrite-quartz association with low-grade native gold (521–738‱) intergrown pyrite. Some accessory...

The purpose of this study is to determine geochemical anomalies on lithogeochemical data from Ardestan area, Central Iran, using concentration-number (C-N) fractal modeling and staged factor analysis. Staged factor analysis is used to the recognition of genetic correlation and elimination of non-indicator elements in three steps. Factor scores of elements were calculated and geochemical data cl...