Nepheline. Properties, genesis and use
Nepheline is a mineral of the class of aluminosilicates and a valuable industrial raw material of great importance.
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Nepheline is a mineral of the class of aluminosilicates and a valuable industrial raw material of great importance.
Bischofite is a natural mineral-chloride rich in magnesium, which is formed during the evaporation of salt pools.
Corundum is a superhard aluminum oxide formed in metamorphic and magmatic conditions and has a characteristic glassy shine.
Molybdenum is widely used in metallurgy for alloying ultra-strong steels for demanding applications.
Vanadium — is a strategic metal with wide applications in the steel, aviation, energy and chemical industries.
Lithium ores — is a source of strategic metal used for batteries, metallurgy and ceramics.
Beryllium ores are a valuable source of a lightweight and strong metal used in the aerospace, electronics, and defense industries.
Uranium ores are natural mineral formations containing uranium at concentrations suitable for industrial extraction.
Rubidium and cesium are rare alkali metals that occur mainly in rare-metal pegmatites and salt deposits.
Iodine and bromine are halogens of significant industrial importance, and in Ukraine they are concentrated in mineral waters.
Marshallite consists of tiny quartz crystals that may seem insignificant, but they have great practical and scientific importance.
Iceland spar is a unique variety of calcite capable of splitting a light beam into two rays.
Talc is an extremely soft, layered silicate that forms during the metamorphism of ultramafic rocks and can be easily ground into a powder.
Shungite — is a carbon-containing metamorphic rock enriched with amorphous carbon and known for its sorption properties.
Phlogopite is a mineral from the mica group known for its fire resistance, thermal insulation properties and decorative appeal.
Andesite — is an volcanic or subvolcanic rock of porphyry structure consisting mainly of medium plagioclase.
Anorthosite is an igneous rock of the gabbro group, which lies in massifs and is characterized by almost complete dominance of plagioclase.
Forming in deep conditions, diorite acquires a coarse-grained structure and decorative properties.
Gabbro is an intrusive igneous rock of the main composition, which forms significant massifs and is widely used as a valuable raw material.
Feldspars — are a group of aluminosilicate minerals that are the most common rock-forming components of the earth’s crust.