Lead and zinc ores of Ukraine: resources, deposits, and prospects
Lead and zinc ores are an important source of lead and zinc, which are widely used in metallurgy, alloy production, and other industrial sectors. Ukraine possesses significant deposits of these ores, which have considerable economic importance. This section examines the characteristics, classification, and main directions of utilization of lead-zinc ores.
Lead and zinc ores is included in the list of minerals of national importance, approved by Resolution of the Cabinet of Ministers of Ukraine No. 827 of December 12, 1994, as non-ferrous metal ores.
List of minerals of national importance
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Go to the listPhysicochemical properties
Lead is a soft, malleable metal of bluish-gray color with a high density (11.34 g/cm³). Its melting point is 327.5°C, making it one of the most easily fusible heavy metals. It is easily machinable but has low electrical conductivity. In air, lead oxidizes, forming a protective film that prevents further oxidation. Under normal conditions, it does not react with hydrochloric or sulfuric acids, but it does react with nitric acid, hot alkalis, and oxidizing agents. Lead has a high capacity for absorbing ionizing radiation, which makes it valuable for radiation shielding.
Zinc is a silvery-white metal with a characteristic luster. Its density is 7.14 g/cm³, and its melting point is 419.5°C. Up to 100°C, zinc is ductile and easily deformed, but at higher temperatures it becomes brittle. It is a good conductor of electricity. In air, zinc forms a protective oxide film that prevents further oxidation. Zinc actively reacts with acids with the release of hydrogen, and also reacts with alkalis, ammonia and ammonium salts. Its chemical activity increases when heated. Zinc is an important trace element vital for many biological processes.
Lead and zinc minerals
Zinc occurs in the Earth’s crust at an average concentration of about 0.0083%. The principal mineral is sphalerite (ZnS), which is the main source of industrial zinc production. Other important minerals include smithsonite (ZnCO₃), hemimorphite (Zn₄Si₂O₇(OH)₂·H₂O), wurtzite, and zincite. These minerals form in both magmatic and sedimentary environments and often accompany lead, copper, and silver deposits. They occur as massive, vein-type, and disseminated accumulations in polymetallic deposits.
The average content of lead in the Earth’s crust is about 0.0016%. The most common lead minerals are galena (PbS), anglesite (PbSO₄), cerussite (PbCO₃), as well as pyromorphite, vanadinite, and mimetite. The main industrial reserves are associated with sulfide ores, where galena is the dominant mineral. Lead also occurs in sulfosalts, phosphates, silicates, and carbonates, often in association with zinc and silver in polymetallic ores.
Applications of lead and zinc
Lead products are of exceptional importance for many industrial sectors. The largest share of this metal is used in the production of batteries, where it serves as a key component of electrodes that ensure reliable energy storage and transfer. In the cable industry, lead is used to create durable insulation that protects wires from moisture and mechanical damage. Its chemical compounds are included in paints, plastic stabilizers, and fuel additives that improve engine performance.
In construction, lead is used as a material for radiation shielding, particularly in medical and nuclear facilities, as well as in the production of sheets and gaskets. Due to its softness and high density, it is also used in solders, antifriction alloys, and even ammunition, where it ensures accuracy and effectiveness.
Zinc, in turn, is equally important. Its unique ability to protect steel from corrosion makes it indispensable in the galvanization process, significantly extending the service life of metal structures in aggressive environments. In metallurgy, zinc serves as a base for producing technical alloys such as brass, bronze, and zinc-aluminum materials, which are widely used in engineering, automotive manufacturing, and household appliances.
In the chemical industry, zinc is essential for producing various compounds—from zinc oxide, used in rubber, paints, and creams, to zinc sulfate, which is applied in agriculture. In medicine, zinc is valued for its ability to support the immune system and accelerate healing, which is why it is included in tablets, ointments, and antiseptic products. Its role in electronics is also significant—as a material for electrodes in batteries and power sources, ensuring stable electrochemical processes.
Main Lead and Zinc Deposits in Ukraine
Dnieper–Donets Metallogenic Zone
This zone includes two types of deposits: vein-type polymetallic deposits in the Donetsk region (the most well-known are the Nagolchanske and Nagolno-Tarasivske deposits), as well as deposits associated with salt-dome structures in the northern part of the basin. Mineralization here is confined to salt uplifts, which create favorable conditions for the accumulation of polymetallic minerals.
Ukrainian Shield
Numerous occurrences of lead, zinc, and nickel ores are known within the Ukrainian Shield. Among them are the Devladivske, Chervone, Synelnykivske, and Prutivske deposits. Promising areas for further exploration include the Middle Dnieper gold-bearing region, the Azov area, the Kryvyi Rih basin in the Dnipropetrovsk region, and the Sugutano-Mayatska zone. Industrial development of these sites has not yet been undertaken due to insufficient geological exploration.
Southwestern Slope of the Voronezh Anteclise
In this zone, a number of lead-zinc ore occurrences have been identified, the most studied being the Markivske deposit. The mineralization is represented by sphalerite, galena, pyrite, and marcasite. Other known occurrences include the Aidar, Rivne, and Kharkiv manifestations, indicating significant potential for the discovery of new deposits in this area.
Carpathian Metallogenic Province
The main direction for the development of Ukraine’s lead and zinc resource base is associated with the deposits of Transcarpathia, including Berehivske, Muzhiivske, and Rakhivske.
The Carpathian metallogenic province covers the Transcarpathian inner trough, the folded Carpathians, and the Forecarpathian region. The most important area is the Berehove ore district, which includes:
- Berehivske deposit: a gold-polymetallic deposit located within tuffaceous rhyolite rocks. Reserves: 350 thousand tons of lead, 850 thousand tons of zinc. Content: Pb — 2.09%, Zn — 5.08%.
- Muzhiivske deposit: adjacent to Berehivske, with lead reserves of 780 thousand tons. Production capacity — up to 500 thousand tons of ore per year.
- Bihanske deposit: promising, part of the district.
- Rakhivske deposit: located in the folded Carpathians; development is complicated by mountainous terrain.
- Truskavetske deposit: located in the Forecarpathian trough; lead mineralization, historically mined since the 18th century.
Forecast resources of the district amount to 1,670 thousand tons of lead and 2,500 thousand tons of zinc.