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Maxworth Minerals is a designated import and export company that offers customers unmatched expertise in all facets of procurement and supply, and a complete end-to-end supply chain solution. We are also the leading producers, processors and exporters of heavy metals and minerals.

At present, Maxworth Minerals has established facilities specializing in minerals such as Garnet, Sillimanite and Ilmenite. A thorough understanding of customer's requirements coupled with a deep emphasis on professionalism and quality control has propelled us to the top niche in this industry in a very short span of time. Our wide supply network and smoothly integrated supply lines have proven an added advantage to help us establish a good distribution network in the country.

Garnet

Garnet Abrasive

Garnet is a semi-precious stone derived from mined Almandite and Andradite deposits. After extraction, it is processed and screened to the grade desired. Its high density and unique physical properties make garnet nature's most efficient, effective and safe abrasive.

Sillimanite

Sillimanite

Sillimanite is a type of aluminium silicate that is polymorphic to both andalusite and kyanite. It is used as a raw material for high alumina refractories, which are extensively used in the Iron and Steel, Petrochemicals, Electrical, Cement, Zinc and Glass Industries.

Ilmenite

Ilmenite

Ilmenite is mostly used in the paints, fabrics, plastics, paper, sunscreen, food and cosmetics industries (as a source of titanium dioxide) . It is used in the steel industry to line blast furnaces, and is also very useful as an abrasive.

PS Balls

PS Balls

PS Ball is an abrasive that is produced by super- cooling molten steel slag. It is suitable for a wide range of applications, and its most common usage is as an abrasive for the surface preparation of steel prior to the application of paint coatings.

Granite

Granite

Granite is a common type of felsic intrusive igneous rock formed of interlocking crystals of quartz, feldspar, mica, and other minerals in lesser quantities. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy. which makes up 70-80% of Earth's crust Large masses of granite are a major ingredient of mountain ranges.

Fly Ash

Fly Ash

Fly ash is a coal combustion product that is composed of the particulates (fine particles of fuel) that are driven out of coal-fired boilers together with the flue gases. Ash that falls to the bottom of the boiler is called bottom ash. In modern coal-fired power plants, fly ash is generally captured by electrostatic precipitators or other particle filtration equipment before the flue gases reach the chimneys.

Olivine

Olivine

Olivine is one of the most common minerals in the earth, and is a major rock forming mineral. Despite this, good specimens and large crystals are uncommon and sought after. Only few localities yield large examples of this mineral, although small and microscopic grains are found worldwide. Olivine is also found in meteorites, and large grains have been reported in many of them.

Micro Silica

Micro Silica (MS)

Micro Silica is a very fine Pozzolanic Material composed of Amorphous Silica. It is a by product in the process of manufacturing of Silicon and Ferro Silicon alloys. It can also be produced by densification of burnt Rice Husk. Micro Silica (MS) has proven to be an excellent admixture for Portland cement concrete.

Barite

Barite

Barite is a mineral composed of barium sulfate, BaSO4. It is usually colorless or milky white, but can be almost any color, depending on the impurities trapped in the crystals during their formation. Barite is relatively soft, measuring 3-3.5 on Moh's scale of hardness. It is unusually heavy for a non-metallic mineral.

Bentonite

Bentonite

Bentonite is a very widely distributed clay material that is the result of the devitrification and chemical alteration of glassy volcanic ash or tuff. Bentonite should be used as the name of a rock derived from volcanic glass and it is commonly composed of the mineral montmorillonite but less often of beidellite.

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