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Ball Clay

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Feldspar Potash

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Mica

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Clay

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Calcite

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Dolomite

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Quartz

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Feldspar

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Eric Minerals (India) Pvt. Ltd is domestic market leader before its incorporation and now focusing to cater world market. We have been blessed to have a rich variety of Feldspar and Quartz mining in Rajasthan which have geologically unique deposits formed by varied genetic processes for centuries, rather millennia. Eric Minerals is playing significant role in sustenance of its populace and laid priority and trust in exploration and processing of fairly vast mineral wealth which has capacity to produce approx 25,000 MT per month and supplying to known ceramic industries of India specially in Gujarat. Eric’s mines are high in grade meta-morphogenic deposits and are endowed geologically and economically unique industrial minerals.Our company operates in compliance with law and acts with high ethical standards in action with integrity and honesty. With multiple existing minerals we continue to acquire mines in various parts of India. We have own processing plants, strong R&D and Quality control team aimed to maintain high quality standards from crude minerals to final product.+ Read More

Nature of Business

Manufacturer

Total Number of Employees

11 to 25 People

Legal Status of Firm

Public Limited Company

Annual Turnover

Rs. 25 - 50 Crore

Ball Clay
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Ball Clay

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StatePowdered, Crystal, Solid
Gradegrade a

Kaolin or China Clay is soft, earthy and usually white mineral (dioctahedral phyllosilicate clay), produced by the chemical weathering of aluminium silicate minerals like feldspar. We process china clay in white powder and also supply in lumps.

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Feldspar Potash
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Feldspar Potash

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StatePowdered, grains, Solid

Potassium feldspars are the feldspar minerals in which the silicate tetrahedral and aluminumtetrahedra are bound with potassium ions, rather than sodium or calcium ions as in the plagioclase feldspar subgroup. The potassium feldspar at Eric’s mines is composed of three mineral polymorphs, each having the same chemical composition, but slightly different crystal structures. Technically these are distinct minerals, but their physical properties are so similar that they are usually only identified as ‘potassium feldspar’ in the field.

Feldspars are an important component of most felsic igneous rocks, pegmatites, low temperature hydrothermal veins and many metamorphic rocks, especially those that formed from the alteration of shale or felsic igneous rocks. Their crystals are often particularly well developed in pegmatites, coarsely crystalline igneous rocks that form during late water-wet stages of a magma cooling.

Feldspars are used for glass, ceramics, tile flooring, pottery, clay, rubber, and a filler and extender in paint. Feldspars are also used for dating in archaeology and earth sciences.

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Mica
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Mica

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Mica is a silicate mineral and chemically contain silica (SiO4). Mica is stable when exposed to electricity, light, moisture, and extreme temperatures. Mica sheets are chemically inert, dielectric, insulating, lightweight, reflective, refractive, resilient, and transparent to opaque.

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Clay
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Clay

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Kaolin or China Clay is soft, earthy and usually white mineral (dioctahedral phyllosilicate clay), produced by the chemical weathering of aluminium silicate minerals like feldspar. We process china clay in white powder and also supply in lumps.

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Calcite
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Calcite

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Calcite is the only common non-silicate rock forming mineral, being instead calcium carbonate. It has two refractive indices causing a significant double refraction effect – when a clear calcite crystal is placed on an image, a double image is observed.

Calcite is one of the most ubiquitous minerals, being an important rock forming mineral in sedimentary environments. It is an essential component of limestone, and occurs in other sedimentary rocks. It also occurs in metamorphic and igneous rocks, and is common in hydrothermal environments. Calcite is a common vein filling mineral in many rock types Chemical Composition- CaCO 3 Hardness – 3, Specific Gravity – 2.7, Transparency – Transparent to translucent, Colour – Generally white or color less, but also with light shades, Streak – White, Lustre – Vitreous to resinous, Cleavage/fracture- Perform in three directions at oblique angles

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Dolomite
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Dolomite

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Dolomite formed as rocks are geographically extensive and hundreds to thousands of feet thick. Most rocks that are rich in dolomite were originally deposited as calcium carbonate muds that were postdepositionally altered by magnesium-rich pore water to form dolomite.

The rock containing 40-45% MgCO3 is usually called dolomite. Dolomite rock which contains in addition to dolomite either Calcite or a mixture of Calcite Magnesite are called “Dolomitic Limestone.

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Quartz
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Quartz

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At Eric’s mines quartz is found with a purity of 99.7%. It’snatural silica formed in geological environment and is at least a component of almost every rock type. It frequently is the primary mineral, >98%. It is also the most varied in terms of varieties, colors and forms. This variety comes about because of the abundance and widespread distribution. It’s composed of SiO 2 and polymorphs of silicon dioxide.

We manufacture Quartz powder as well in snow white colour which has 96% whiteness in Grade silica. Usually white colour, vitreous in luster, is insoluble in acids except hydrogen fluoride and is non combustive in nature and supplied specially customized as per industry’s desired specification.

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Feldspar
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Feldspar

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Potassium feldspars are the feldspar minerals in which the silicate tetrahedral and aluminumtetrahedra are bound with potassium ions, rather than sodium or calcium ions as in the plagioclase feldspar subgroup. The potassium feldspar at Eric’s mines is composed of three mineral polymorphs, each having the same chemical composition, but slightly different crystal structures. Technically these are distinct minerals, but their physical properties are so similar that they are usually only identified as ‘potassium feldspar’ in the field.

Feldspars are an important component of most felsic igneous rocks, pegmatites, low temperature hydrothermal veins and many metamorphic rocks, especially those that formed from the alteration of shale or felsic igneous rocks. Their crystals are often particularly well developed in pegmatites, coarsely crystalline igneous rocks that form during late water-wet stages of a magma cooling.

Feldspars are used for glass, ceramics, tile flooring, pottery, clay, rubber, and a filler and extender in paint. Feldspars are also used for dating in archaeology and earth sciences.

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