Quartz is the most abundant and most common mineral on the Earth. It is found in almost every geological environment and also it is at least a component of almost every rock type. It has a hexagonal crystal structure and is made of trigonal crystallized silica. It is most varied in terms of varieties, colours and forms. The most important distinction between the types of quartz is that one is of macro crystalline, which is individual crystal visible to the unaided eye, and the other is microcrystalline or cryptocrystalline varieties, aggregates of crystals visible only under high magnification. Chalcedony is the generic term for cryptocrystalline quartz. The transparent variety tends to be microcrystalline and the cryptocrystalline varieties are either translucent or mostly opaque.
This sedimentary rock which is composed primarily of Calcium Carbonate is integrally a multi-functional mineral used in industries for centuries. Limestone as one of the oldest minerals due to its very enduring geological evolution possesses different forms in nature and exhibits different colors. Its properties such as hardness, compactness, imperviousness, and durability have a significant role to play when it comes to its uses which are vast and versatile. This oldest component of ancient landmarks in the world is still practically an inseparable part of industries today. Middle East is amongst the top commodity traders of this mineral. And Arij is honored for having supplied the highest quality of Limestone and specifically the highest purity of 99% at a cost-effective price to different countries. This mineral has enormous diversity of industrial applications and what follows are some key uses of Limestone: Steel industry Construction Materials Refractory Sugar Refining Agriculture Paper manufacturing Glass Manufacturing Leather Tanning Pharmaceutics Food Industry
Aggregates are composed of geological materials such as gravel, sand and crushed rock. The size of the particles determines whether it is a coarse aggregate (e.g. gravel) or a fine aggregate (e.g. sand). The resulting concrete can be used in its natural state or crushed, according to its use and application
Marble is a metamorphic rock that forms when limestone is subjected to intense heat and pressure, causing it to recrystallize and develop a smooth, polished surface. Marble is prized for its beauty, durability, and versatility, making it a popular choice for a wide range of applications. Origin and Formation Marble is primarily composed of calcite, a mineral form of calcium carbonate. Limestone, which is also composed of calcite, is the precursor to marble. When limestone is buried deep underground, it is subjected to high temperatures and pressures. These conditions cause the limestone to recrystallize, forming marble. The intense heat and pressure also eliminate any impurities in the limestone, resulting in a pure, crystalline rock with a smooth, even texture. Types of Marble Marble comes in a wide range of colors, patterns, and textures, depending on the impurities present in the original limestone and the geological conditions during its formation. Some of the most common types of marble include: White Marble: White marble is the most popular type of marble, renowned for its elegant appearance and versatility. It is often used for countertops, flooring, wall cladding, and decorative applications. Carrara Marble: This highly prized white marble originates from quarries in the Carrara Mountains of Tuscany, Italy. It has been used for centuries for sculptures, monuments, and architectural elements due to its exceptional purity and beauty. Calacatta Marble: This type of marble is characterized by its dramatic veining, which often resembles flowing ribbons of darker shades against a white background. Calacatta marble is a popular choice for countertops, floors, and bathroom vanities. Pink Marble: Pink marble is often associated with luxury and elegance. It is derived from limestone deposits that have been enriched with iron oxides, giving it its characteristic pinkish hue. Pink marble is commonly used for countertops, flooring, and wall cladding. Green Marble: Green marble is created when limestone is infused with the mineral chlorite, resulting in a verdant appearance. It is often used for architectural elements, sculptures, and decorative applications.
Mugla white marble Late jurassic-cretaceous aged (mugla white÷ marble is lithologically defined as marble. It is a white colared, coarse grained, thick foliated and fractured rock and it forms upper parts of limestone sequence which is known as pasal¦dag formation. This rock unit has approximately 7 km length and 200-500 m width. It also contains local diasporite lenses through long distances. This rock unit is underlied by paleozoic basement rocks and overlied by early-middle triassic rock units by tectonic disconformity, Geological reserves : 1.000.000 m3 General properties Quarrying method And technology :step by step wire cutting, Yield of block : %20-80 Block dimensions (cm) : 250x150x150 v 300x170x180 Plate dimension (cm) : plates of 1-2-3 cm With cases, bundle inside the containers
Ganesh’s Garnet Abrasive Sand is one of the most superior products to come from superior garnet-bearing sands in North & East India. Through a unique geological history of erosion and deposition, these river sands contain the highest quality of garnet found anywhere around the world, available in various grade sizes. Garnet Sand has multiple industrial applications, such as sand blasting, for water jet cutting, in water filtration plants, as sandpaper for finishing bare wood and in the petrochemical industry. For water jet cutting, garnet extracted from hard rock is suitable since it is more angular in form, therefore more efficient in cutting.
Bentonite is a high swelling clay mineral whose name was derived from the location of the first commercial deposits mined at fort benton, wyoming u. S. A. Mineralogically, bentonite mainly consists of montmorillonite in combination with various mineral impurities such as feldspars, calcite, silica, etc. Montmorillonite belongs to the smectite group of clays which also include similar behaving minerals such as beidellite, saponite and hectorite. Geologically bentonites are mainly of volcanic origin, the majority of commercial deposits were formed by the hydrolysis or metamorphism of volcanic rock or ash and are almostly found in everywhere in world. The structure of montmorillonite is fundamentally a three layer structure with an octahedral aluminium hydroxyl sheet sandwiched between two layers of silicon- oxygen tetrahedra. However, the aluminium atoms are partially replaced by the substitution of either magnesium or iron atoms, thereby creating a charge deficiency within the unit structure. This results in a small negative charge on the basal plane of silica tetrahedra which is balanced by absorption of exchangeable cations between adjacent platelets. In natural montmorillonite, these cations are usually calcium, sodium or magnesium according to the formations of bentonite. Specification -welldry activated clay (montmorillonite clay, bentonite clay), 100% pure clay desiccant without any calcium chloride. In p.P. Woven bags of 25 kgs / 50kgs /1000 kgs net Kept in dry and ventilating place, prevent from rain and moisture when storage; if agglomerated, please crush and make it into solution, and its effect will be the same.
Product introduction Use 1. Coal body water injection, dust reduction, coal pressure reduction, coal splitting, gas discharge, etc. 2. Grouting, water injection and hole plugging of coal or rock mass. 3. It is used for curtain, consolidation, backfilling, chemical grouting and cement grouting of hydropower stations and reservoirs. 4. Water pressure test for geological exploration and water plugging for drilling.
