Fluorspar, also known as fluorite, is a mineral composed of calcium fluoride (CaF2). It is a widely occurring mineral that is found in various types of rock formations. Fluorspar has a wide range of uses, including in the production of aluminum, steel, hydrofluoric acid, and as a flux in the production of glass, ceramics, and enamels. It is also used as a source of fluorine in the pharmaceutical and chemical industries, and as a gemstone. Fluorspar is known for its unique fluorescence, which is caused by the presence of certain impurities in the mineral. Following the extraction of fluorspar from mines located in Pakistan, our highly skilled team diligently assesses and classifies the fluorspar before initiating the processing stage for our valued customers. Our fluorspar products encompass a broad spectrum of grades, ranging from 30% to 96%, catering to the requirements of the acid, cement, and steel industries. Additionally, we offer fluorspar in various size specifications, including 0-10mm, 3-10mm, and 10-80mm, which are already being successfully distributed to diverse markets, including China, Turkey, Korea, Japan, and Europe. With a substantial monthly production capacity of 10,000 tons, we stand as a dependable and robust source for meeting industrial demands. In parallel to our expertise in fluorspar extraction and processing, Bare Syndicate boasts extensive proficiency in logistics and international trade. This comprehensive skill set enables us to provide our customers with a seamless, all-inclusive solution for their supply management needs
Syrian Rock Phosphate
Fine gypsum stone - ready for export worldwide.
Talc, common silicate mineral that is distinguished from almost all other minerals by its extreme softness (it has the lowest rating on the Mohs scale of hardness). Its soapy or greasy feel accounts for the namesoapstone given to compact aggregates of talc and other rock-forming minerals. Dense aggregates of high-purity talc are called steatite. Since ancient times, soapstones have been employed for carvings, ornaments, and utensils; Assyrian cylinder seals, Egyptian scarabs, and Chinese statuary are notable examples. Soapstones are resistant to most reagents and to moderate heat; thus, they are especially suitable for sinks and countertops. Talc is also used in lubricants, leather dressings, toilet and dusting powders, and certain marking pencils. It is used as a filler in ceramics, paint, paper, roofing materials, plastic, and rubber; as a carrier in insecticides; and as a mild abrasive in the polishing of cereal grains such as rice and corn.
kaolin, also called china clay, soft white clay that is an essential ingredient in the manufacture of china and porcelain and is widely used in the making of paper, rubber, paint, and many other products. Kaolin is named after the hill in China (Kao-ling) from which it was mined for centuries. Samples of kaolin were first sent to Europe by a French Jesuit missionary around 1700 as examples of the materials used by the Chinese in the manufacture of porcelain. In its natural state kaolin is a white, soft powder consisting principally of the mineral kaolinite, which, under the electron microscope, is seen to consist of roughly hexagonal, platy crystals ranging in size from about 0.1 micrometre to 10 micrometres or even larger. These crystals may take vermicular and booklike forms, and occasionally macroscopic forms approaching millimetre size are found. Kaolin as found in nature usually contains varying amounts of other minerals such as muscovite, quartz, feldspar, and anatase. In addition, crude kaolin is frequently stained yellow by iron hydroxide pigments. It is often necessary to bleach the clay chemically to remove the iron pigment and to wash it with water to remove the other minerals in order to prepare kaolin for commercial use.
Bentonite is an absorbent aluminium phyllosilicate clay consisting mostly of montmorillonite. It was named by Wilbur C. Knight in 1898 after the Cretaceous Benton Shale near Rock River, Wyoming. The different types of bentonite are each named after the respective dominant element, such as potassium (K), sodium (Na), calcium (Ca), and aluminium (Al). Experts debate a number of nomenclatorial problems with the classification of bentonite clays. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin. For industrial purposes, two main classes of bentonite exist: sodium and calcium bentonite. In stratigraphy and tephrochronology, completely devitrified (weathered volcanic glass) ash-fall beds are commonly referred to as K-bentonites when the dominant clay species is illite. In addition to montmorillonite and illite anther common clay species that is sometimes dominant is kaolinite. Kaolinite-dominated clays are commonly referred to as tonsteins and are typically associated withcoal.
we can offer you Bentonite. Bentonite is an absorbent aluminium phyllosilicate clay consisting mostly of montmorillonite. It was named by Wilbur C. Knight in 1898 after the Cretaceous Benton Shale near Rock River, Wyoming. The different types of bentonite are each named after the respective dominant element, such as potassium (K), sodium (Na), calcium (Ca), and aluminium (Al). Experts debate a number of nomenclatorial problems with the classification of bentonite clays. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin. For industrial purposes, two main classes of bentonite exist: sodium and calcium bentonite. In stratigraphy and tephrochronology, completely devitrified (weathered volcanic glass) ash-fall beds are commonly referred to as K-bentonites when the dominant clay species is illite. In addition to montmorillonite and illite anther common clay species that is sometimes dominant is kaolinite. Kaolinite-dominated clays are commonly referred to as tonsteins and are typically associated withcoal.
we can offer you Ball Clay. Ball clays are kaolinitic sedimentary clays that commonly consist of 20-80% kaolinite, 10-25% mica, 6-65% quartz. Localized seams in the same deposit have variations in composition, including the quantity of the major minerals, accessory minerals and carbonaceous materials such as lignite. They are fine-grained and plastic in nature, and, unlike most earthenware clays, produce a fine quality white-coloured pottery body when fired, which is the key to their popularity with potters. Ball clays are relatively scarce deposits due to the combination of geological factors needed for their formation and preservation. They are mined in parts of the Eastern United States and from three sites in Devon and Dorset in South West England. They are commonly used in the construction of many ceramic articles, where their primary role, apart from their white colour, is to either to impart plasticity or to aid rheological stability during the shaping processes.
Bentonite is an absorbent aluminium phyllosilicate clay consisting mostly of montmorillonite. It was named by Wilbur C. Knight in 1898 after the Cretaceous Benton Shale near Rock River, Wyoming. The different types of bentonite are each named after the respective dominant element, such as potassium (K), sodium (Na), calcium (Ca), and aluminium (Al). Experts debate a number of nomenclatorial problems with the classification of bentonite clays. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin. For industrial purposes, two main classes of bentonite exist: sodium and calcium bentonite. In stratigraphy and tephrochronology, completely devitrified (weathered volcanic glass) ash-fall beds are commonly referred to as K-bentonites when the dominant clay species is illite. In addition to montmorillonite and illite anther common clay species that is sometimes dominant is kaolinite. Kaolinite-dominated clays are commonly referred to as tonsteins and are typically associated withcoal.
kaolin, also called china clay, soft white clay that is an essential ingredient in the manufacture of china and porcelain and is widely used in the making of paper, rubber, paint, and many other products. Kaolin is named after the hill in China (Kao-ling) from which it was mined for centuries. Samples of kaolin were first sent to Europe by a French Jesuit missionary around 1700 as examples of the materials used by the Chinese in the manufacture of porcelain. In its natural state kaolin is a white, soft powder consisting principally of the mineral kaolinite, which, under the electron microscope, is seen to consist of roughly hexagonal, platy crystals ranging in size from about 0.1 micrometre to 10 micrometres or even larger. These crystals may take vermicular and booklike forms, and occasionally macroscopic forms approaching millimetre size are found. Kaolin as found in nature usually contains varying amounts of other minerals such as muscovite, quartz, feldspar, and anatase. In addition, crude kaolin is frequently stained yellow by iron hydroxide pigments. It is often necessary to bleach the clay chemically to remove the iron pigment and to wash it with water to remove the other minerals in order to prepare kaolin for commercial use.
Origin - India, UAE , American & china Packaging - 25K Bag- 55 LB's Bag General Specs - "Color - Blackish Gray Sized powder Moisture content 1% Max Bulk density 750-950 Resiliency 100% Minimum Order - One 20 MT Container
We have the following for sale From different countries Ilmenite Graphite Rutile Zircon Quartz Feldspar Clay, Kaolin Apatite (Phosphate Rock), Silica Sand Garnet sand, Mica, Calcite Dolomite Please do connect with us for further details
Bentonite Clay is another one of the most common varieties of clays found in the world. Bentonite Clay is used in various products such as: Ceramic (Tile Companies) Drilling (Oil & Gas) Rubber & Tube Fertilizer Soap Making Paint & Coating ALAM CERAMIC ENTERPRISE carry Bentonite Clay in bulk quantity We are providing the best quality Bentonite Clay to industries up and foreign countries.
Gypsum Rock Size: 0-50mm Purity: CaSO42H2O â?? Min 90% - as per shared specs SIO2: 0.26 AI2O3: 0.16 Fe2O3: 0.19 CaO: 32.42 Na2O: 0.02 K2O: 0.02 MgO: 0.59 TiO: 0.012 MnO: 0.015 P2O5: 0.023 SO3 : 45.78 L.O.I: 20.18
Arc333 - 3d gypsum tiles The first 3d gypsum tile in the gypsum tile industry
Gypsum board from saudi to india, srilanka & other countries
We supply drywalll screws as per the customer sizes
Pvc laminated gypsum tiles Sizes - 595 x 595 , 603 x 603 Thickness - 7mm , 8mm Branding can be done as per customer requirement
Crude oil, bauxite.Buying agent, export
Micro Silica, Fly Ash, Slag, Ggbs, Copper Ore Concentrates, Nickel Ore Concentrates..Importer
