Ore concentrates and minerals, semi precious metals, oil products, fertilizers, f&b items, light & heavy industrial equipment, urea granular 46b, vietnamese jasmine rice, sulphur, sugar.Import/export, trade facilitation, distribution, recycling & recovery of metals
We are offering Crystal Gypsum in different sizes.
We produce high quality and super fine GYPSUM POWDER. It is available in different packaging and we also offer it in various setting time.
Applications: In glass making In ceramics production
Sodium Bentonite (Oil Well Drilling 13A Sec 9& Sec 11 / Piling Grade) & Calcium Bentonite 25 Kg, 50 Kg, 1 ton
Origin - India, American & Egypt Packaging - 55 Gal Drum Minimum Order - One 20 MT Container
Nepheline is an important feldspathoid mineral. It is white, grey or yellow in colour with a vitreous lustre and a poor cleavage. The name Nepheline comes from the Greek word nephele, which means cloud, because it becomes strongly clouded when put in strong acid. Nepheline only forms in silica-poor rocks. It is almost never associated with quartz. It may be found in some contact metamorphosed rocks otherwise it occurs in alkaline complexes in igneous rocks. Nepheline is mostly found in the rock Nepheline Syenite in nature.
Chemical analysis: Baso4 90% min Water soluble solids 0.1% max Moisture content 1% max Size 200 mesh Physical analysis : S.G 4.1 gr / cm 3 min
Silica 64.94 Aluminum 12.46 Sodium 1.99 Magnesium 2.61 Potassium 0.26 Titanium 0.31 Manganese 0.02 Calcium 0.94 Phosphorus 0.02 Sulfate 0 Iron 2.69 L.O.I 13.41
Direct selling zeolite from Iran No packed and sizes are free
We have the Availability of Dead Burned Magnesite. If Anyone have the requirement please let us know.
Talc, Hydrous magnesium silicate Mg3Si4O10(OH)2 is a hydrous magnesium silicate mineral with a chemical composition of Mg3Si4O10(OH)2. Although the composition of talc usually stays close to this generalised formula, some substitution occurs. Talc, a mineral made up mainly of the elements magnesium, silicon, and oxygen. As a powder, it absorbs moisture well and helps cut down on friction, making it useful for keeping skin dry and helping to prevent rashes. Ground talc makes talcum powder. The massive variety (soapstone) is used for sinks, table tops, etc. Soapstone found a use in Babylonian days when signature cylinder seals were often carved from it. The Egyptians also used it as a base for some of their blue faience figurines, which were then fired to fuse the glaze. California Indians also used it as sculpture material. Eshal
Cryptocrystalline Magnesite MgCO3 with extremely low silica and iron content, white colour, and very low level of heavy metals. RMA is a raw magnesite milled product with 90% MgO content on ignited basis, which is used in the production of ceramics (tiles etc.). Magnesium Carbonate: isolation, rubber, ink, glass, ceramics, paint, pharmacy and cosmetics industry. Magnesium Chloride: Magnesium metal production, textile, paper, ceramics and cement. Magnesium sulphate: Pharmaceutics, artificial fertilizer industry.
Particle size - 2 microne density 0.5 Oil absorption -30 Flow point 20 25 kg Paper bag
Are you looking for potash in metric tonnes and would like to know more in order to provide you with a suitable inquiry. What are you going to do with it Also, do you want it in huge chunks crushed Because each procedure is unique and comes in a variety of packages. 50 pound bags are the most handy and popular
Red shale Shale is a fine-grained sedimentary rock that forms from the compaction of silt and clay-size mineral particles that we commonly call "mud". Application • Shale is used to produce cement, • Terra cotta pots, bricks and tile roofs.
Barite is a mineral composed of barium sulfate (BaSO4). It receives its name from the Greek word "barys" which means "heavy." This name is in response to barite's high specific gravity of 4.5, which is exceptional for a nonmetallic mineral. The high specific gravity of barite makes it suitable for a wide range of industrial, medical, and manufacturing uses. Barite also serves as the principal ore of barium. Most barite produced is used as a weighting agent in drilling muds. This is what 99% of the barite consumed in the United States is used for. These high-density muds are pumped down the drill stem, exit through the cutting bit and return to the surface between the drill stem and the wall of the well. This flow of fluid does two things: 1) it cools the drill bit; and, 2) the high-density barite mud suspends the rock cuttings produced by the drill and carries them up to the surface. Barite is also used as a pigment in paints and as a weighted filler for paper, cloth and rubber. The paper used to make some playing cards has barite packed between the paper fibers. This gives the paper a very high density that allows the cards to be "dealt" easily to players around a card table. Barite is used as a weighting filler in rubber to make "anti-sail" mudflaps for trucks. Barite is the primary ore of barium, which is used to make a wide variety of barium compounds. Some of these are used for x-ray shielding. Barite has the ability to block x-ray and gamma-ray emissions. Barite is used to make high-density concrete to block x-ray emissions in hospitals, power plants, and laboratories. Barite compounds are also used in diagnostic medical tests. If a patient drinks a small cup of liquid that contains a barium powder in a milkshake consistency, the liquid will coat the patient's esophagus. An x-ray of the throat taken immediately after the "barium swallow" will image the soft tissue of the esophagus (which is usually transparent to x-rays) because the barium is opaque to x-rays and blocks their passage. A "barium enema" can be used in a similar way to image the shape of the colon.
Dolomite is a common rock-forming mineral. It is a calcium magnesium carbonate with a chemical composition of CaMg(CO3)2. It is the primary component of the sedimentary rock known as dolostone and the metamorphic rock known as dolomitic marble. Limestone that contains some dolomite is known as dolomitic limestone. Dolomite is rarely found in modern sedimentary environments, but dolostones are very common in the rock record. They can be 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. Dolomite is also a common mineral in hydrothermal veins. There it is often associated with barite, fluorite, pyrite, chalcopyrite, galena, or sphalerite. In these veins it often occurs as rhombohedral crystals which sometimes have curved faces Dolomite as a mineral has very few uses. However, dolostone has an enormous number of uses because it occurs in deposits that are large enough to mine. The most common use for dolostone is in the construction industry. It is crushed and sized for use as a road base material, an aggregate in concrete and asphalt, railroad ballast, rip-rap, or fill. It is also calcined in the production of cement and cut into blocks of specific size known as "dimension stone." Dolomite's reaction with acid also makes it useful. It is used for acid neutralization in the chemical industry, in stream restoration projects, and as a soil conditioner. Dolomite is used as a source of magnesia (MgO), a feed additive for livestock, a sintering agent and flux in metal processing, and as an ingredient in the production of glass, bricks, and ceramics. Dolomite serves as the host rock for many lead, zinc, and copper deposits. These deposits form when hot, acidic hydrothermal solutions move upward from depth through a fracture system that encounters a dolomitic rock unit. These solutions react with the dolomite, which causes a drop in pH that triggers the precipitation of metals from solution. Dolomite also serves as an oil and gas reservoir rock. During the conversion of calcite to dolomite, a volume reduction occurs. This can produce pore spaces in the rock that can be filled with oil or natural gas that migrate in as they are released from other rock units. This makes the dolomite a reservoir rock and a target of oil and gas drilling.
Quartzite is a very hard rock composed predominantly of an interlocking mosaic of quartz crystals. The grainy, sandpaper-like surface is glassy in appearance. Minor amounts of former cementing materials, iron oxide, silica, carbonate and clay, often migrate during recrystallization, causing streaks and lenses to form within the quartzite. To be classified as a quartzite by the British Geological Survey, a metamorphic rock must contain at least 80% quartz by volume Parameters Percentage Silica (SiO) : 97.00% Alumina (Al - O) : 1.00% Moisture : 1.00% Size : 10 to 40 mm, 20 to 70 mm, 40 to 80 mm Origin ; Maharashtra, India.
Laterite is both a soil and a rock type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by intensive and prolonged weathering of the underlying parent rock, usually when there are conditions of high temperatures and heavy rainfall with alternate wet and dry periods
