alkali Basalt is a heavy volcanic rock that makes up most of the world's oceanic crust with igneous composition and availability in most markets around the world at cheap price. Some of these also erupt on land, but generally, basalt is a marine rock. Basalt ("ba-SALT") is darker, denser, and more detailed than the familiar continental granite. This material is dark and dense because it is rich in dark and heavy metals containing magnesium and iron (i.e. mafic) and weaker silicon and aluminum minerals. It is cooled and contains only very small crystals. Much of the world's basalt erupts quietly in the deep ocean, along the highlands in the middle of the ocean - areas where plate tectonics spread. Small amounts of basalt erupt in volcanic islands in the ocean, in higher subduction zones, and in occasional large events elsewhere. Basalt is a type of lava where rocks in the mantle begin to melt. If you think of basalt as mantle juice, when we talk about oil extraction from olives, basalt is the first compression of the fleshy material. 
The biggest difference is that olives hold oil under pressure, and when the pressure in the mantle is released, intermediate basalts form. The upper mantle consists of rocky peridotite, more basalt. It is called ultramafic. As the Earth's plates separate at continental boundaries, the release of pressure in the peridotite causes it to begin melting - the exact composition of the melt depends on many details, but it usually cools and separates into the minerals clinopyroxene and plagioclase, the smaller A large amount of olivine, rhombohedrite and magnetite. What's more, any water and carbon dioxide in the source rock will also move toward the melt, causing it to melt even at low temperatures. Peridotite is dry, with a high deficiency of olivine and orthopyroxene. Like almost all materials, molten rock is less dense than solid rock. Once formed deep in the Earth's crust, basaltic magma rises to the center of the central cavity overlying ocean valleys, where it accelerates in icy water to form lava pillows. , unsprayed basalt hardened into mounds, stacked vertically like cards in a deck. These dike complexes cover the mid-ocean crust and beneath are larger reservoirs of magma that slowly crystallize into plutonic gabbros. However, the oceanic crust is constantly returning to the mantle through plate tectonics. As a result, MORB is rare, even though it is the main constituent of basalt in the world. To study it, we had to go to the bottom of the ocean with cameras, samples and submarines. 
Alkali basalt price per ton
The price for basalt is around 175$ per ton for each pallet. Ordinary alkaline basalt contains olivine, usually bipyrite or titanite. Alkaline basalts predominate in lavas in oceanic basins and are common in mafic lavas in foreland and back mountains. In Brito-Iceland, the Paleogene and Neogene. The diversity of minerals and their use in various industries has forced many developed countries to make huge investments in the mining industry. Minerals are mined and processed back into the processing process, allowing the minerals to obtain the necessary economic benefits. At the same time, basalt is one of the minerals obtained from volcanic activity, and the processing of this mineral offers the possibility of its application in various industries from road construction to fiber production. The stone, which is called alkaline stone because it does not contain silicon, is also abundant in Iran and has been used by the ancients for a long time. Of course, it should be noted that today, many industrialized and developed countries rely on modern engineering knowledge and equipment to process this mineral and use it to make lightweight and durable steel bars, automobile and ship hulls, and oil and gas pipelines. 
It is likely that many of you have heard the name basalt in school and education because of your field of study or construction work environment, and a question has formed in your mind, what kind of stone is basalt, its characteristics and What are the characteristics? Or what is the use of basalt in construction and other industries. This stone is one of the most abundant types of stone on earth, and due to this abundance, it is used in large quantities in various industries including the construction industry. The many uses of this stone prompted us to show you this stone by examining its properties. This stone is one of the most abundant on earth after granite and comes in different types. Some basalts have a completely glassy structure (tachydrite), and many basalts have a fine-grained and dense structure. The typical form of basalt is a porphyritic structure with large crystals of olivine, pyroxene or feldspar (phenocryst) in a fully crystalline matrix (matrix). The minerals olivine and pyroxene are the most common porphyry minerals in basalt. In addition to these two minerals, porphyry plagioclase is also found in basalt structures. Basalt lava is usually spongy or pumice-like. The cavities formed by the gases and vapors released by the lava material are filled with secondary minerals such as calcite, chlorite and zeolite. 
Basalt price per ton
The average price for basalt is 60$ per ton but based on the quality and type this could widely vary. Various igneous rocks and minerals are currently being evaluated as potential prospects for promoting permanent carbon sequestration. Olivine, serpentine, and peridotite are some of the many substances that combine with carbon dioxide to form carbonates, thereby removing the bound carbon more permanently. This article is about a rock that deserves more attention: basalt. Basalt is an igneous rock that is widespread throughout the world and can combine with carbon dioxide faster than other options. Different forms of basalt are a strong candidate for large-scale subsurface or in situ carbonation of minerals, so why isn't it a hotter topic in carbon removal? To achieve this, there are various rocks used to remove and store carbon. Those believed to sequester carbon may do so by enhancing the corrosion process. Enhanced erosion usually occurs at the surface level, such as the mineral olivine that binds to environmental carbon dioxide along the coastline. For storage purposes, rocks can be evaluated based on their presence in different layers below the Earth's crust. For both processes, mineralization can occur where siliceous materials and gases, such as carbon dioxide, combine to form products such as carbonates. Basalt is generally considered to be storable. 
The carbon dioxide must first be captured by other technological processes and then injected into the basalt aquifer for carbonation. Although basalt has the potential to be used for weathering purposes, the focus of this article will be on in-situ storage. This stone is one of the most abundant on earth after granite and comes in different types. Some basalts have a completely glassy structure (tachydrite), and many basalts have a fine-grained and dense structure. The typical form of basalt is a porphyritic structure with large crystals of olivine, pyroxene or feldspar (phenocryst) in a fully crystalline matrix (matrix). The minerals olivine and pyroxene are the most common porphyry minerals in basalt. In addition to these two minerals, porphyry plagioclase is also found in basalt structures. Basalt lava is usually spongy or pumice-like. The cavities formed by the gases and vapors released by the lava material are filled with secondary minerals such as calcite, chlorite and zeolite. Basalts are generally divided into two major categories based on their chemical and petrological properties: tau basalts and alkaline basalts. Laban basaltic lava is characterized by calcareous plagioclase, with pyroxene, mafic or superpyrite and olivine as the main basic minerals. Basalt without olivine is also well represented. Labanite basalts containing 45-63% silica are rich in iron, including Labanite basalts (calcium-poor pyroxene basalts). They dominate lava in the mountains. Alkali basalts are rich in alkali metals. This type of basalt, unsaturated silica, may contain striatum, alkali feldspar, phlogopite, and olivine. Augustus is a titanium-rich pyroxene in alkaline basalt, and low calcium pyroxene was never present. In some cases, basalt is divided into two categories, high-titanium and low-titanium, based on titanium content. In some cases, gemstones are divided into two categories based on titanium content: high-titanium and low-titanium. 
Alkali basalt composition
Alkaline basalt or olivine Alkaline basalt in composition is a dark porphyry volcanic rock commonly found in oceanic and continental areas associated with volcanic activity, such as oceanic islands, continental rifts, and volcanic fields. The mineral characteristics of basalt depend on the content of plagioclase, feldspar, and pyroxene. Olivine can also be a defined and important compound. Minor minerals found in basalt include iron oxides and iron-titanium oxides such as magnetite, olivine, and ilmenite. Due to the presence of this mineral oxide, basalt can acquire strong magnetism as it cools. In puller basalt, pyroxene (pyroxene and orthopyroxene or dove) and plagioclase are rich in calcium, a mineral commonly found in phenocrysts. Olivine can also be phenocryst. Alkaline basalts typically have mineral assemblages that lack orthopyroxene but contain olivine. The composition of feldspar phenocrysts typically ranges from lavadorite to feldspar. The augite in the bila porphyry basalt is rich in titanium. Basalt has high liquid and solid temperatures. The liquid temperature value of basalt on the earth's surface is equal to or greater than 1200 degrees Celsius, and the solid temperature is equal to or less than 1000 degrees Celsius, which is higher than other common igneous rocks. Most basalts form about 50 to 100 kilometers deep in the mantle. Many alkaline basalts can form at greater depths, possibly as deep as 150-200 kilometers in the mantle. Experts are still divided on the origin of high-alumina basalt, mainly on whether the original molten material cooled into rock or whether other types of basalt broke down. One of the most important applications of basalt is its use in the production of basalt fibers. 
Basalt is a neutral natural material that is the product of extrusive igneous rocks, the main rock type in the Earth's crust. One of the characteristics of materials containing basalt compounds is that these materials are completely compatible with the environment and are completely non-toxic. For this reason, they use basalt to produce basalt fibers. One of the characteristics of basalt fiber is its high chemical stability compared to glass fiber, especially in noisy playing environments. These fibers are non-toxic, non-flammable and resistant to high temperatures. Another feature of these fibers is their relatively high thermal stability, which is why basalt has three times the thermal insulation capacity of refractory wool, which is why these fibers are used for marine fire protection due to their excellent insulating properties. Furthermore, according to research and studies conducted in the field of fibers for the marine industry, it has been concluded that basalt fibers have mechanical properties comparable to or even better than E-glass fibers, and therefore, these fibers are a suitable choice for use on board ships. And for the final part, More than 8% of the Earth's surface consists of basalt, Sanna et al. noted that the storage potential of the basalt ocean could reach 8,238 gigatons (at a depth of 2,700 meters, 200 meters of sediment form a capping layer for capture). This marine storage is attractive because the sedimentary layers of the deep ocean would provide an additional layer of natural infiltration to retain carbon in the soil and reduce potential escape, effectively acting as a "lid" to capture the carbon beneath it. Trap is important because it helps prevent gas escape during mineralization. 
For other rock forms, elevated temperatures (think: energy demands), higher levels of carbon dioxide removal, and high pressure may place stricter requirements on persistence below the Earth's surface. This is an important question because proper storage can reduce the risk of escaping back into the atmosphere or ocean. The basalt has also recently been found to be mineralizing at a much faster rate than previously expected. The CarbFix project near the Hellisheidi power plant in Iceland conducted a pilot study in 2012, pumping more than 175 tons of clean carbon dioxide into a basalt aquifer. Initial expectations were that the mineralization process would take years, but the study found that the carbonate material formed in just two years, impressing scientists with its rapid recovery time and storage potential. Cap rates are also generally cheaper than other mineralization options. In areas such as Wallula, WA and the vicinity of Hellisheidi, the cost of storage per ton of stored coal is around $10-30. Although the price of deep ocean basalt reserves is higher, early estimates can reach $200 per ton. In contrast, serpentine has higher pressure, temperature, and cleaning requirements, and promises prices may range from $200 to $600 per ton. My company has for long been the lead in both supply and export of basalt products to all countries around the world and is hence gently honored to invite all dear customers and traders to join us in world trade of basalt and experience the best purchase of basalt ever in your life.