Product Description : 3-5mm granules,color:PINK Price of product ( USD price or FOB price) : USD 350- USD 400 per MT Product origin : Khewra Mines,Pakistan Key Specifications/Special Features : Himalayan Crystal Salt is the most beneficial, cleanest salt available on this planet, mined in Khewra Mines of Jhelum district of Punjab region in Pakistan.With history of about 250 million years and contains all the elements found in our bodies. In this crystal salt, the elements are available in such tiny particles that they can be easily absorbed by the human cells and metabolized. Crystal Salt was once called ""King Salt"" because it was reserved for Royal families where as common Citizens only got Rock Salt. Minimum Order Size and Packaging details : 50kgs,25kg or 800g-AURA branding
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
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.
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.
Chromite is a mineral composed of iron, chromium, and oxygen (FeCr2O4). It is a dark-colored mineral that is commonly found in ultramafic rocks, and it is the main source of the metal chromium. Chromite is highly valued for its high chromium content, as chromium is a critical component in the production of stainless steel and other alloys. It is also used in the production of refractory materials and pigments. Chromite is notable for its high melting point and resistance to corrosion, making it a valuable mineral for a variety of industrial applications. After extracting chromium from mines located in Pakistan and Afghanistan, our dedicated processing team meticulously assesses and grades the chromium ore lumps before delivering them to our esteemed customers. Our product range encompasses multiple grades, including: 1. Metallurgical Grade: With chromium oxide content ranging from 26% to 42% (Cr2O3), our metallurgical grade chromium ore is ideal for industries requiring high-quality raw materials for stainless steel production and alloy manufacturing. 2. Refractory Grade: Our refractory grade chromium ore boasts chromium oxide content between 48% and 54% (Cr2O3) while maintaining silica content at a maximum of 3.5%. This grade is well-suited for applications where high-temperature resistance is critical, such as refractory materials for furnaces and kilns. We take pride in successfully supplying these grades to various markets, including China and Europe, catering to the diverse needs of our clients. With a substantial monthly production capacity of 15,000 tons, Bare Syndicate stands as a dependable source for fulfilling industrial demands. In addition to our expertise in chromium extraction and processing, our extensive experience in logistics and international trade allows us to provide our customers with a comprehensive solution for their supply management needs.
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