This dataset describes the vanadium-titanium magnetite ore from Sichuan Province, with the following information:
Vanadium-titanium magnetite is a complex, polymetallic ore primarily containing iron, vanadium, and titanium, and associated with various valuable elements (such as chromium, cobalt, nickel, copper, scandium, gallium, and platinum group elements). It has high contents of valuable elements, making it an important industrial mineral resource with significant potential for development and comprehensive utilization. In recent years, global demand for vanadium and titanium products has been continuously increasing. Vanadium products are primarily used in the steel industry and energy storage batteries, while titanium materials are widely applied in chemical engineering, aerospace, power generation, and light industry. Vanadium-titanium magnetite has closely associated iron and titanium, with titanium, vanadium, chromium, etc. occurring in the form of isomorphous substitution within vanadium-titanium magnetite. In nature, vanadium-titanium magnetite primarily forms in mafic and ultramafic rock bodies. Common valuable ore minerals in such deposits are mainly vanadium-titanium magnetite and ilmenite, along with minor amounts of magnetite, hematite, and sulfides. Vanadium-titanium magnetite is a type of magnetite containing exsolved solid solution phases such as ilmenite, ulvöspinel, and magnesioferrite; through regional metamorphic processes, it can recrystallize into ilmenite and magnetite. Generally, vanadium-titanium magnetite contains 1%–15% TiO₂ and V₂O₅0. 1% to 2%. The chemical composition of ilmenite is FeTiO3. Ilmenite contains 52.66% TiO2. Complete solid solution can occur between Fe2+ and Mg2+, Mn2+, forming the FeTiO3-MgTiO3 or FeTiO3-MnTiO3 series. When FeO is dominant, it is called ilmenite; when MgO is dominant, it is called geikielite; and when MnO is dominant, it is called pyrophanite. Ilmenite has a Mohs hardness of 5–6, a specific gravity of 4.70–4.78, weak magnetism, and a magnetic susceptibility of 1173.33–224. 56×10^-9 m³/kg. The Panzhihua-Xichang area in southwestern Sichuan is located in the hinterland of Sichuan Province. The mining region has experienced intense neotectonic movements, which primarily resulted in a series of northwest to west-northwest trending faults, reactivation of north-south trending fractures, and strong differential uplift and subsidence. These tectonic activities have formed a magmatic complex zone composed of magmatic rocks of different types and ages. Along this complex zone, from south to north, there are stratiform mafic to ultramafic intrusions containing titanomagnetite deposits at Panzhihua, Hongge, Baima, and Taihe. These intrusions constitute a north-south trending vanadium-titanium magnetite metallogenic belt, which is the most extensive and richest in reserves of vanadium and titanium resources, and represents one of the world's major regions for this type of deposit. Due to its enormous potential resources, it is known as " natural resource base," it is widely used in various industries. The Panzhihua, Hongge, Baima, and Taihe four typical super-large vanadium-titanium magnetite mining areas are not only very important special iron and steel ore supply bases in China, but also important production sites for vanadium and titanium metals, holding significant strategic and economic importance.