This dataset describes Sichuan vanadium-titanium magnetite, with the following information introduction:
Vanadium-titanium magnetite is a complex associated mineral primarily composed of iron, vanadium, and titanium, and coexisting with various valuable elements (such as chromium, cobalt, nickel, copper, scandium, gallium, and platinum group elements). It has high content of valuable elements and is an important industrial mineral resource with significant development and comprehensive utilization value. In recent years, the global demand for vanadium and titanium products has been continuously increasing. Vanadium products are mainly used in the steel industry and energy storage batteries, while titanium materials are widely applied in chemical industry, aerospace, power, light industry, and other fields. Vanadium-titanium magnetite features a close association between iron and titanium, with titanium, vanadium, chromium, and other elements occurring in the form of isomorphous substitution within vanadium-titanium magnetite. In nature, vanadium-titanium magnetite primarily forms within mafic and ultramafic rock masses. Common valuable ore minerals in such deposits include vanadium-titanium magnetite and ilmenite, along with minor amounts of magnetite, hematite, and sulfides. Vanadium-titanium magnetite is a magnetite containing exsolved solid solutions such as ilmenite, ulvöspinel, and magnesium-aluminum spinel, which can, through regional metamorphism, recrystallize into ilmenite and magnetite. Typically, vanadium-titanium magnetite contains 1%–15% TiO₂ and V₂O₅0. 1% to 2%. The chemical composition of ilmenite is FeTiO3. Ilmenite contains 52.66% TiO2. Fe2+ can be completely isomorphously substituted by Mg2+ and Mn2+, forming FeTiO3-MgTiO3 or FeTiO3-MnTiO3 series. When FeO predominates, it is called ilmenite; when MgO predominates, it is called geikielite; when MnO predominates, 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, forming a series of predominantly northwest to west-northwest trending faults, reactivation of north-south trending fractures, and strong differential uplift and subsidence. These processes have created a magmatic complex zone composed of different types of igneous rocks from various geological periods. Along this magmatic complex zone, from south to north, there are stratabound 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 widespread and richest in reserves of vanadium and titanium resources, and is also one of the world's major producing regions of this type of deposit. Due to its enormous potential resources, it is known as " The natural resources of these "natural resource repositories" are widely used in various industries. The Panzhihua, Hongge, Baima, and Taihe, four typical super-large vanadium-titanium magnetite mining areas, are very important special iron and steel ore supply bases in China, as well as significant production sites for vanadium and titanium metals, possessing extremely important strategic and economic status.