Geological Characteristics And Mineralization Of Nalaqing Vanadium-titanium Magnetite In Panzhihua

Panzhihua vanadium-titanium magnetite is a typical multi-metal associated mineral.Despite iron, vanadium, titanium, it associated with useful components such as chromium,cobalt, nickel, platinum, scandium, two dozen beneficial component, wherein ilmenite reserves and ranks first in the world; vanadium ore reserves ranking first in the country and the third in the world. It occupies an important position in China's mineral resources.Funding projects of Panzhihua vanadium-titanium magnetite fully equipped exploration-based, as Nalaqing vanadium-titanium magnetite of Panzhihua is the research object, first systematically use the material, chemical, remote areas combine information on the surrounding deposits field geological survey analyzed regional metallogenic background, and through the work of the mine geological stratigraphy, structure, rock and ore mining spatial distribution, mineral composition, structure, mineral content, ore group structure, chemical composition and other characteristics of the ore are summarized geological characteristics and mineralization regularity inquiry, on this basis, and then based on magmatic theory, a more detailed analysis of the crystalline mineral iron mineralization of Nalaqing vanadium-titanium magnetite of Panzhihua, to arrive at the overall Panzhihua is a multi-stage magmatic differentiation crystallization deposits, and exhibit more pronounced rhythm.The geological characteristics of Nalaqing vanadium-titanium magnetite deposit of Panzhihua analysis and study of metallogenic regularity, guided the deep ore bodies and relatively poor ore body for further work and by the contrast of north and south sections mineralization law of Panzhihua vanadium-titanium magnetite, making the whole theory of Panzhihua vanadium-titanium magnetite mineralization more rich and complete.