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内生钒矿床成因类型的建立要考虑与矿化有成因联系的岩浆岩建造和控制含矿侵入体位置的区域构造。划分出岩浆的、接触交代的和水热的钒矿床类型。按储量和开采量来说首要的是在基性和超基性杂岩侵入体里的含钒钛磁铁矿、磁铁矿-钛铁矿以及较少见的赤铁矿-金红石-钛铁矿等矿石类型构成的岩浆矿床。在这些矿床中钒的主要富集者是钛磁铁矿和磁铁矿(含量可达4.9％.通常是0.x％)。钒的最大富集联系着古地台和结晶台盾周围的前塞武纪的岩浆岩建造——斜长岩侵入体(美国阿德朗达克山磁铁矿—钛
The establishment of genetic types of endogenous vanadium deposits should take into account the regional structure of the magmatic rocks that are genetically linked to mineralization and the location of ore-bearing intrusions. Divided magmatic, contact metasomatism and hydrothermal vanadium deposit types. In terms of reserves and production, the most important are vanadium-bearing titanium magnetite, magnetite-ilmenite, and rare hematite-rutile-ilmenite Ore and other ore types of magmatic deposits. The major contributors to vanadium in these deposits are titanium magnetite and magnetite (up to 4.9%, usually 0.x%). The maximum enrichment of vanadium is associated with the formation of the Paleo-Sertury magmatic rocks around the Paleoqidai and Jinghuai shields - plagioclase intrusions (Adirondack Mountain Magnetite-Titanium