Vanadic titanomagnetite deposits in the Kangdian Axis, Sichuan are confined to layered basic and ultrabasic intrusions. They may be divided into two subtypes such as basic magmatic differentiation subtype and ultrabasic magmatic differentiation subtype. This paper deals with time-space evolution for three minerogenetic series of ore deposits and host intrusions with geological setting, time and depth of intrusion emplacement, character of wall rock and its influence on diagenesis and mineralization, magmatic origin and evolution and genesis of intrusions and vanadic titanomagnetite deposits.