Abstract:Minerogenetic series of mineral deposits(minerogenetic series for short) is a theoretical concept in the field of mineral deposits, which can be divided into five orders by ore- forming sequence. As the first order, minerogenetic series group is a set of interrelated minerogenetic series for mineral deposits which developed in a certain period of geological history and in a certain crustal movement process. A complete minerogenetic series group (G) ideally contains 5 types of minerogenetic series for mineral deposits of relating to igneous magmatism (I), sedimentation (S), metamorphism (M), regional tectonic eventfluid action (F) and hypergenesis (H). From the perspective of tectonic evolution, the formation of minerogenetic series group is internally related to the stage and cycle of continental mineralization system, which is the objective record and inevitable product of different stages of crustal tectonic evolution and can correspond to crustal scale tectonic movement. In- depth study of minerogenetic series group is of great significance to explore the evolution regularity of the earth, deepen understanding of metallogenic tectonic environment and metallogenic process at different scales and periods, and reveal the basic law of crustal movement. At the same time, the application of the concept of “mineralization in allposition, exploration to any location” and the principle of “metallogenic sequence” (order) can not only explain the uneven distribution of mineral resources, but also guide the regional metallogenic prediction effectively. The study of minerogenetic series group is still in the initial stage and needs to be further studied because it involves extensive subject knowledge.