Abstract: The Paleozoic metallogenic doma in of the Central Asian was agiant metallogenic doma in which can compare favourably with the ring Pacific ocean and the Tethys. Its mineralization has the manifest singularity of the Paleozoic orogenic mineralization. In the every stage that crustal develops ten siletran sitional,crust-oceanic,crust-convergent transitional, crust-new continental of the Paleozoic orogenic zone in Meddle Asia,it formed various specific metallogenic series type. The series type evolved regularly with the raise of the crustal maturity.