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研究认为在不同时代、不同地质构造单元中重复出现的矿床成矿系列，可称为矿床成矿系列类型。新疆主要矿床成矿系列类型带有鲜明的古生代造山带成矿作用特点，它们联系于新疆各造山带古生代地壳发展的拉张型过渡壳－洋壳－汇聚型过渡壳－古生代新陆壳的各特定阶段，与各阶段地质构造作用密不可分。矿床成矿系列类型本身也随着地壳发展、地壳成熟度的提高而有规律地演化
It is concluded that the ore-forming series recurring in different geological tectonic units in different ages may be regarded as the type of metallogenic series. The types of metallogenic series of the major gold deposits in Xinjiang are characterized by distinct Paleozoic orogenic belt mineralization. They are related to the extensional transitional crust-oceanic crust-convergent transitional crust-Palaeozoic new continental crust developed in all orogenic belts in Xinjiang The specific stage, with the role of geological structure in each stage are inseparable. The type of metallogenic series of deposits also evolves regularly along with the development of the crust and the maturity of the crust