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阿吾拉勒陆相火山岩型铜矿分为火山热液型、次火山热液型和中低温热液充填脉型，认为岩浆和成矿物质来源于深部地壳或上地幔，成矿与华力西晚期火山一次火山作用密切相关，铜矿是在同一构造环境下同一岩浆源分异演化不同阶段的产物。矿床成因属中低温火山一次火山热液成因。
The Ulalale continental volcanic copper deposits are divided into volcanic hydrothermal, sub-volcanic hydrothermal and medium-low temperature hydrothermal filling vein types. The magma and ore-forming materials are derived from deep crust or upper mantle, mineralization and Variscan Late Volcano is closely related to a volcano, and copper deposits are the products of different stages of the same magmatic source differentiation and evolution under the same tectonic setting. Origin of the deposit is a volcanic hydrothermal cause of low-temperature volcanoes.