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艾肯达坂一带火山机体位于伊犁石炭—二叠纪裂谷阿吾拉勒二叠纪火山岩带东段，在航卫片上表现为较明显的环形构造。艾肯达坂火山穹窿构造保留较完整，地层层面和流动构造呈现以次安山岩为中心，向周边倾斜，倾角平缓稳定，大多小于３０°，火山岩相较完整，集块岩、火山角砾岩、熔岩等发育，火山岩以钙碱性系列为主，形成环境为造山带，时代确定为早三叠世早期。艾肯达坂铜银矿及３个铜矿点均受艾肯达坂火山穹窿的环状断裂和放射状断裂及交汇处控制。
The volcanic body in the area of Ai Ke Daban is located in the eastern section of the Awulale Permian volcanic belt in the Carboniferous-Permian rift in the Yili area, showing a rather pronounced ring structure on the Hangwei sheet. The structure of the Aiken Daban volcano dome retains relatively intact. The stratigraphic and flow structures are characterized by the sub-andesite, which is inclined toward the periphery and gently and steadily inclined, mostly less than 30 °. The volcanic rocks are relatively complete, and the volcanic rocks are conglomerate, volcanic breccia, Lava and other development, volcanic rocks to calcium-alkaline series, the formation of the environment orogenic belt, the era identified as Early Triassic early. Aiken Daban copper-silver mine and three copper deposits are subject to the ring of Aiken Daban volcano dome fracture and radial fracture and intersection control.