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奥木和金矿产于中泥盆统萨吾尔山组中性火山岩地层中,矿体受断裂构造控制,矿体定位于强硅化带中,属构造破碎带蚀变岩型金矿床。
The Aoki and gold mines are found in the neutral volcanic rocks of the Middle Silurian Uygur group. The ore body is controlled by the fault structure. The orebody is located in a strong silicification zone and belongs to the structural crustal altered rock type gold deposit.