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浩尧尔忽洞金矿位于华北陆台北缘西段中元古界白云鄂博裂谷带西段。区内出露地层有中元古界白云鄂博群尖山组、哈拉霍疙特组和比鲁特组,其中比鲁特组第二岩段为主要的赋矿地层。区内主要构造为浩尧尔忽洞向斜,其核部为比鲁特组,两翼分别为尖山组和哈拉霍疙特组,矿床产于NE向展布的向斜南翼。断裂构造主要为一条左行的脆韧性剪切带和一条近NE向展布的平移断层。整个剪切带由一系列呈近EW向到NE向分布的近似平行的挤压破碎带和片理化带构成,是最重要的导矿和容
Hao Yao Seoul hole gold mines located in the northern margin of North Taiwan Rutai Miocene Epoch Proterozoic Bayan Obo rift western section. The exposed strata in the area include Jianshan Formation, Halahuojute Formation and Birut Formation of Mesoproterozoic of Bayan Obo Group, in which the second member of the Beirut Formation is the main ore-bearing formation. The main structure of the area is the Haooyuerhugong syncline, the core of which is the Beirut Formation, and the two wings are the Jianshan Formation and the Halahuojute Formation, respectively. The ore deposit is produced in the southward syncline of the NE direction. The fault structure is mainly composed of a left-bank brittle-ductile shear zone and a translational fault with near NE spreading. The entire shear zone is composed of a series of approximately parallel crushed and fragmented zones distributed in a nearly EW-to-NE direction and is the most important guide and tolerance