Mesozoic intermediate and acidic dykes which are closely related to Huangnihe granite were formed during the mineralization period.
中生代中酸性脉岩为成矿期脉岩，且与黄泥河花岗岩岩基有着密切的成因联系。
Shapes, occurrences, thicknesses and tenors of the ore bodies were controlled by features, occurrences and sizes of the fractures active during the mineralization period.
矿体的形态、产状、厚度、品位等完全受控于成矿期断裂的性质及其产状、规模。
Porphyry mineralization, occurred in the Silurian Period, finally formed ore bodies.
晚期矿化发生于志留纪，使矿床最终形成。
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