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该矿床的钨锡石英脉切穿泥盆系砂页岩和碳酸盐岩,产于一组共轭 X 节理系中。矿脉具对称带状构造,可用交代成分共生图解解释。计算表明,富钙环境中也能形成黑钨矿。组成复脉构造的各单脉间为强烈交代蚀变的残留物,各单脉的形成温度相近。故认为矿脉是热液沿裂隙或节理交代围岩而成,复脉是由相邻单脉交代掉其间围岩联合而成。
The tungsten-tin-quartz vein of this deposit cuts through Devonian sand shale and carbonate rocks and is produced in a set of conjugate X-joints. The veins have a symmetrical banded structure that can be explained by the symbiosis of the account components. Calculations show that wolframite can also be formed in a calcium-rich environment. The composition of the complex pulse structure between the monolayers for the intense alteration of the remnants of the formation of each single pulse temperature is similar. Therefore, it is considered that the veins are hydrothermal fluids that are formed along the fissures or joints and are surrounded by the adjacent single veins.