矿体呈层状、似层状和透镜状。
The orebody appears in bedded, near bedded and lenticular shapes.
矿体受层滑断层控制呈层状、似层状。
The strata form and quasi strata form ore bodies are controlled by strike slip faults.
研究表明该夕卡岩的主要特征为：（1）呈层状、似层状赋存于碳酸盐岩和细碎屑岩接触带，产状与地层一致；
The main characteristics of the skarn are as follows:(1)occurring as bedded, para-bedded in the contact zone between carbonate and microclastic rock, and its occurrence being accordance to the strata;
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