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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