摘要
本文以贵州晴隆大厂锑矿床为例、试说明在具层间古喀斯特的条件下,宽缓褶曲中的层间滑动构造。
Citing the Dechang antimony ore deposit as an example,the writers try to explain the bedding glide structure formed in the wide and slow fold under the condition of ancient karst,and the secondary structure formed in the process of folding and bedded gliding,and the relation between the structnres mentioned above and their metallogeny.
基金
国家自然科学基金
关键词
锑矿
古喀斯特
层滑构造
成矿
ancient karst
bedded gliding structure
secondary structure
