摘要
仁差盆地是形成于中生代的典型的火山断陷盆地,区内断裂构造发育,火山活动频繁,成矿地质条件优越。通过岩矿鉴定,确定矿床岩石学、热液蚀变基本特征,分析其与铀矿关系。
Rencha Basin is a typical volcanic break basin formed in the Mesozoic.In the region,there are developed fault structures and frequent volcanic activities that have created favorable geological conditions for ore-forming.through appraise the rock and ore,determine the basic characteristic of petrology and hydrothermal alteration,analyse the relation of mineralization
出处
《四川建材》
2012年第6期128-129,136,共3页
Sichuan Building Materials
关键词
仁差盆地
铀矿床
岩石特征
Rencha basin
uranium deposit
rock characteristics
