“浅成低温热液铀矿床”的概念及有关问题

• 作 者: 季弗鲁瓦(J.Jeffroy) 沙尔西亚(J.A.Sarcia) 张待时
• 出 处: 铀矿地质
• 发表日期: 1964年02期
• 关键词: 铀矿床 低温热液 铀矿地质学 矿床 矿脉 矿床成因 利木赞 地质特点 花岗岩 一篇

根据目前已有资料的对比,法国、葡萄牙、西班牙一带(即中欧地块)的热液铀矿床和常见的一些矿床有一系列相似的地质特点,另外他们对这种类型矿床成因的看法在许多方面会给我们以启发,因此特意选登这篇文章,供读者们参考。我们在1962年第3期副刊上刊登了另外两篇法文文章(鲁包等人一篇和季弗鲁瓦等人一篇)也是基于同一理由。这三篇文章大体上可以代表法国铀矿地质学界目前的认识水平。

Based on the available data, there are a series of similar geological features of hydrothermal uranium deposits and some common deposits in France, Portugal and Spain (ie, the Central Europe block). In addition, their views on the genesis of this type of deposit are in many respects Will give us inspiration, so deliberately selected this article for readers reference. We also published two other French articles in the 3rd Supplement, 1962 (one by Lu Ba et al and one by Ji Fulu Wa et al.) For the same reason. These three articles generally represent the current level of understanding of the French uranium geology community.