离子迁移假设与离子成矿说——以U、Th、K为例

Hypothesis of ion migration and ion metallogeny ——Taking U,Th,K as an example

地壳岩石中存在U、Th、K分布特征带,而传统理论无法解释这些特征带及其特征。根据岩石中存在着自由离子和3种电压,且这3种电压有随机械力加大而增高的性质提出了离子迁移假设,并对该假设进行了论证。从大量数据和图中提取U、Th、K分布特征带,根据特征带提出假设,再推理证明其假设成立。离子成矿说是建立在离子地质学基础上的成矿理论,认为成矿物质以离子形式迁移,通过化学反应沉淀富集,在有利地段形成矿床。提出了离子成矿说的5个法则。实践结果初步证明华南两研究区的离子成矿学说及推论是正确的。它们不仅能解释U、Th、K分布特征带及其特征,而且能解释化探找矿效果好的原因。

In the crust rocks of the earth, there occurs characteristic U, Th, K distribution belts, and it is very difficult to explain these belts and their features with traditional theories. The ion migration hypothesis is propesed in this paper based on the fact that there are free ions and three types of electronic voltages in the rock and that the voltage rises with the increase of mechanical power, and some arguments and reasons have been expound. The author makes the hypothesis on the belt characteristics extracted from lager amount data. Ion metallogeny is based on the metallogenetic theory, which is believed that the metallogenetic mass is migrated by forms of ion. They are precipitated and concentrated by chemical reaction, then form a deposit in favorable areas. The author provides five laws on ion metallogeny hypothesis. The practical results of two studied areas in southern China initially prove that ion metallogeny and its deduction are correct. The hypothesis explains not only the characteristic belts of U, Th, K distribution, but also the reason why the geochemical exploration method obtained is better effects in exploration.