此外，铀的吸附作用也是重要的成矿作用。

In addition, adsorption of uranium is also thought of an important mineralization.

其成矿作用主要受二叠纪火山岩相及火山机构控制。

The metallization is controlled by the Permian volcanic lithofacies and volcanic edifice.

铌、稀土成矿作用与脉状、瘤状碳酸岩有关。

The niobium rare earth mineralization was concerned with tumour carbonatite.

稳定同位素测年信息，是深部构造、成矿作用和地层年代学的重要依据。

The information of stable isotopic aging is the important basis for the deep structures, mineralization and chronostratigraphy.

此巨型成矿域以发育中、晚元古代及晚古生代成矿作用为其特点。

This metallogenic province is characterized by the Mid-Late Proterozoic and the Late Paleaozoic mineralizations.