Abstract

The metasomatic rocks of gold-ore deposits of the Auminzatau Mountains (Central Kyzylkum), which are similar in mineral composition and their features of the formation, are distinguished. The corresponding stages of ore mineralization are associated with certain types of metasomatic rocks, which are their typomorphic signs. They reflect the features of the evolution of the stages of a unified mineral-forming system, which can be used as search criteria.

中文翻译：

---

奥明扎托山（克孜勒库姆中部）金矿交代岩及其与成矿过程的联系

摘要

奥明扎托山脉（克孜勒库姆中部）金矿床的交代岩在矿物成分和形成特征上相似，具有明显的区别。矿石成矿的相应阶段与某些类型的交代岩有关，这是它们的标型标志。它们反映了统一成矿系统阶段演化的特征，可作为检索标准。