Abstract

Summary Modeling has been carried out on the basis of the structural mapped of the folded structures of the Teutedzhak gold ore field in the back-arc zone of the Okhotsk-Chukotka volcanogenic belt. According to the structural position, three generations of intrusions have been divided: pre-ore sills, possibly ore-controlling granodiorites and diorites and post-ore granitoid dikes. Based on the analysis of fracturing and orientation of quartz veinlets, it was concluded that there is a series of ore-bearing stockworks of northwestern strike in the ore field.

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