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高加索现代成矿分区图,是根据地壳上大型地块:斯基夫地块,外高加索中央地块和伊朗中央地块的划分原则而编制出来的。上述地块之间发育有优地槽拗陷带—山前海西奥菲奥岩带和位于斯基夫地块和外高加索地块之间的大高加索南坡早阿尔卑期奥菲奥岩带,以及阿尔卑斯谢万湖亚科林奥菲奥岩带,它位于外高加索地块和伊朗地块之间。奥菲奥岩带的早期发展阶段可能是属于裂谷带,而晚期发展阶段则属于地槽带。随着巨厚沉积物的堆积,这些地带在周围地块运动的影响
The modern Caucasus metallogenic zoning map is based on the principle of the division of large-scale crustal blocks on the crust: the Siskiv block, the outer Caucasus central block and the Iranian central block. Well-developed trough-depressions-piedmont Hessio-Olympio rock belt and the Greater Alpes-Pospole Ophiot rock belt located between the Squif and the Caucasus massif , As well as the Alpine Shevchenko-Arrecife Rock Belt, located between the Transcaucasia and Iranian plots. The early stage of development of the Orofio rock belt may belong to the rift zone, while the late stage of development belongs to the zone of the earth. With the accumulation of thick sediments, the impact of these zones on the movement of the surrounding land