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The article focuses on the formation of rich datolite ores on the Dalnegorskoe skarn borosilicate deposit located in the center of the ore region, Russia. It states that this formation is interrupted by Altered basalts, alkaline basalts, and gabbro from dykes. It mentions that rocks of the ore zone has acquired a low oxygen isotope composition which resulted in the postmagnetic interaction with waters of meteoric origin. It also mentions that the Dal'negorskii ore region is known for its skarn and vein polymetallic deposits.

The article focuses on the zones of paleospreading and crustal extension in the Ural Mountains, Russia runs from north to south through western Russia. It states that the fragments of the sheeted dyke complex extends with breaks over 60 kilometers in the eastern framework of the Revda massif, Urals Region, Russia. It mentions that these dykes are made of fine grained gabbrodolerites and porphyritic dolerites with plagioclase and hornblende phenocrysts, as well as less common aphyric and fine porphyritic varieties.