Isotope and geochemical evidence for the influence of ore-bearing solutions on basic dykes of the Dal'negorskii ore region.

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.