A. N. Glukhov, V. V. Priymenko, M. I. Fomina, V. V. Akinin
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引用次数: 0

摘要

本文介绍了奥莫伦地块孔金岩浆岩带中斑岩-铜、金银和银多金属矿的地质、矿物学和地球化学的新资料以及与之相关的花岗岩类。岩石学特征和花岗岩年龄与OCVB Penzhina段相似。孔金带的成矿作用与OCVB非常接近,不同之处在于斑岩铜矿石中Mo含量相对较高,银多金属成矿作用大于金银。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Металлогения Конгинской зоны Омолонского террейна (Северо-Восток Азии)
The article presents new data on geology, mineralogy, and geochemistry of porphyry-copper, gold-silver, and silver-polymetallic ore occurrences in the Kongin magmatic zone of the Omolon terrane and granitoids, associated with it. It has been demonstrated that petrology and the age of granitoids are similar to those in the OCVB Penzhina segment. Mineralization of the Kongin zone is very close to that of the OCVB, differing in relatively high Mo in porphyry-copper ores and prevalence of silver-polymetallic mineralization over gold-silver.
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