Abstract

Sulfide-free mineral assemblages with the chalcophile element minerals from occurrences associated with altered rocks of Pelagonian massif, Republic of North Macedonia have been studied. The inputting sequence of various ore-forming constituents has been revealed on the basis of morphological features, zoning of the spinel-group minerals, and the högbomite supergroup minerals. Conclusions about the inputting consequences of various ore-forming components have shown that these minerals easily form epitaxial and syntaxial intergrowths with each other and with nežilovite due to commensurable unit cell parameters. Some potentially new minerals were identified belonging to the högbomite supergroup.

中文翻译：

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北马其顿共和国Pelagonian地块中无硫化物的内生Pb–Zn–Sb–As组合的尖晶石和Högbomite-Supergroup矿物

摘要

已经研究了与北马其顿共和国Pelagonian断层岩石蚀变有关的事件中无硫化物与硫属元素元素矿物的组合。根据形态特征，尖晶石族矿物的分区和菱镁矿超族矿物，揭示了各种成矿成分的输入顺序。关于各种成矿成分输入后果的结论表明，由于可比的晶胞参数，这些矿物很容易彼此之间以及与新硅铁矿形成外延和句法共生。确定了一些潜在的新矿物，它们属于白钨矿超群。