{"title":"关于欧莫隆·特伦(亚洲北部)贵金属和有色金属的矿质形式","authors":"A. N. Glukhov","doi":"10.34078/1814-0998-2021-3-18-33","DOIUrl":null,"url":null,"abstract":"The author characterizes gold, silver, copper, lead, and zinc deposits developed within the Omolon craton terrane. Outlined are ore formations (genetic types) including the deposits. The principal features of the terrane metallogeny terrane are shown as determined by the stable structure of the crystalline basement, consolidated in Early Precambrian, which resulted in contraction of the range of mineralization genetic types and in formation of deep ore- and magma-controlling faults and large deposits.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"49 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"К вопросу о рудных формациях благородных и цветных металлов Омолонского террейна (Cеверо-Восток Азии)\",\"authors\":\"A. N. Glukhov\",\"doi\":\"10.34078/1814-0998-2021-3-18-33\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The author characterizes gold, silver, copper, lead, and zinc deposits developed within the Omolon craton terrane. Outlined are ore formations (genetic types) including the deposits. The principal features of the terrane metallogeny terrane are shown as determined by the stable structure of the crystalline basement, consolidated in Early Precambrian, which resulted in contraction of the range of mineralization genetic types and in formation of deep ore- and magma-controlling faults and large deposits.\",\"PeriodicalId\":341033,\"journal\":{\"name\":\"Bulletin of the North-East Science Center\",\"volume\":\"49 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-09-30\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Bulletin of the North-East Science Center\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.34078/1814-0998-2021-3-18-33\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of the North-East Science Center","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.34078/1814-0998-2021-3-18-33","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
К вопросу о рудных формациях благородных и цветных металлов Омолонского террейна (Cеверо-Восток Азии)
The author characterizes gold, silver, copper, lead, and zinc deposits developed within the Omolon craton terrane. Outlined are ore formations (genetic types) including the deposits. The principal features of the terrane metallogeny terrane are shown as determined by the stable structure of the crystalline basement, consolidated in Early Precambrian, which resulted in contraction of the range of mineralization genetic types and in formation of deep ore- and magma-controlling faults and large deposits.
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