{"title":"构造岩石物理分析方法在南乌拉尔珠萨块状硫化物矿床主岩及矿石变质作用评价中的应用","authors":"A. A. Burmistrov, I. Vikentyev, E. I. Yartsev","doi":"10.33623/0579-9406-2021-6-77-85","DOIUrl":null,"url":null,"abstract":"Based on a comparison of the chemical composition and a number of petrophysical and thermodynamic parameters of changed to varying degrees syn-ore and post-ore Devonian gabbroids of the Dzhusa pyrite-polymetallic deposit (South Ural), the principal possibility of quantifying the grade of their alteration and transformation related with the hydrothermal post-volcanic and dynamic metamorphism is shown.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"20 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-01-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Application of methods of structural petrophysical analysis for estimating metamorphogenic transformations of host rocks and ores of Dzhusa massive sulfide deposit (South Urals)\",\"authors\":\"A. A. Burmistrov, I. Vikentyev, E. I. Yartsev\",\"doi\":\"10.33623/0579-9406-2021-6-77-85\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Based on a comparison of the chemical composition and a number of petrophysical and thermodynamic parameters of changed to varying degrees syn-ore and post-ore Devonian gabbroids of the Dzhusa pyrite-polymetallic deposit (South Ural), the principal possibility of quantifying the grade of their alteration and transformation related with the hydrothermal post-volcanic and dynamic metamorphism is shown.\",\"PeriodicalId\":253271,\"journal\":{\"name\":\"Moscow University Bulletin. Series 4. Geology\",\"volume\":\"20 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-01-29\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Moscow University Bulletin. Series 4. Geology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.33623/0579-9406-2021-6-77-85\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Moscow University Bulletin. Series 4. Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.33623/0579-9406-2021-6-77-85","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Application of methods of structural petrophysical analysis for estimating metamorphogenic transformations of host rocks and ores of Dzhusa massive sulfide deposit (South Urals)
Based on a comparison of the chemical composition and a number of petrophysical and thermodynamic parameters of changed to varying degrees syn-ore and post-ore Devonian gabbroids of the Dzhusa pyrite-polymetallic deposit (South Ural), the principal possibility of quantifying the grade of their alteration and transformation related with the hydrothermal post-volcanic and dynamic metamorphism is shown.
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