东萨延蛇绿岩带奥帕-基托伊地块超基岩多组分矿石成矿作用:形成副长岩及其成因(金刚石、软玉、贵金属、铬、镍)

{"title":"东萨延蛇绿岩带奥帕-基托伊地块超基岩多组分矿石成矿作用:形成副长岩及其成因(金刚石、软玉、贵金属、铬、镍)","authors":"A. V. Tatarinov, L. I. Yalovik","doi":"10.4236/gm.2021.114005","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":67978,"journal":{"name":"地质材料(英文)","volume":"1 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Multicomponent Ore Mineralization in Ultrabasites of the Ospa-Kitoy Massif of the East Sayan Ophiolite Belt: Formational Parageneses and Origin (Diamond, Nephrite, Noble Metals, Chromium, Nickel)\",\"authors\":\"A. V. Tatarinov, L. I. Yalovik\",\"doi\":\"10.4236/gm.2021.114005\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":67978,\"journal\":{\"name\":\"地质材料(英文)\",\"volume\":\"1 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"地质材料(英文)\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.4236/gm.2021.114005\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"地质材料(英文)","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.4236/gm.2021.114005","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}