加拿大新不伦瑞克省中部 Burnthill Brook 地区花岗岩岩石的 U-Pb 和 Re-Os 地球年代学及岩石地球化学：对关键矿产勘探的影响

{"title":"加拿大新不伦瑞克省中部 Burnthill Brook 地区花岗岩岩石的 U-Pb 和 Re-Os 地球年代学及岩石地球化学：对关键矿产勘探的影响","authors":"N. Mohammadi, David R. Lentz, K. Thorne, Jim Walker, Neil Rogers, Brian L. Cousens, C. McFarlane","doi":"10.1016/j.chemer.2024.126087","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":12522,"journal":{"name":"Geochemistry","volume":"60 10","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"U-Pb and Re-Os geochronology and lithogeochemistry of granitoid rocks from the Burnthill Brook area in central New Brunswick, Canada: Implications for critical mineral exploration\",\"authors\":\"N. Mohammadi, David R. Lentz, K. Thorne, Jim Walker, Neil Rogers, Brian L. Cousens, C. McFarlane\",\"doi\":\"10.1016/j.chemer.2024.126087\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":12522,\"journal\":{\"name\":\"Geochemistry\",\"volume\":\"60 10\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-02-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geochemistry\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1016/j.chemer.2024.126087\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochemistry","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1016/j.chemer.2024.126087","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}