{"title":"意大利西北部阿亚斯谷Brusson金石英脉的K-Ar辐射年龄:阿尔卑斯西北部中渐新世热液活动的证据","authors":"L. Diamond, M. Wiedenbeck","doi":"10.7892/BORIS.90851","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":407711,"journal":{"name":"Schweizerische Mineralogische Und Petrographische Mitteilungen","volume":"44 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"22","resultStr":"{\"title\":\"K-Ar radiometric ages of the gold-quartz veins at Brusson, Val d'Ayas, NW Italy: evidence of mid-Oligocene hydrothermal activity in the Northwestern Alps\",\"authors\":\"L. Diamond, M. Wiedenbeck\",\"doi\":\"10.7892/BORIS.90851\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":407711,\"journal\":{\"name\":\"Schweizerische Mineralogische Und Petrographische Mitteilungen\",\"volume\":\"44 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"22\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Schweizerische Mineralogische Und Petrographische Mitteilungen\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.7892/BORIS.90851\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Schweizerische Mineralogische Und Petrographische Mitteilungen","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.7892/BORIS.90851","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
K-Ar radiometric ages of the gold-quartz veins at Brusson, Val d'Ayas, NW Italy: evidence of mid-Oligocene hydrothermal activity in the Northwestern Alps