瑞典Väster Silvberg和蒙古Tumurtijn-ovoo夕卡岩矿床矿物组成:海底热液-沉积矿床成因中不同元素供应的指示

{"title":"瑞典Väster Silvberg和蒙古Tumurtijn-ovoo夕卡岩矿床矿物组成:海底热液-沉积矿床成因中不同元素供应的指示","authors":"W. Gottesmann, B. Gottesmann","doi":"10.1127/njma/2019/0123","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":"36 1","pages":"135-148"},"PeriodicalIF":0.5000,"publicationDate":"2019-11-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Composition of minerals from the skarn deposits Väster Silvberg (Sweden) and Tumurtijn-ovoo (Mongolia): Indications of different element supply in submarine hydrothermal-sedimentary ore genesis\",\"authors\":\"W. Gottesmann, B. Gottesmann\",\"doi\":\"10.1127/njma/2019/0123\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":51139,\"journal\":{\"name\":\"Neues Jahrbuch Fur Mineralogie-Abhandlungen\",\"volume\":\"36 1\",\"pages\":\"135-148\"},\"PeriodicalIF\":0.5000,\"publicationDate\":\"2019-11-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Neues Jahrbuch Fur Mineralogie-Abhandlungen\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1127/njma/2019/0123\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"MINERALOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1127/njma/2019/0123","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"MINERALOGY","Score":null,"Total":0}