刘等人的“平衡橄榄石熔体镁同位素分馏解释了弧熔岩中高δ26Mg值”更正，2022

{"title":"刘等人的“平衡橄榄石熔体镁同位素分馏解释了弧熔岩中高δ26Mg值”更正，2022","authors":"X.-N. Liu, R. Hin, C. Coath, M. van Soest, E. Melekhova, T. Elliott","doi":"10.7185/geochemlet.2226cor","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":12613,"journal":{"name":"Geochemical Perspectives Letters","volume":" ","pages":""},"PeriodicalIF":3.4000,"publicationDate":"2022-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Corrigendum to “Equilibrium olivine-melt Mg isotopic fractionation explains high δ26Mg values in arc lavas” by Liu et al., 2022\",\"authors\":\"X.-N. Liu, R. Hin, C. Coath, M. van Soest, E. Melekhova, T. Elliott\",\"doi\":\"10.7185/geochemlet.2226cor\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":12613,\"journal\":{\"name\":\"Geochemical Perspectives Letters\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":3.4000,\"publicationDate\":\"2022-08-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geochemical Perspectives Letters\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.7185/geochemlet.2226cor\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochemical Perspectives Letters","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.7185/geochemlet.2226cor","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}