{"title":"对智利北部(18-22°S)新生代岩浆岩年代学(Ar-Ar、K-Ar和he暴露年龄)的评论:对安第斯山脉中部岩浆作用和构造演化的启示Wörner等(2000)","authors":"Marcelo H. García, G. Hérail","doi":"10.4067/S0716-02082001000100008","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":140719,"journal":{"name":"Revista Geologica De Chile","volume":"22 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2001-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"23","resultStr":"{\"title\":\"Comment on 'Geochronology (Ar-Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from northern Chile (18-22°S): implications for magmatism and tectonic evolution of the central Andes' of Wörner et al. (2000)\",\"authors\":\"Marcelo H. García, G. Hérail\",\"doi\":\"10.4067/S0716-02082001000100008\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":140719,\"journal\":{\"name\":\"Revista Geologica De Chile\",\"volume\":\"22 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"23\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Revista Geologica De Chile\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4067/S0716-02082001000100008\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Revista Geologica De Chile","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4067/S0716-02082001000100008","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Comment on 'Geochronology (Ar-Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from northern Chile (18-22°S): implications for magmatism and tectonic evolution of the central Andes' of Wörner et al. (2000)