I. Garrido, J. Cembrano, Armando Sina, P. Stedman, G. Yáñez
{"title":"Respuesta al Comentario de F. Munizaga al artículo“高岩浆氧化状态和整体地壳缩短:安第斯斑岩铜矿成因的关键因素,智利中部(31-34°S)”,de Garrido et al. (2002)","authors":"I. Garrido, J. Cembrano, Armando Sina, P. Stedman, G. Yáñez","doi":"10.4067/S0716-02082003000100010","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":140719,"journal":{"name":"Revista Geologica De Chile","volume":"22 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2003-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Respuesta al Comentario de F. Munizaga al artículo 'High magma oxidation state and bulk crustal shortening: key factors in the genesis of Andean porphyry copper deposits, central Chile (31-34°S)', de Garrido et al. (2002)\",\"authors\":\"I. Garrido, J. Cembrano, Armando Sina, P. Stedman, G. Yáñez\",\"doi\":\"10.4067/S0716-02082003000100010\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":140719,\"journal\":{\"name\":\"Revista Geologica De Chile\",\"volume\":\"22 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2003-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Revista Geologica De Chile\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4067/S0716-02082003000100010\",\"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/S0716-02082003000100010","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Respuesta al Comentario de F. Munizaga al artículo 'High magma oxidation state and bulk crustal shortening: key factors in the genesis of Andean porphyry copper deposits, central Chile (31-34°S)', de Garrido et al. (2002)