Erratum: Zircon Trace Element and O-Hf Isotope Analyses of Mineralized Intrusions from El Teniente Ore Deposit, Chilean Andes: Constraints on the Source and Magmatic Evolution of Porphyry Cu-Mo Related Magmas (Journal of Petrology (2012) 53:6 (egs010) DOI: 10.1093/petrology/egs010)

M. Muñoz, R. Charrier, C. M. Fanning, V. Maksaev, K. Deckart

Resultado de la investigación: Contribución a una revistaComentario/Debaterevisión exhaustiva

Resumen

In the original article, the words mantle source appear in two places by mistake: Page 1108 (right column, end of first paragraph) and Page 1110 (left column, end of second paragraph). These two occurrences should read as magmatic source. In the Conclusions section, number (4), the words Hf isotopic composition is inferred to fingerprint the source and O the isotope composition of the melting process should read as Hf isotopic composition is inferred to fingerprint the source, while O the melting process. These details have been corrected only in this corrigendum to preserve the published version of record.

Idioma originalInglés
Número de artículoegac030
PublicaciónJournal of Petrology
Volumen63
N.º4
DOI
EstadoPublicada - 1 abr. 2022
Publicado de forma externa

Áreas temáticas de ASJC Scopus

  • Geofísica
  • Geoquímica y petrología

Huella

Profundice en los temas de investigación de 'Erratum: Zircon Trace Element and O-Hf Isotope Analyses of Mineralized Intrusions from El Teniente Ore Deposit, Chilean Andes: Constraints on the Source and Magmatic Evolution of Porphyry Cu-Mo Related Magmas (Journal of Petrology (2012) 53:6 (egs010) DOI: 10.1093/petrology/egs010)'. En conjunto forman una huella única.

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