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)

Munoz, M.; Charrier, R.; Fanning, C. Mark; Maksaev, V; Deckart, K.

Abstract

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.

Más información

Título según WOS: 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 (vol 53, egs010, 2012)
Título según SCOPUS: ID SCOPUS_ID:85129264506 Not found in local SCOPUS DB
Título de la Revista: JOURNAL OF PETROLOGY
Volumen: 63
Editorial: OXFORD UNIV PRESS
Fecha de publicación: 2022
DOI:

10.1093/PETROLOGY/EGAC030

Notas: ISI, SCOPUS