In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 24, No. 11 ( 2023-11)
Abstract:
Geochemical and isotopic monitoring of Peteroa volcano allowed us to elaborate a conceptual model that explains the evolution of the magmatic‐hydrothermal system Fumarolic gases exhibit different compositions during quiescent and unrest/eruptive periods, allowing the identification of precursory signals of the last eruption Despite variations in activity, the deep magmatic gas source of Peteroa volcano remained relatively constant, as indicated by consistent He and C isotopic values
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2023GC011064
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2023
detail.hit.zdb_id:
2027201-7
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