Tectonic and climate history influence the geochemistry of large-volume silicic magmas: New δ18O data from the Central Andes with comparison to N America and Kamchatka

Journal of Volcanology and Geothermal Research

Volumn 262, Issue , 2013, Pages 90-103

  Folkes, Chris B ^a   de Silva, Shanaka L ^b   Bindeman, Ilya N ^c   Cas, Raymond A F ^a  

^a MONASH UNIVERSITY   (Australia)

^b OREGON STATE UNIVERSITY   (United States)

^c UNIVERSITY OF OREGON   (United States)

Author keywords

Central Andes; Crustal assimilation; Hydrothermal alteration; Ignimbrites; North America; Oxygen isotopes; Paleoclimate; Paleoelevation

Indexed keywords

CENTRAL ANDES; CRUSTAL ASSIMILATION; HYDROTHERMAL ALTERATIONS; IGNIMBRITES; NORTH AMERICA; OXYGEN ISOTOPES; PALEOCLIMATES; PALEOELEVATION;

GLACIAL GEOLOGY; ISOTOPES; LEAD; QUARTZ; SILICATE MINERALS;

VOLCANOES;

CRUSTAL STRUCTURE; ELEVATION; GLACIATION; HYDROTHERMAL ALTERATION; IGNIMBRITE; ISOTOPIC COMPOSITION; MAGMA CHEMISTRY; OXYGEN ISOTOPE; PALEOCLIMATE; TECTONIC STRUCTURE;

ANDES; KAMCHATKA; NORTH AMERICA; RUSSIAN FEDERATION;

EID: 84881241324     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2013.05.014     Document Type: Article

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