Fe-Ti-P oxide melts generated through magma mixing in the Antauta subvolcanic center, Peru: Implications for the origin of Nelsonite and iron oxide-dominated hydrothermal deposits

Economic Geology

Volumn 99, Issue 2, 2004, Pages 377-395

  Clark, Alan H ^a   Kontak, Daniel J ^b  

^a QUEEN S UNIVERSITY   (Canada)

^b Nova Scotia Dept of Natural Rsrc   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

HYBRIDIZATION; MAGMA MIXING; PARTIAL CRYSTALLIZATION;

COMPOSITION; CRYSTALLIZATION; GRANITE; MINERALS; OXIDATION; QUARTZ;

GEOLOGY;

HYDROTHERMAL DEPOSIT; IRON; MINERALIZATION; MIXING; NELSONITE; OXIDE; PETROGENESIS; PETROLOGY; TITANIUM;

PERU; PUNO [PERU]; SOUTH AMERICA;

EID: 3342949988     PISSN: 03610128     EISSN: None     Source Type: Journal    
DOI: 10.2113/gsecongeo.99.2.377     Document Type: Article

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