REE, Y, Nb, U, and Th contents and tetrad effect in zircon from a magmatic-hydrothermal F-rich system of Sn-rare metal-cryolite mineralized granites from the Pitinga Mine, Amazonia, Brazil

Journal of South American Earth Sciences

Volumn 33, Issue 1, 2012, Pages 34-42

  Nardi, Lauro V S ^a   Formoso, Milton L L ^a   Jarvis, Kym ^b   Oliveira, Leondres ^a   Bastos Neto, Artur C ^a   Fontana, Eduardo ^a  

^a FEDERAL UNIVERSITY OF RIO GRANDE DO SUL   (Brazil)

^b IMPERIAL COLLEGE LONDON   (United Kingdom)

Author keywords

M type REE patterns; REE zircon chemistry; Tetrad effect; Trace elements in magmatic systems; Zircon chemistry; Zircon in hydrothermal systems; Zircon partition coefficient

Indexed keywords

AMPHIBOLE; BIOTITE; CHEMICAL COMPOSITION; CONCENTRATION (COMPOSITION); CRYSTALLIZATION; GEOCHEMISTRY; GRANITE; IGNEOUS GEOCHEMISTRY; METALLOGENESIS; NIOBIUM; ORE DEPOSIT; PARTITION COEFFICIENT; PETROGENESIS; PROVENANCE; RARE EARTH ELEMENT; THORIUM; TIN; TRACE ELEMENT; URANIUM; YTTRIUM; ZIRCON;

AMAZONAS [BRAZIL]; BRAZIL;

EID: 80053340795     PISSN: 08959811     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsames.2011.07.004     Document Type: Article

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