The peralkaline tin-mineralized madeira cryolite albite-rich granite of pitinga, amazonian craton, brazil: Petrography, mineralogy and crystallization processes

Canadian Mineralogist

Volumn 47, Issue 6, 2009, Pages 1301-1327

  Costi, Hilton Tulio ^a   Dall'Agnol, Roberto ^a   Pichavant, Michel ^b   Rämö, Osmo Tapani ^c  

^a FEDERAL UNIVERSITY OF PARÁ   (Brazil)

^b UMR 7327   (France)

^c UNIVERSITY OF HELSINKI   (Finland)

Author keywords

Albite rich subsolvus granite; Brazil; Cryolite; Immiscibility; Madeira granite; Niobium; Peralkaline; Pitinga mine; Tin

Indexed keywords

ALBITE-RICH SUBSOLVUS GRANITE; BRAZIL; CRYOLITE; IMMISCIBILITY; PERALKALINE;

CRYSTALLIZATION; CRYSTALLOGRAPHY; FELDSPAR; GALLIUM; HALIDE MINERALS; MINERALOGY; MINERALS; MINING; NIOBIUM; OXIDE MINERALS; PETROGRAPHY; QUARTZ; RUBIDIUM; SILICATE MINERALS; TIN; TITANIUM COMPOUNDS;

GRANITE;

A-TYPE ROCK; CRYOLITE; CRYSTALLIZATION; FELDSPAR GROUP; IGNEOUS GEOCHEMISTRY; IMMISCIBILITY; MAGMATISM; MELT; MINERALOGY; NIOBIUM; PERALKALINE ROCK; PETROGRAPHY; QUARTZ; TIN;

AMAZONAS [BRAZIL]; BRAZIL; PITINGA MINE;

EID: 77249158399     PISSN: 00084476     EISSN: None     Source Type: Journal    
DOI: 10.3749/canmin.47.6.1301     Document Type: Article

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