Geochemical and isotopic constraints on the petrogenesis of Early Ordovician granodiorite and Variscan two-mica granites from the Gouveia area, central Portugal

Lithos

Volumn 111, Issue 3-4, 2009, Pages 186-202

  Neiva, A M R ^a   Williams, I S ^b   Ramos, J M F ^c   Gomes, M E P ^d   Silva, M M V G ^a   Antunes, I M H R ^e  

^a UNIVERSITY OF COIMBRA   (Portugal)

^b AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^c INETI   (Portugal)

^d UNIVERSITY OF TRÁS OS MONTES AND ALTO DOURO   (Portugal)

^e INSTITUTO POLITÉCNICO DE CASTELO BRANCO   (Portugal)

Author keywords

Fractional crystallization; Geochemistry; Geochronology; Granite; Isotopes; Tin

Indexed keywords

BIOTITE; FRACTIONAL CRYSTALLIZATION; GEOCHRONOLOGY; GRANITE; GRANODIORITE; IGNEOUS GEOCHEMISTRY; ISOTOPIC COMPOSITION; MICA; MONAZITE; ORDOVICIAN; PARTIAL MELTING; PETROGENESIS; SHRIMP DATING; TIN; URANIUM-LEAD DATING; ZIRCON;

PORTUGAL;

MICAS;

EID: 78549266173     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2009.01.005     Document Type: Article

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