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Volumn 119, Issue 5, 2011, Pages 521-534

Petrogenesis of Ordovician magmatism in the Pyrenees (Albera and Canigó massifs) determined on the basis of zircon minor and trace element composition

Author keywords

[No Author keywords available]

Indexed keywords

AMPHIBOLITE; CHEMICAL COMPOSITION; FRACTIONAL CRYSTALLIZATION; GEOCHEMISTRY; GNEISS; MAGMATISM; NEODYMIUM ISOTOPE; ORDOVICIAN; PETROGENESIS; PLAGIOCLASE; STRONTIUM ISOTOPE; TRACE ELEMENT; ZIRCON;

EID: 79960974474     PISSN: 00221376     EISSN: None     Source Type: Journal    
DOI: 10.1086/660889     Document Type: Article
Times cited : (31)

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