The diversity and geodynamic significance of Late Cambrian (ca. 500 Ma) felsic anorogenic magmatism in the northern part of the Bohemian Massif: A review based on Sm-Nd isotope and geochemical data

Special Paper of the Geological Society of America

Volumn 423, Issue , 2007, Pages 209-229

  Pin, Christian ^a   Kryza, R ^b   Oberc Dziedzic, T P ^b   Mazur, S ^b   Turniak, K ^b   Waldhausrová, Jarmila ^c  

^a UNIVERSITÉ BLAISE PASCAL   (France)

^b UNIVERSITY OF WROC AW   (Poland)

^c Nad Hercovkow 422   (Czech Republic)

Author keywords

A type; Fertility; Geochemistry; Granitoids; Partial melting

Indexed keywords

BINARY ALLOYS; GEOCHEMISTRY; GEODYNAMICS; ISOTOPES; LITHOLOGY; MELTING; NEODYMIUM ALLOYS; SAMARIUM ALLOYS; STRUCTURAL GEOLOGY;

A-TYPE; CONTINENTAL BREAK-UP; CONTINENTAL LITHOSPHERE; EXTENSIONAL TECTONICS; FERTILITY; GRANITOIDS; MANTLE DERIVED MAGMAS; PARTIAL MELTING;

IGNEOUS ROCKS;

ADVECTION; CADOMIAN OROGENY; CAMBRIAN; CONTINENTAL LITHOSPHERE; DEHYDRATION MELTING; FELSIC ROCK; FERTILITY; GEOCHEMICAL METHOD; IGNEOUS PROVINCE; LOWER CRUST; MAGMATISM; MANTLE; PARTIAL MELTING;

BOHEMIAN MASSIF;

TRACHYTES;

EID: 55549104131     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2007.2423(09)     Document Type: Conference Paper

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