Sr-Nd-Pb-O isotopic evidence for decreasing crustal contamination with ongoing magma evolution at Alicudi volcano (Aeolian arc, Italy): Implications for style of magma-crust interaction and for mantle source compositions

Lithos

Volumn 78, Issue 1-2, 2004, Pages 217-233

  Peccerillo, Angelo ^a   Dallai, Luigi ^b,e   Frezzotti, Maria Luce ^c   Kempton, Pamela D ^d  

^a UNIVERSITY OF PERUGIA   (Italy)

^b SAPIENZA UNIVERSITY OF ROME   (Italy)

^c UNIVERSITY OF SIENA   (Italy)

^d NATURAL ENVIRONMENT RESEARCH COUNCIL   (United Kingdom)

^e CNR   (Italy)

Author keywords

Aeolian arc; Alicudi; Calcalkaline magma; Crustal assimilation; Oxygen isotopes; Radiogenic isotopes; Tyrrhenian Sea

Indexed keywords

BASALT; CRUSTAL CONTAMINATION; ISOTOPIC COMPOSITION; MAGMA CHEMISTRY; MANTLE SOURCE;

EID: 4544359388     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2004.04.040     Document Type: Article

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