Bimodality of lavas in the teide-pico viejo succession in tenerife-the role of crustal melting in the origin of recent phonolites

Journal of Petrology

Volumn 53, Issue 12, 2012, Pages 2465-2495

  Wiesmaier, Sebastian ^a,b,c   Troll, Valentin R ^c,d   Carracedo, Juan Carlos ^c   Ellam, Robert M ^e   Bindeman, Ilya ^f   Wolff, John A ^g  

^a TRINITY COLLEGE DUBLIN   (Ireland)

^b UNIVERSITY OF MUNICH   (Germany)

^c UNIVERSITY OF LAS PALMAS DE GRAN CANARIA   (Spain)

^d UPPSALA UNIVERSITY   (Sweden)

^e SCOTTISH UNIVERSITIES ENVIRONMENTAL RESEARCH CENTRE   (United Kingdom)

^f UNIVERSITY OF OREGON   (United States)

^g WASHINGTON STATE UNIVERSITY   (United States)

Author keywords

Anatexis; Crustal melting; Daly gap; Ocean island evolution; Phonolite; Teide

Indexed keywords

ANATEXIS; BIMODAL ASSOCIATION; ISOTOPIC COMPOSITION; LAVA; MAGMATIC DIFFERENTIATION; OCEAN ISLAND BASALT; PHONOLITE; TRACE ELEMENT;

CANARY ISLANDS; PICO VIEJO; SANTA CRUZ DE TENERIFE [(PRV) CANARY ISLANDS]; SPAIN; TEIDE; TENERIFE;

EID: 84869995924     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egs056     Document Type: Article

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