Podiform chromitites and mantle peridotites of the Antalya ophiolite, Isparta Angle (SW Turkey): Implications for partial melting and melt-rock interaction in oceanic and subduction-related settings

Lithos

Volumn 114, Issue 3-4, 2010, Pages 307-326

  Caran, Şemsettin ^a   Çoban, Hakan ^a   Flower, Martin F J ^b   Ottley, Chris J ^c   Yilmaz, Kamil ^a  

^a SULEYMAN DEMIREL UNIVERSITY   (Turkey)

^b UNIVERSITY OF ILLINOIS AT CHICAGO   (United States)

^c DURHAM UNIVERSITY   (United Kingdom)

Author keywords

Antalya ophiolite; Dunite envelope; Harzburgite; Isparta Angle; Podiform chromitite; Spinel lherzolite

Indexed keywords

CHROMITITE; DISSOLUTION; DUNITE; FUGACITY; HARZBURGITE; IGNEOUS GEOCHEMISTRY; LHERZOLITE; OCEAN BASIN; OPHIOLITE; PARTIAL MELTING; PETROGRAPHY; SPINEL; SUBDUCTION ZONE; TECTONIC SETTING;

TURKEY;

EID: 74149093192     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2009.09.006     Document Type: Article

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