Mid-ocean ridge and supra-subduction affinities in the Pindos ophiolites (Greece): Implications for magma genesis in a forearc setting

Lithos

Volumn 73, Issue 3-4, 2004, Pages 229-253

  Saccani, Emilio ^a   Photiades, Adonis ^b  

^a UNIVERSITY OF FERRARA   (Italy)

^b Inst of Geology/Mineral Exploration   (Greece)

Author keywords

Greece; Jurassic; MORB; Ophiolites; Petrogenesis; SSZ

Indexed keywords

FOREARC BASIN; FRACTIONAL CRYSTALLIZATION; MAGMATISM; MANTLE SOURCE; MID-OCEAN RIDGE BASALT; OPHIOLITE; SOURCE ROCK; SUBDUCTION;

EURASIA; EUROPE; GREECE; PINDUS MOUNTAINS; SOUTHERN EUROPE;

EID: 1842679123     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2003.12.002     Document Type: Article

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