Mantle source characteristics and melting models for the early-middle Miocene mafic volcanism in Western Anatolia: Implications for enrichment processes of mantle lithosphere and origin of K-rich volcanism in post-collisional settings

Journal of Volcanology and Geothermal Research

Volumn 198, Issue 1-2, 2010, Pages 112-128

  Ersoy, E Yalççn ^a   Helvac, Cahit ^a   Palmer, Martin R ^b  

^a DOKUZ EYLUL UNIVERSITY   (Turkey)

^b UNIVERSITY OF SOUTHAMPTON   (United Kingdom)

Author keywords

Neogene volcanism; Shoshonitic volcanism; Subduction enrichment; Ultrapotassic volcanism; Western Anatolia

Indexed keywords

NEO GENES; SHOSHONITIC VOLCANISM; SUBDUCTION ENRICHMENT; ULTRAPOTASSIC VOLCANISM; WESTERN ANATOLIA;

AGRICULTURAL CHEMICALS; EARTHQUAKE EFFECTS; ISOTOPES; MELTING; NEODYMIUM; ROCKS; SEDIMENTOLOGY; SILICON COMPOUNDS; SOLVENTS; STRONTIUM; TECTONICS; TRACE ELEMENTS; VOLCANOES;

VOLCANIC ROCKS;

DETACHMENT FAULT; EXHUMATION; LITHOSPHERIC STRUCTURE; MAFIC ROCK; MAGMATISM; MANTLE SOURCE; MELTING; MIOCENE; NUMERICAL MODEL; POTASSIC ROCK; SHOSHONITE; SUBDUCTION; TRACE ELEMENT; VOLCANISM;

ANATOLIA; TURKEY;

EID: 78649448994     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2010.08.014     Document Type: Article

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