Petrogenesis of dacite in an oceanic subduction environment: Raoul Island, Kermadec arc

Journal of Volcanology and Geothermal Research

Volumn 156, Issue 3-4, 2006, Pages 252-265

  Smith, Ian E M ^a   Worthington, Timothy J ^a   Price, Richard C ^b   Stewart, Robert B ^c   Maas, R ^d  

^a UNIVERSITY OF AUCKLAND   (New Zealand)

^b UNIVERSITY OF WAIKATO   (New Zealand)

^c MASSEY UNIVERSITY   (New Zealand)

^d LA TROBE UNIVERSITY   (Australia)

Author keywords

crustal anatexis; dacite; fractional crystallisation; Kermadec arc; oceanic subduction

Indexed keywords

COMPOSITION; CRYSTALLIZATION; DEHYDRATION; FRACTIONATION; MAGNETITE; VOLCANIC ROCKS; VOLCANOES;

CALDERA FORMATION; CRUSTAL ANATEXIS; DACITE; OCEANIC SUBDUCTION; SILICEOUS MELTS;

PETROLOGY;

ANATEXIS; CALDERA; CHEMICAL COMPOSITION; DACITE; FRACTIONAL CRYSTALLIZATION; PETROGENESIS; SUBDUCTION; VOLCANO;

AUSTRALASIA; KERMADEC ARC; KERMADEC ISLANDS; NEW ZEALAND; PACIFIC ISLANDS; PACIFIC OCEAN; RAOUL ISLAND;

EID: 33747590403     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2006.03.003     Document Type: Article

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