Are arc-type rocks the products of magma crystallisation? Observations from a simple oceanic arc volcano: Raoul Island, Kermadec Arc, SW Pacific

Journal of Volcanology and Geothermal Research

Volumn 190, Issue 1-2, 2010, Pages 219-234

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

^a UNIVERSITY OF AUCKLAND   (New Zealand)

^b MASSEY UNIVERSITY   (New Zealand)

^c UNIVERSITY OF WAIKATO   (New Zealand)

Author keywords

Kermadec Arc; Oceanic Arc; Subduction zone petrology

Indexed keywords

ARC VOLCANOES; CLINOPYROXENES; COMPOSITIONAL RANGE; CORE COMPOSITION; CRYSTAL COMPONENTS; CRYSTALLISATION; GEOCHEMICAL COMPOSITION; KERMADEC ARC; LOWER CRUST; MAGMATIC SYSTEMS; MANTLE WEDGE; ORTHOPYROXENE; SUBDUCTION ZONES;

CHROMIUM; CRYSTALLIZATION; OLIVINE; PETROGRAPHY; PETROLOGY; ROCKS; SILICATE MINERALS; TECTONICS; VOLCANOES;

CAVITY RESONATORS;

CHEMICAL COMPOSITION; CRYSTALLIZATION; FRACTIONAL CRYSTALLIZATION; ISLAND ARC; LAVA; LOWER CRUST; MAGMATISM; PETROLOGY; PHENOCRYST; STRATOVOLCANO; SUBDUCTION ZONE; ZONING;

KERMADEC ISLANDS; NEW ZEALAND; PACIFIC OCEAN; PACIFIC OCEAN (SOUTHWEST); RAOUL ISLAND;

EID: 75849163799     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.05.006     Document Type: Article

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