Temporal evolution of a high-K andesitic magmatic system: Taranaki volcano, New Zealand

Journal of Petrology

Volumn 53, Issue 2, 2012, Pages 325-363

  Zernack, A V ^a   Price, R C ^b   Smith, I E M ^c   Cronin, S J ^a   Stewart, R B ^a  

^a MASSEY UNIVERSITY   (New Zealand)

^b UNIVERSITY OF WAIKATO   (New Zealand)

^c UNIVERSITY OF AUCKLAND   (New Zealand)

Author keywords

Debris avalanche deposits; High K andesite; Lower crustal hot zone; Magmatic evolution; Taranaki Egmont Volcano

Indexed keywords

ANDESITE; CHEMICAL COMPOSITION; CLINOPYROXENE; DEBRIS AVALANCHE; FRACTIONATION; IGNEOUS GEOCHEMISTRY; LOWER CRUST; LOWER MANTLE; MAGMATISM; PARENT BODY; POTASSIUM; TEMPORAL VARIATION;

MOUNT TARANAKI; NEW ZEALAND; NORTH ISLAND; TARANAKI;

EID: 84856179060     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egr064     Document Type: Article

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