Volcanic and structural evolution of the Okataina Volcanic Centre; dominantly silicic volcanism associated with the Taupo Rift, New Zealand

Journal of Volcanology and Geothermal Research

Volumn 190, Issue 1-2, 2010, Pages 123-135

  Cole, J W ^a   Spinks, K D ^b   Deering, C D ^a   Nairn, I A ^c   Leonard, G S ^d  

^a UNIVERSITY OF CANTERBURY   (New Zealand)

^b Mighty River Power Limited   (New Zealand)

^c GNS Science ^*  (New Zealand)

^d GNS SCIENCE   (New Zealand)

Author keywords

caldera complex; ignimbrite; Okataina; rhyolite; Taupo Rift

Indexed keywords

EXPLOSIVE ERUPTION; IGNIMBRITES; LONG DURATION; NEAR-SURFACE; NEW ZEALAND; PYROCLASTICS; REGIONAL STRUCTURE; REGIONAL TECTONICS; RHYOLITE ERUPTIONS; RHYOLITIC; SILICIC VOLCANISM; STRIKE-SLIP COMPONENT; STRUCTURAL BOUNDARY; STRUCTURAL EVOLUTION; TAUPO VOLCANIC ZONE; TRANSFER ZONES; TRANSTENSION; VOLCANIC ACTIVITIES; WESTERN SIDE;

DOMES; ENGINEERING GEOLOGY; GEOTHERMAL WELLS; MICA; OXIDE MINERALS; QUARTZ; VOLCANOES;

GRANITE;

CALDERA; FISSURE; IGNIMBRITE; LAVA FLOW; PYROCLASTIC DEPOSIT; RHYOLITE; SILICICLASTIC DEPOSIT; TECTONIC EVOLUTION; TECTONIC SETTING; TRANSTENSION; VOLCANISM;

BAY OF PLENTY; NEW ZEALAND; NORTH ISLAND; OKATAINA VOLCANIC CENTRE; TAUPO RIFT;

EID: 75849129611     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.08.011     Document Type: Article

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