Conditions of melt generation beneath the Taupo Volcanic Zone: The influence of heterogeneous mantle inputs on large-volume silicic systems
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/42/1/3/3544910/3.pdf
Reference27 articles.
1. Rhyolites and their source mushes across tectonic settings;Bachmann;Journal of Petrology,2008
2. The origin of lavas and ignimbrites of the Taupo Volcanic Zone, New Zealand, in the light of oxygen isotope data;Blattner;Geochimica et Cosmochimica Acta,1982
3. Contrasting origins of Cenozoic silicic volcanic rocks from the western Cordillera of the United States;Christiansen;Bulletin of Volcanology,2008
4. Structural control and origin of volcanism in the Taupo volcanic zone, New Zealand;Cole;Bulletin of Volcanology,1990
5. A rhyolite compositional continuum governed by lower crustal source conditions in the Taupo Volcanic Zone, New Zealand;Deering;Journal of Petrology,2008
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