The Whakamaru magmatic system (Taupō Volcanic Zone, New Zealand), part 2: Evidence from ignimbrite deposits for the pre-eruptive distribution of melt-dominated magma and magma mush
Author:
Funder
Vanderbilt University
National Science Foundation
Publisher
Elsevier BV
Reference93 articles.
1. From mush to eruption in centuries: Assembly of the super-sized Oruanui magma body;Allan;Contrib. Mineral. Petrol.,2013
2. Construction and evolution of igneous bodies: Towards an integrated perspective of crustal magmatism;Annen;Lithos,2015
3. On the origin of crystal-poor rhyolites: Extracted from batholithic crystal mushes;Bachmann;J. Petrol.,2004
4. The magma reservoirs that feed supereruptions;Bachmann;Elements,2008
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1. Granitic mush compaction by impingement of a large felsic enclave: Evidence from the Aztec Wash pluton (Nevada, USA);GEOSPHERE;2024
2. Reconciling mechanical models of caldera ring-fault nucleation within the transcrustal magmatic system paradigm;Journal of Volcanology and Geothermal Research;2024-05
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