Mafic inputs into the rhyolitic magmatic system of the 2.08 Ma Huckleberry Ridge eruption, Yellowstone
Author:
Affiliation:
1. School of Geography, Environment and Earth Sciences, Victoria University of Wellington, P.O. Box 600, Wellington 6140, New Zealand
Publisher
Mineralogical Society of America
Subject
Geochemistry and Petrology,Geophysics
Link
https://pubs.geoscienceworld.org/msa/ammin/article-pdf/103/5/757/4135839/am-2018-6273.pdf
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2. Spatio-temporal clustering of post-caldera eruptions at Yellowstone caldera: implications for volcanic hazards and pre-eruptive magma reservoir configuration;Bulletin of Volcanology;2023-09-12
3. Degassing from magma reservoir to eruption in silicic systems: The Li elemental and isotopic record from rhyolitic melt inclusions and host quartz in a Yellowstone rhyolite;Geochimica et Cosmochimica Acta;2022-06
4. The Huckleberry Ridge Tuff, Yellowstone: evacuation of multiple magmatic systems in a complex episodic eruption;Journal of Petrology;2019-06-28
5. The influence of basement faults on local extension directions: Insights from potential field geophysics and field observations;Basin Research;2019-03-26
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