Glass geochemical compositions from widespread tephras erupted over the last 200 years from Mount St. Helens
Author:
Affiliation:
1. Asian School of the EnvironmentNanyang Technological UniversitySingapore 637459
2. Department of Earth and Atmospheric SciencesUniversity of AlbertaEdmonton Alberta T6G 2E3 Canada
Funder
Natural Sciences and Engineering Research Council of Canada
Publisher
Wiley
Subject
Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3166
Reference62 articles.
1. Physical properties of the 1980 Mount St. Helens cryptodome magma
2. Rapid decompression-driven crystallization recorded by melt inclusions from Mount St. Helens volcano
3. BlundyJ CashmanKV BerloK.2008. Evolving magma storage conditions beneath Mount St. Helens inferred from chemical variations in melt inclusions from the 1980–1986 and current (2004–2006) eruptions. In A volcano rekindled: the renewed eruption of Mount St. Helens 2004‐2006 Sherrod DR Scott WE Stauffer PH (eds).US Geological Survey Professional Papers1750: 755–790.
4. The intensity and magnitude of Holocene plinian eruptions from Mount St. Helens volcano
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1. Understanding and modeling tephra transport: lessons learned from the 18 May 1980 eruption of Mount St. Helens;Bulletin of Volcanology;2022-12-16
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4. How does tephra deposit thickness change over time? A calibration exercise based on the 1980 Mount St Helens tephra deposit;Journal of Volcanology and Geothermal Research;2020-07
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