The nature of active magma reservoirs and storage underneath Cascade volcanoes

Elements
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Abstract

Volcanic activity is dictated by crustal pathways and reservoirs through which magma ascends and collects. The Cascades are a natural laboratory to study the variable influence of the crust on erupted magmas and subterranean reservoirs. The interaction of ascending magmas with the variable subduction geometry and tectonics of the overriding North American plate have given rise to a diversity of magmatic storage conditions. The confluence of geochemical and geophysical investigations emphasizes that most magmatic systems in the Cascades have been built at multiple levels in the crust as determined by tectonics, pre-existing structure, and magmatic flux from the mantle.

Suggested Citation

Dufek, J., Cashman, K., Hooft, E., and Bedrosian, P.A., 2022, The nature of active magma reservoirs and storage underneath Cascade volcanoes: Elements, v. 18, no. 4, p. 239-245, https://doi.org/10.2138/gselements.18.4.239.

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Publication type Article
Publication Subtype Journal Article
Title The nature of active magma reservoirs and storage underneath Cascade volcanoes
Series title Elements
DOI 10.2138/gselements.18.4.239
Volume 18
Issue 4
Year Published 2022
Language English
Publisher GeoScienceWorld
Contributing office(s) Geology, Geophysics, and Geochemistry Science Center
Description 7 p.
First page 239
Last page 245
Country Canada, United States
State British Columbia, California, Oregon, Washington
Other Geospatial Cascades
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