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Vertically extensive and unstable magmatic systems: A unified view of igneous processes

Cashman, Katharine V., Sparks, R. Stephen J., Blundy, Jonathan D.·2017·Science
DOI 10.1126/science.aag3055
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Abstract

Making magma chambers from mush: Shallow magma chambers either erupt as volcanoes or solidify as intrusive magma bodies. These magma bodies are traditionally considered to be long-lived and dominated by melt. Cashman et al. review the evidence that shallow magma chambers are actually assembled quickly from much larger, crystal-rich transcrustal magmatic systems. This paradigm helps explain many geophysical and geochemical features of volcanic systems. It also presents challenges for understanding the evolution of magma and provides insight into how and why volcanoes erupt. Science , this issue p. eaag3055

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Cited by

See all 1,159

Metadata

Authors
Cashman, K. V., Sparks, R. S. J., & Blundy, J. D.
Affiliations
School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK.
ORCID
Venue
Science
Publisher
American Association for the Advancement of Science (AAAS)
Published
2017-03-24
Volume
355
Issue
6331
ISSN
  • 0036-8075
  • 1095-9203
DOI
10.1126/science.aag3055
Cited by
1,159
References
0
Language
en
Licence
www.sciencemag.org/about/science-licenses-journal-article-reuse (vor, 365 d)
Funders
AXA Research Fund (award282399)

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CoChat. (2026). Citation check: Vertically extensive and unstable magmatic systems: A unified view of igneous processes. https://app.cochat.ai/papers/10.1126/science.aag3055
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Cashman, K. V., Sparks, R. S. J., & Blundy, J. D. (2017). Vertically extensive and unstable magmatic systems: A unified view of igneous processes. Science. https://doi.org/10.1126/science.aag3055