Vertically extensive and unstable magmatic systems: A unified view of igneous processes
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- Katharine V. Cashman
- School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK.
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- R. Stephen J. Sparks
- School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK.
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- Jonathan D. Blundy
- School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK.
書誌事項
- 公開日
- 2017-03-24
- 権利情報
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- http://www.sciencemag.org/about/science-licenses-journal-article-reuse
- DOI
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- 10.1126/science.aag3055
- 公開者
- American Association for the Advancement of Science (AAAS)
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説明
<jats:title>Making magma chambers from mush</jats:title> <jats:p> 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 <jats:italic>et al.</jats:italic> 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. </jats:p> <jats:p> <jats:italic>Science</jats:italic> , this issue p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" issue="6331" page="eaag3055" related-article-type="in-this-issue" vol="355" xlink:href="10.1126/science.aag3055">eaag3055</jats:related-article> </jats:p>
収録刊行物
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- Science
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Science 355 (6331), eaag3055-, 2017-03-24
American Association for the Advancement of Science (AAAS)
