globalchange  > 气候变化与战略
DOI: 10.1073/pnas.1616129113
论文题名:
Warm storage for arc magmas
作者: Barboni M.; Boehnke P.; Schmitt A.K.; Mark Harrison T.; Shane P.; Bouvier A.-S.; Baumgartner L.
刊名: Proceedings of the National Academy of Sciences of the United States of America
ISSN: 0027-8424
出版年: 2016
卷: 113, 期:49
起始页码: 13959
结束页码: 13964
语种: 英语
英文关键词: Arc magma ; Eruption ; Volcano ; Zircon
Scopus关键词: zirconium ; Article ; geochemistry ; heat ; priority journal ; storage ; storage temperature ; volcano
英文摘要: Felsic magmatic systems represent the vast majority of volcanic activity that poses a threat to human life. The tempo and magnitude of these eruptions depends on the physical conditions under which magmas are retained within the crust. Recently the case has been made that volcanic reservoirs are rarely molten and only capable of eruption for durations as brief as 1,000 years following magma recharge. If the "cold storage" model is generally applicable, then geophysical detection of melt beneath volcanoes is likely a sign of imminent eruption. However, some arc volcanic centers have been active for tens of thousands of years and show evidence for the continual presence of melt. To address this seeming paradox, zircon geochronology and geochemistry from both the frozen lava and the cogenetic enclaves they host from the Soufrière Volcanic Center (SVC), a long-lived volcanic complex in the Lesser Antilles arc, were integrated to track the preeruptive thermal and chemical history of the magma reservoir. Our results show that the SVC reservoir was likely eruptible for periods of several tens of thousands of years or more with punctuated eruptions during these periods. These conclusions are consistent with results from other arc volcanic reservoirs and suggest that arc magmas are generally stored warm. Thus, the presence of intracrustal melt alone is insufficient as an indicator of imminent eruption, but instead represents the normal state of magma storage underneath dormant volcanoes.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/162197
Appears in Collections:气候变化与战略

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作者单位: Barboni, M., Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA 90095, United States; Boehnke, P., Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA 90095, United States; Schmitt, A.K., Institute of Earth Sciences, Heidelberg University, Heidelberg, 69120, Germany; Mark Harrison, T., Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA 90095, United States; Shane, P., School of Environment, University of Auckland, Auckland, 1142, New Zealand; Bouvier, A.-S., Institute of Earth Sciences, University of Lausanne, Lausanne, 1015, Switzerland; Baumgartner, L., Institute of Earth Sciences, University of Lausanne, Lausanne, 1015, Switzerland

Recommended Citation:
Barboni M.,Boehnke P.,Schmitt A.K.,et al. Warm storage for arc magmas[J]. Proceedings of the National Academy of Sciences of the United States of America,2016-01-01,113(49)
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