Caldera-forming Currents
Caldera-Forming Currents is a type of pyroclastic density current distinguished by its exceptional volume, mobility, and sustained eruptive flux, capable of inducing magma chamber roof collapse and subsequent caldera formation through the generation of large-scale, ignimbrite-depositing flows.
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2017–2026
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Ilya N. Bindeman, V. L. Leonov, Pavel Izbekov et al. · Journal of Volcanology and Geothermal Research · 2009 · 108 citations
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Geological Survey of Japan
Tsukuba, Japan
5 h-index
5 publications
136 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
5 h-index
15 publications
433 citations
United States Geological Survey
Reston, United States
4 h-index
6 publications
363 citations

McGill University
Montreal, Canada
3 h-index
4 publications
274 citations

University of British Columbia
Vancouver, Canada
2 h-index
3 publications
119 citations
Smithsonian Institution
Washington, United States
2 h-index
2 publications
99 citations
Alaska Volcano Observatory
Fairbanks, United States
2 h-index
3 publications
116 citations
Universidad de Buenos Aires
Buenos Aires, Argentina
2 h-index
3 publications
49 citations
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14 publications · 781 citations
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17 publications · 723 citations
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4 publications · 133 citations
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2 publications · 35 citations
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2 publications · 63 citations
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