Silicic Lava Flows is a type of volcanic lava flow characterized by high silicon dioxide content, typically exceeding 65 weight percent, that distinguishes it from mafic and intermediate lava flows by its high viscosity, low eruption temperature, and tendency to form thick, slow-moving, and often blocky or obsidian-rich deposits.
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2017–2026
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Parents
Publications
80
T. L. Grove, Julie M. Donnelly‐Nolan · Contributions to Mineralogy and Petrology · 1986 · 299 citations
Volcanology and geothermal energy
Choice Reviews Online · 1992 · 287 citations
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Institutions
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Arizona State University
Tempe, United States
8 h-index
13 publications
853 citations
United States Geological Survey
Reston, United States
5 h-index
10 publications
814 citations
Centre National de la Recherche Scientifique
Paris, France
4 h-index
10 publications
255 citations
University of Hawaii System
Honolulu, United States
4 h-index
7 publications
478 citations
Planetary Science Institute
Tucson, United States
4 h-index
4 publications
148 citations
Black Hills State University
Spearfish, United States
3 h-index
3 publications
106 citations
Johannes Gutenberg University Mainz
Mainz, Germany
3 h-index
3 publications
172 citations
Jet Propulsion Laboratory
Pasadena, United States
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5 publications
201 citations
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- Journal of Geophysical Research Atmospheres
JGR · 13 publications · 1.1K citations
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- Journal of Volcanology and Geothermal Research
12 publications · 674 citations
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- Bulletin of Volcanology
8 publications · 511 citations
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- Geological Society of America Bulletin
6 publications · 358 citations
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- Journal of Petrology
4 publications · 225 citations
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