Title: Acoustic Characterization of Explosion Complexity at Sakurajima, Karymsky, and Tungurahua Volcanoes
Abstract: Research Article| October 15, 2014 Acoustic Characterization of Explosion Complexity at Sakurajima, Karymsky, and Tungurahua Volcanoes Robin S. Matoza; Robin S. Matoza aInstitute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093‐0225 [email protected] Search for other works by this author on: GSW Google Scholar David Fee; David Fee bGeophysical Institute, Alaska Volcano Observatory, University of Alaska Fairbanks, 903 Koyukuk Drive, Fairbanks, Alaska 99775 U.S.A. Search for other works by this author on: GSW Google Scholar Taryn M. López Taryn M. López bGeophysical Institute, Alaska Volcano Observatory, University of Alaska Fairbanks, 903 Koyukuk Drive, Fairbanks, Alaska 99775 U.S.A. Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2014) 85 (6): 1187–1199. https://doi.org/10.1785/0220140110 Article history first online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Robin S. Matoza, David Fee, Taryn M. López; Acoustic Characterization of Explosion Complexity at Sakurajima, Karymsky, and Tungurahua Volcanoes. Seismological Research Letters 2014;; 85 (6): 1187–1199. doi: https://doi.org/10.1785/0220140110 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search Great diversity has been observed in volcanic infrasound signals worldwide, reflecting rich variability in their physical source mechanisms. Infrasound waveforms, estimated signal powers, and frequency contents vary dramatically across a large spectrum of physical eruptive styles (e.g., Johnson and Ripepe, 2011; Fee and Matoza, 2013; Garces et al., 2013). The observed infrasound signals and eruptive styles span, but do not fall neatly into, the idealized terms such as Hawaiian, Strombolian, Vulcanian, sub‐Plinian, and Plinian (e.g., Walker, 1973; Fee and Matoza, 2013). In physical volcanology, the description and classification of explosive eruption styles are traditionally... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.