Conduit Seismicity
Conduit Seismicity is a type of volcanic seismic signal characterized by high-frequency earthquakes originating within the volcanic conduit, distinguished from other volcanic seismic phenomena by its spatial localization to the active magma pathway and its association with brittle failure processes during magma ascent.
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Mapping the Hawaiian plume conduit with converted seismic waves
X. Li, R. Kind, Keith Priestley et al. · Nature · 2000 · 186 citations
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United States Geological Survey
Reston, United States
10 h-index
19 publications
958 citations

University of Alaska Fairbanks
Fairbanks, United States
10 h-index
18 publications
871 citations
Alaska Volcano Observatory
Fairbanks, United States
7 h-index
14 publications
640 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
7 h-index
14 publications
455 citations
Institute of Petroleum Geology and Geophysics
Novosibirsk, Russia
5 h-index
13 publications
441 citations
University of Florence
Florence, Italy
5 h-index
8 publications
389 citations
The University of Tokyo
Tokyo, Japan
5 h-index
9 publications
365 citations
Novosibirsk State University
Novosibirsk, Russia
4 h-index
5 publications
155 citations
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14 publications · 856 citations
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JGR · 7 publications · 816 citations
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