Waveform classification of volcanic low-frequency earthquake swarms and its implication at Soufrière Hills Volcano, Montserrat
Low-frequency volcanic earthquakes are indicators of magma transport and activity within shallow conduit systems. At a number of volcanoes, these events exhibit a high degree of waveform similarity providing a criterion for classification. Using cross-correlation techniques to quantify the degree of...
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Veröffentlicht in: | Journal of volcanology and geothermal research 2006-05, Vol.153 (1), p.51-63 |
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Sprache: | eng |
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