期刊
GEOPHYSICAL RESEARCH LETTERS
卷 32, 期 7, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2004GL022265
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资金
- Natural Environment Research Council [NER/A/S/2003/00512] Funding Source: researchfish
In March 2004, during a period of no magma extrusion at Soufriere Hills volcano, Montserrat, an explosive event occurred with little precursory activity. Recorded broadband seismic signals ranged from an ultra-long-period signal with a dominant period of 120 s to impulsive, short-duration events containing frequencies up to 30 Hz. Synthetic displacement functions were fit to the long-period data after application of the seismometer response. These indicate a shallow collapse of the volcanic edifice occurred, initiated similar to 300 m below the surface, lasting similar to 100 s. Infrasonic tremor and pulses were also recorded in the 1 - 20 Hz range. The high-frequency seismicity and infrasound are interpreted as the subsequent collapse of a gravitationally unstable buttress of remnant dome material which impacted upon the edifice surface. This unique dataset demonstrates the benefits of deploying multiparameter stations equipped with broadband instruments.
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