Spatial variations in the frequency-magnitude distribution of earthquakes at Soufriere Hills Volcano, Montserrat, West Indies

dc.contributorThe University of the West Indies
dc.creatorPower, John A. "et al."
dc.date1998
dc.date.accessioned2018-03-14T14:13:48Z
dc.date.available2018-03-14T14:13:48Z
dc.descriptionThe frequency-magnitude distribution of earthquakes measured by the b-value is determined as a function of space beneath Soufriere Hills Volcano, Montserrat, from data recorded between August 1, 1995 and March 31, 1996. A volume of anomalously high b-values (b > 3.0) with a 1.5 km radius is imaged at depths of 0 and 1.5 km beneath English's Crater and Chance's Peak. This high b-value anomaly extends southwest to Gage's Soufriere. At depths greater than 2.5 km volumes of comparatively low b-values (b∼1) are found beneath St. George's Hill, Windy Hill, and below 2.5 km depth and to the south of English's Crater. We speculate the depth of high b-value anomalies under volcanoes may be a function of silica content, modified by some additional factors, with the most siliceous having these volumes that are highly fractured or contain high pore pressure at the shallowest depths.
dc.identifier.urihttps://hdl.handle.net/2139/45478
dc.sourceGeophysical Research Letters, Vol. 25, No. 19, 3653-3656
dc.subjectEarthquakes
dc.subjectSoufriere Hills Volcano
dc.subjectFrequency magnitude
dc.subjectb-values
dc.titleSpatial variations in the frequency-magnitude distribution of earthquakes at Soufriere Hills Volcano, Montserrat, West Indies

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