1887

Abstract

We investigate the use of seismic sensors as small seismic sources. A voltage signal is applied to a number of geophones, forcing the mass within the geophones to move, generating a seismic wavefield that is recorded on a separate array of geophones. We observe higher-frequency (25 Hz and above) surface and body waves propagating from the geophone source at offsets of 10s of metres.

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/content/papers/10.3997/2214-4609.20131233
2013-06-10
2021-10-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20131233
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