Abstract
A significant and often overlooked aspect of seismic surveys is the importance of data fidelity. Geophone fidelity is particularly critical for multicomponent seismic surveys in which the full vector wavefield is sampled by geophones which house multiple elements. Traditionally, geophones are tested on “shake tables” in the laboratory (with field testing equipment) or evaluated on the basis of simulation or equivalent circuits. There appear, however, to be few studies which evaluate geophone performance in the field.
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