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DEPARTMENT OF GEOPHYSICS, FACULTY OF SCIENCE THE UNIVERSITY OF WESTERN ONTARIO, LONDON 72, Canada
Abstract
The substitution of an oscilloscope as detector into a Willmore bridge circuit allows a simple, accurate, and direct method of calibration for seismometer systems. An example of the method is given and its modification for a seismometer having appreciable inductance is discussed. It is also shown that transient methods do not allow an accurate determination of high-frequency response.
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