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principles and applications of microearthquake networks

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26 2. Itistrutnetztntioti System<br />

5Hz<br />

I<br />

system<br />

-<br />

Modulator (VCO)<br />

0.1 1.0 10 100 c<br />

system<br />

FREQl<br />

ICY (Hz)<br />

Fig. 9. Stylized amplitude response <strong>of</strong> individual components <strong>and</strong> combinations <strong>of</strong> components<br />

used in the USGS Central California Microearthquake Network (modified from<br />

Eaton, 1977). Amplitude attenuation is shown as an integer in dB/octave.<br />

<strong>and</strong> the Helicorder. The Oscillomink is used for making high-speed<br />

playbacks <strong>of</strong> earthquakes originally recorded on magnetic tape. It has a<br />

flat frequency response from dc to well over 100 Hz. The Develocorder is<br />

the primary on-line film recording device. In order to suppress lowfrequency<br />

microseismic noise <strong>and</strong> to prevent trace w<strong>and</strong>ering caused by<br />

VCO drift, a 0.5-Hz low-cut filter has been added to each input terminal <strong>of</strong><br />

the Develocorder. The 15.5-Hz galvanometer accounts for the highfrequency<br />

roll-<strong>of</strong>f in the Develocorder response. Because the Helicorder<br />

uses recording speeds as low as 30 <strong>and</strong> 60 mdmin, its frequency response<br />

roll-<strong>of</strong>f points are set at 0.1 <strong>and</strong> 5 Hz.<br />

Figure 91-K shows the combined response <strong>of</strong> the electronics <strong>and</strong> recording<br />

media-in other words, <strong>of</strong> everything but the seismometer. Because<br />

the Oscillomink response (Fig. 9E) is flat to well beyond 100 Hz, the

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