15.11.2014 Views

principles and applications of microearthquake networks

principles and applications of microearthquake networks

principles and applications of microearthquake networks

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

2.2. Central California Microearthquake Network 25<br />

1 2 3 4 5 6 7 8 T1 T2 C Channel<br />

I I I I I I 1 I 1 1 I<br />

680 1020 1360 1700 2040 2380 2720 3060 3500 3950 46875 Ctr Freq (HI)<br />

+I25 k125 k125 f125 i125 i125 +125 2125 f50 k50 k0 Modulation (Hz)<br />

k125 i125 +125 f125 f125 f125 k125 2125 z125 f125 +ZOO Derodulation (Hz)<br />

I I 1 I I I I I I 1<br />

500 1000 2000 3000 4000 5000<br />

FREOUENCY (Hz)<br />

Fig. 8. Format <strong>of</strong> frequency division multiplexing (FDM) used for telemetry transmission<br />

<strong>and</strong> recording by the USGS Central California Microearthquake Network (modified<br />

from Eaton, 1976).<br />

would show eight spectral peaks, spaced at intervals <strong>of</strong> 340 Hz <strong>and</strong> <strong>of</strong><br />

approximately the same height. The reason for using FDM is to reduce the<br />

cost <strong>of</strong> data transmission.<br />

When the telemetered FDM signal reaches the central recording site, it<br />

is divided <strong>and</strong> sent to two places (Fig. 7). First, it is sent through an<br />

automatic gain control (AGC) system, time code <strong>and</strong> other signals are<br />

added to it, <strong>and</strong> the combined signal is recorded in direct mode on an<br />

analog magnetic tape recorder. Second, it is sent through a bank <strong>of</strong> eight<br />

frequency discriminators (matching the eight FDM subcarriers), <strong>and</strong> the<br />

original analog signals are restored. The analog signals may be recorded<br />

on paper or photographic film. They may also be sent to an on-line computer<br />

system or retransmitted to other recording centers.<br />

Eaton (1977) summarized the amplitude-frequency response <strong>of</strong> each <strong>of</strong><br />

the major components <strong>of</strong> the USGS telemetry system (Fig. 9). Before<br />

proceeding with a summary <strong>of</strong> the instrumentation, it is instructive to<br />

consider how each system component contributes to the response <strong>of</strong> the<br />

entire system. The response curves in Fig. 9 are determined from design<br />

<strong>and</strong> manufacturers’ specifications <strong>and</strong> from simple tests with a function<br />

generator. Each response curve is stylized, with emphasis given to the<br />

frequency at which various slopes change <strong>and</strong> to the rate <strong>of</strong> attenuation.<br />

Figure 9A-C shows the essential features <strong>of</strong> the amplitude-frequency<br />

response for the major electronic units-the amplifier <strong>and</strong> VCO in the field<br />

package, <strong>and</strong> the discriminator at the central recording site. The combined<br />

response <strong>of</strong> these three units is shown in Fig. 9D <strong>and</strong> is referred to<br />

as the electronics response. The low-frequency roll-<strong>of</strong>f starting at 0.1 Hz<br />

for the electronics response is due solely to the amplifier in the field<br />

package, whereas the high-frequency roll-<strong>of</strong>f starting at 30 Hz has contributions<br />

from both the amplifier in the field <strong>and</strong> the discriminator at the<br />

central site. Figure 9E-G shows the response <strong>of</strong> the recording devicesthe<br />

Oscillomink (a multichannel ink-jet oscillograph), the Develocorder,

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!