principles and applications of microearthquake networks
principles and applications of microearthquake networks
principles and applications of microearthquake networks
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3.4. Everrt Processitig 61<br />
duration <strong>of</strong> the earthquake. Precise measurement <strong>of</strong> the phase data is<br />
essential because they are used to compute the origin time. hypocenter,<br />
<strong>and</strong> magnitude <strong>of</strong> the earthquake, <strong>and</strong> to deduce its focal mechanism. In<br />
the following subsection, we give some general methods <strong>of</strong> measuring the<br />
phase data.<br />
The goals <strong>of</strong> event processing are to measure the phase data as uniformly<br />
<strong>and</strong> precisely as possible <strong>and</strong> to prepare the so-called phase list<br />
containing these data for each earthquake. In this section. we discuss<br />
processing the individual seismic traces, while in Section 3.5 we discuss<br />
processing the phase lists.<br />
3.4.1. Visual Methods<br />
The traditional way <strong>of</strong> measuring phase data is to read visually the<br />
phase time, amplitudes <strong>and</strong> periods, etc., from the seismograms using<br />
rulers or scales (see, e.g., Willmore, 1979). The phase data are usually<br />
recorded on a printed form to facilitate punching cards or otherwise entering<br />
the data into a computer. The visual method has the advantage that it<br />
is straightforward. It is also a simple matter to read <strong>and</strong> merge data from a<br />
variety <strong>of</strong> visual recording media. For a small <strong>microearthquake</strong> network<br />
operating in an area <strong>of</strong> moderate seismicity, this may be the most costeffective<br />
method to use. However, the visual method has the following<br />
disadvantages: (1) different analysts may read the seismograms differently:<br />
(2) errors may be introduced in measuring, writing, or keypunching<br />
the data; <strong>and</strong> (3) it may be difficult to carry out such a tedious task over a<br />
long period <strong>of</strong> time. Also, visual recording media have a limited dynamic<br />
range <strong>and</strong> a limited recording speed, so that some <strong>of</strong> the phase data (such<br />
as first P-motion, S-arrival, <strong>and</strong> maximum trace amplitude) cannot be read<br />
precisely, if at all.<br />
For a large <strong>microearthquake</strong> network where the data volume is large,<br />
the visual method <strong>of</strong> measuring phase data requires a considerable amount<br />
<strong>of</strong> checking to minimize errors in data h<strong>and</strong>ling. This includes systematic<br />
checking <strong>of</strong> measured phase data by another analyst before keypunching,<br />
<strong>and</strong> systematic verifying <strong>of</strong> the phase data after keypunching. Our experience<br />
shows that analysts or keypunch operators occasionally enter the<br />
data in the wrong place or transpose digits in the data. For example, a<br />
P-arrival time <strong>of</strong> 13.55 sec may be written or keypunched as 3 1.55 sec.<br />
3.4.2. Semiautomated Methods<br />
Semiautomated methods usually are designed to eliminate the tasks <strong>of</strong><br />
recording <strong>and</strong> keypunching data that are required in the visual methods.