The REDI system has routinely produced automatic estimates of moment magnitude
(
) for many years. However, wary of complications caused by the
publication of
multiple magnitudes, these estimates were not routinely
used as the ``official" magnitude until after the
05/14/2002 Gilroy earthquake (
4.9,
5.1).
Since then, solutions that meet a
minimum quality criterion are automatically reported (a variance
reduction of 40% or higher). This criterion appears to work
very well and screens out events contaminated
by teleseisms. Over the last few years, nearly all events over
4.5 have met this criterion, as have a number of events in the
M3.5-4.5 range. As part of the effort to establish a
statewide magnitude reporting
hierarchy, we have looked more closely at the estimates of
(Gee et al., 2003b; 2004) and the comparison between
and
.
Two methods of
determining regional moment tensor (RMT) solutions were originally
part of the REDI system - the complete waveform
modeling technique (CW) of Dreger and Romanowicz (1994) and
the surface wave inversion (SW) of Romanowicz et al. (1993). In FY05/06,
processing for the SW algorithm was discontinued, however
CW moment tensors continue to be calculated, reviewed and reported.
Comparison between the results of the CW
method and other regional moment tensor
studies in northern California and the western United States
show excellent agreement in the estimate of seismic moment and
.
As we transition toward
statewide reporting of earthquake information, a comparison of magnitudes
calculated for Southern and Northern California
becomes important. We have collected
a set of events recorded well by digital broadband and and strong
motion stations of the Northern California (NC), Berkeley (BK) and Southern
California (CI) networks and are assessing the computation of local
magnitude for each station. Reseacrh Study 2.13. reports on these activities.
Table 3.19:
Moment tensor solutions for significant
events from July 1, 2006 through
June 30, 2007 using a complete waveform fitting
inversion. Epicentral information is
from the UC Berkeley/USGS Northern California Earthquake
Management Center. Moment is in dyne-cm and
depth is in km.
|
|
Location |
Date |
UTC Time |
Lat. |
Lon. |
MT |
|
|
Str. |
Dip |
Rake |
Mo |
|
|
|
|
|
|
Depth |
|
|
|
|
|
|
|
Offshore of Fort Ross |
7/6/2006 |
20:43:24 |
38.508 |
-123.463 |
5 |
3.7 |
3.7 |
4.69E+21 |
295 |
46 |
84 |
|
Petrolia |
7/19/2006 |
11:41:43 |
40.281 |
-124.426 |
30 |
4.7 |
5 |
3.53E+23 |
102 |
83 |
173 |
|
Glen Ellen |
8/3/2006 |
3:08:12 |
38.363 |
-122.589 |
5 |
4.7 |
4.4 |
5.64E+22 |
256 |
86 |
19 |
|
Bishop |
9/7/2006 |
1:38:59 |
37.31 |
-118.284 |
8 |
3.6 |
3.4 |
1.86E+21 |
342 |
86 |
158 |
|
Willits |
9/26/2006 |
20:56:13 |
39.31 |
-123.217 |
8 |
3.9 |
3.9 |
9.52E+21 |
333 |
61 |
-171 |
|
Petrolia |
10/17/2006 |
20:53:18 |
40.55 |
-126 |
11 |
4.9 |
4.8 |
2.03E+23 |
277 |
85 |
-166 |
|
Geysers |
10/20/2006 |
17:00:08 |
38.867 |
-122.7873 |
5 |
4.5 |
4.6 |
9.88E+22 |
254 |
68 |
-39 |
|
Geysers |
10/20/2006 |
23:31:39 |
38.867 |
-122.783 |
5 |
4.5 |
3.8 |
6.50E+21 |
240 |
55 |
-65 |
|
Petrolia |
10/24/2006 |
14:26:43 |
40.403 |
-125.066 |
5 |
4 |
4.4 |
4.50E+22 |
99 |
85 |
182 |
|
Willits |
11/9/2006 |
8:38:13 |
39.355 |
-123.285 |
8 |
4 |
4 |
1.49E+22 |
336 |
87 |
172 |
|
Willits |
11/10/2006 |
5:05:56 |
39.357 |
-123.282 |
8 |
3.7 |
3.7 |
4.69E+21 |
329 |
90 |
-167 |
|
Paso Robles |
11/30/2006 |
4:06:40 |
35.631 |
-120.754 |
8 |
4.7 |
3.8 |
5.33E+21 |
245 |
89 |
7 |
|
Coalinga |
12/16/2006 |
6:14:05 |
36.174 |
-120.292 |
5 |
4.3 |
4.2 |
2.16E+22 |
299 |
71 |
89 |
|
Petrolia |
12/17/2006 |
15:13:40 |
40.392 |
-125.023 |
5 |
3.9 |
4.3 |
3.57E+22 |
274 |
90 |
-159 |
|
Bishop |
12/19/2006 |
15:21:42 |
37.493 |
-118.188 |
5 |
4 |
3.7 |
4.33E+21 |
221 |
86 |
-27 |
|
Berkeley |
12/21/2006 |
3:12:28 |
37.86 |
-122.237 |
8 |
3.7 |
3.6 |
2.85E+21 |
49 |
80 |
-14 |
|
Berkeley |
12/23/2006 |
6:49:57 |
37.862 |
-122.237 |
11 |
3.7 |
3.6 |
2.82E+21 |
139 |
89 |
-153 |
|
Berkeley |
12/23/2006 |
17:21:15 |
37.861 |
-122.235 |
11 |
3.5 |
3.4 |
1.63E+21 |
148 |
86 |
-169 |
|
Glen Ellen |
1/12/2007 |
11:27:50 |
38.391 |
-122.615 |
11 |
3.8 |
3.7 |
3.27E+23 |
236 |
89 |
34 |
|
Bishop |
1/17/2007 |
14:01:08 |
37.408 |
-118.531 |
5 |
4 |
3.6 |
3.66E+21 |
37 |
83 |
17 |
|
Morgan Hill |
1/17/2007 |
17:43:22 |
37.12 |
-121.523 |
8 |
3.5 |
3.4 |
1.38E+21 |
328 |
89 |
-159 |
|
Petrolia |
1/24/2007 |
13:42:52 |
40.312 |
-124.584 |
18 |
3.7 |
4.4 |
5.05E+22 |
187 |
85 |
25 |
|
San Simeon |
2/20/2007 |
16:46:13 |
35.78 |
-121.382 |
8 |
3.7 |
3.7 |
4.96E+21 |
151 |
59 |
137 |
|
Berkeley |
2/24/2007 |
23:46:15 |
37.865 |
-122.241 |
11 |
3.4 |
3.3 |
1.15E+21 |
154 |
88 |
-176 |
|
Ferndale |
2/26/2007 |
12:19:54 |
40.647 |
-124.864 |
8 |
5 |
5.4 |
1.48E+24 |
60 |
89 |
-4 |
|
Lafayette |
3/2/2007 |
4:40:00 |
37.901 |
-122.098 |
14 |
4.4 |
4.2 |
2.77E+22 |
82 |
89 |
-1 |
|
Bridgeport |
3/9/2007 |
3:17:32 |
38.428 |
-119.367 |
11 |
5 |
4.7 |
1.29E+23 |
349 |
65 |
-114 |
|
Petrolia |
4/5/2007 |
22:54:29 |
40.311 |
-124.578 |
18 |
3.8 |
4.1 |
1.93E+22 |
12 |
88 |
18 |
|
Ferndale |
4/7/2007 |
23:55:03 |
40.616 |
-124.753 |
18 |
3.7 |
4.1 |
2.00E+22 |
256 |
78 |
21 |
|
Geysers |
4/24/2007 |
21:08:28 |
38.796 |
-122.794 |
5 |
4.4 |
4.4 |
4.62E+22 |
342 |
82 |
-160 |
|
Geysers |
4/30/2007 |
15:51:28 |
38.82 |
-122.823 |
5 |
3.1 |
3.7 |
3.89E+21 |
136 |
58 |
-133 |
|
Markleeville |
4/30/2007 |
21:57:32 |
38.72 |
-119.62 |
5 |
3.5 |
3.1 |
5.66E+20 |
226 |
87 |
47 |
|
Petrolia |
5/9/2007 |
7:50:05 |
40.376 |
-125.014 |
11 |
5 |
5.2 |
7.81E+23 |
188 |
85 |
24 |
|
Bishop |
5/26/2007 |
8:04:12 |
37.416 |
-118.525 |
8 |
3.5 |
3.3 |
1.24E+21 |
59 |
81 |
10 |
|
Mammoth |
6/12/2007 |
7:22:36 |
37.5425 |
-118.8677 |
11 |
3.6 |
3.6 |
3.14E+21 |
140 |
82 |
-143 |
|
Mammoth |
6/12/2007 |
7:23:43 |
37.539 |
-118.876 |
14 |
5.1 |
4.6 |
9.96E+21 |
310 |
82 |
172 |
|
Offshore of McKinleyville |
6/25/2007 |
2:32:25 |
41.1155 |
-124.825 |
18 |
5 |
5 |
3.36E+23 |
128 |
84 |
160 |
|
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215 McCone Hall, UC Berkeley, Berkeley, CA 94720-4760
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