ML20039C013

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Forwards Response to FSAR Question 361.25 Re Mammoth Lakes Earthquakes
ML20039C013
Person / Time
Site: Summer 
Issue date: 12/18/1981
From: Nichols T
SOUTH CAROLINA ELECTRIC & GAS CO.
To: Harold Denton
Office of Nuclear Reactor Regulation
References
NUDOCS 8112280314
Download: ML20039C013 (57)


Text

{{#Wiki_filter:. o s g m SOUTH CAROLINA ELECTRIC & GAS COMPANY b POST OFF8CE MOR 794 cotuwau, sourw canouwA eseis RECEVM 1 I c;yicjts December 18, 1981 D DEC2812lb a w ono, ase. Mr. Harold R. D'enton, Director 7E Office of Nuclear Reactor Regulation U. S. Nuclear Regulatory Commission Washington, DC 20555

Subject:

Virgil C. Surmer Nuclear Station Docket No. 50/395 Seismic Question 361.25

Dear Mr. Denton:

South Carolina Electric and Gas Company acting for itself and as agent for the South Carolina Public Service Authority hereby provides forty-five (45) copies of our response to FSAR question 361.25 concerning the Mammoth Lakes earthquakes. Since this material deals with the seismic issues under litigation at the ASLB hearings, additional copies of this report are being distributed to the service list in that proceeding. If you have additional questions, please let us know. Very truly yours, l m l jg T. C. Nichols, Jr. L NEC:TCN:1kb Enclosures cc: V. C. Summer Carl Newton T. C. Nichols, Jr. Phyllis Sobel G. H. Fischer Andy Murphy H. N. Cyrus Herbert Grossman H. T. Babb Frank F. Hooper D. A. Nauman Gustave A. Linenberger M. B. Whitaker, Jr. Richard P. Wilson W. A. Williams, Jr. Steven C. Goldberg O. S. Bradham Jack Harris R. B. Clary J. B. Fletcher M. N. Browne W. B. Joyner A. R. Koon E. Luco G. J. Braddick M. Trifunac J. L. Skolds J. B. Knotts, Jr. B. A. Bursey \\ f J. C. Ruoff NPCF gg File O 00 PDR

i 3 g k[ sing all appropriate records from the 361.25 A. Mammoth Lake sequence between magnitude 4.0 and 5.0 compute site specific response spectra for a nearby magnitude 4.5 event recorded at site conditions most similar to the Summer site. If appropriate and available include data collected by the USGS ~ and CDMD. Show all response spectra used and the computed 50th and 84th percentiles at the dampings of interest. Tabulate epicen-tral locations, depths and hypocentral distances for all records used. Discuss the applicability of these records to the condi-tions at the Summer site in terms of depth, hypocentral distances, known source para-meters and tectonic conditions. B. If not already included, discuss the appro-priateness of the McGee site and the effect of the overlying soil upon the response spectra. C. Examine and if applicable compare response spectra from earthquakes recorded at Monti-~ cello with those at Mammoth Lakes in the magnitude and distance range that are most similar. Include high frequency ground motion (greater than 20 Hz) in this com-parison. Discuss the bearing this comparison has upon the use of Mammoth Lake data to estimate ground motion at Monticello. D. Examine and if applicable show site specific spectra at several magnitude ranges to demonstrate the changes in spectral level and shape as a function of increasing event magnitude. E. Discuss the use of the low pass filter used and. its effect upon higher frequencies and peak ground accelerations. Show response spectra utilizing different low filters in the 20 to 50 Hz range. Try to include as l many high frequencies as possible in the l computed site specific spectra. F. Examine and if applicable compare computed site specific spectra with spectra of similar t event sizes and distances recorded at other site conditions at Mammoth Lakes. 361.25-1 l l

I b G. k[ompare site specific spectra computed from Mammoth Lakes - data to the applicant's esti-mated RIS and SSE spectra and discuss the significance of any exceedance in the dif-ferent frequency ranges. l l-1 i i 361.25-2 l l l [

i i

RESPONSE

A. Mammoth Lakes earthquake response spectra for a nearby magnitude 4-5 event i i The Mammoth Lakes, earthquake sequence of 1980 occurred predominantly within the Sierra Nevada immediately to the south of Long Valley Caldera Site conditons within the caldera, where many seismographic instruments were deployed for reasons of accessibility and logistics, do not resemble the site conditons at the Virgil C. Summer Nuclear Station. Descriptions of surficial geologic conditions at instru-ment sites located outside the caldera are given in Table 361.25-1. The site for which seismic absorption effects would be expected'to be lowest is the McGee Creek site, which was occupied by a wideband digital displacement seismograph system. This site is taken to be the mos't similar to the Summer site. The McGee Creek site is centrally located with respect to epicenters of the carthquake sequence (Figure 361.25-24). Hypocentral distances, seismic moments, peak horizontal ground accelerations and Richter magnitudes are given in Table 361.25-2 for all events recorded at McGee Creek with magnitude 4.0 and more, and for smaller events with the shortest hypocentral distances. Hypocentral distance is measured from S-P time using 7.09 kilometers per second of S-P time. Response spectra were calculated for all events of magnitude in the range 4.3 to 4.8, recorded at McGee Creek. 361.25-3

The average magnitude of the events is 4.5, and the aver' S-P time is 1.03 sec (average hypocentral distance 7.3 km). Horizontal-component response spectra of these events (index numbers 1,4,,5,14,32,41,,42,44,48, and 55 in Table 361.25-2) are shown in Figures 361.25-1 to 20 for 2,5, and 7 percent of critical damping. Mean and mean-plus-one standard deviation response spectra for the ensemble are given in Figures 361.25-21, 361.25-22 and 361.25-23 for 2,5, and 7 percent of critical damping. Individual response spectra were not normalized in any way in the statistical calcu-lation. The averaged spectra show response peaks at fre-quencies of approximately 9 and 15 Hz. Individiual spectra show prominant response peaks at one or both of these frequencies. Hypocentral determinations are not available for all o'f the events recorded at McGee Creek. In order to be infor-mative about hypocentral determinations, we compare in Figure 361.25-24 and Table 361.25-3 our master-event loca-tions with hypocenters determined by Archuleta et al. (1981: personal communication, HYPO output dated October 30, 14:03 P.S.T.) for all 13 events in common. Average focal depths for the two sets of hypocenters are very similar: 5.14 km and 5.13 km respectively. However, the solutions of Ar-chuleta et al. show a greater range of depths, with a calculated ' standard deviation' of 3.16 km as compared with 1.94 km. 361.25-4

r Shear wave corner frequencies meacured from Fourier spectra of the horizontal components at McGee Creek are plotted against seismic moment in Figure 361.25-25. Synthe-tic Richter magnitudes in Figure 361.25-26 plot with nearly unit slope against the logarithm of seismic moment. This result is to be expected because both momt.t and Richter magnitude are determined in the displacement-flat portion of the speJtrum for these earthquakes, as their corner frequen-cies are approximately 10 Hz. The Mammoth Lakes earthquakes occurred at considerably greater depths, and were recorded at considerably greater hypocentral distances than the RIS events recorded by the USGS accelerograph on the Monticello Dam abutment. The Mammoth Lakes events represent the release at normal focal depths of relatively rapidly-accumulating tectonic strain', and can not be considered representative of shallow RIS activity at Monticello Reservoir. B. Influence of propagation effects on McGee Creek Spectra while the McGee Creek site may be geologically the most similar of the Mammoth Lakes recording sites to the Summer site, there is evidence for a site-specific propagation effeet that would not be observed. at the Summer site. As noted above, most but not all of the McGee Creek response spectra show peaks at approximately 9 and 15 Hz. One explanation for this effect is modal response of the glacial moraine near whose edge the site is located. However, this does not explain why some of the McGee Creek records are 361.25-5

~ very simple. Nn alternative explanation is that the reson-ance observed for some events is a path (waveguide) effect, due to the presence of a fault or contact zone in the underlying bedrock. The bedrock under the site consists of faulted, folded, metamorphosed Ordovician rocks intruded by granitic batholith. Examples of simple and complex displacement seismograms are shown in Figures 361.25-27 and 361.25-28. These wideband (0.1 to 50 Hz) seismograms are for the earthquakes of May 26 at 19:25 U.T.C. and May 30 at 18:24 U.T.C. Response spectra for these events are shown in Figur.es 361.25-7,8 and 361.25-11,12. Displacement seismograms of the 18:24 event.(Figure 361.25-28) show pronounced resonance following the P and S arrivals. By contrast the 19:25 records (Figure 361.25-27) are exceedingly simple. Figur'e 361.25-29 compares the observed displacement record, north component, with a synthetic displacement seismogram computed for a point dislocation in an elastic halfspace. For this event there is evidently no anomalous path or site effect. Therefore, the most satisfactory explanation for the reson-ance observed in some of the records is a directionally dependent waveguide effect. C. Comparison of spectra of Monticello and Mammoth Lakes earthquakes of similar magnitude recorded at similar distances. At Mammoth Lakes, S-P times read reliably from wideband displacement seismograms indicate that none of the hundreds of events was recorded by the wideband instruments at a 351.25-6

range of less tEan 2.5 km. At Monticello Reservoir, useable ~ accelerograms have been recorded on the dam, abutment only for earthquakes with foci within approximately 1 km. Thus it is not possible to, compare spectra of earthquzkes record-ed at a similar distance range at the two sites. D. Variation of spectral shape with magnitude. Response spectra have not been prepared for Mammoth Lakes events over a wide range of magnitude. A convenient illustration of the variation of spectral shape with magni-tude is shown in Figure 361.25-25, where corner frequencies of shear waves recorded on horizontal components at McGee Creek are plotted against seismic moment. Another indica-tion concerning the spectral shape variation is provided by the observed dependence of-peak ground acceleration op seismic moment (Figures 361.25-31 to 34). E. Effect of low-pass filtering on computed peak ground accelerations. Accelerograms were computed from the wideband displace-ment seismograms by removing the system response and differ-i entiating twice. In order to minimize aliasing effects near the Nyquist frequency (50 Hz), the records were filtered l l with an'8-pole Butterworth filter (a minimum phase, causal, l realizable filter). A filter frequency of 25 Hz was used for all records. This frequency was chosen after conducting I ( a study to determine the effect of varying the filter i l frequency. Table 361.25-4 shows peak accelerations computed i for the earthquake of 10:25 U.T.C., May 26, 1980, recorded 361.25-7 l

~ at McGee Creek, for filter' frequencies of 1 0,1 5,2'5, and 30 Hz. Computed peak accelerations are insensitive to filter frequency for frequencies above about 20 Hz. This is as expected be,cause the peak acelerations occur near the corner frequencies (n 10 15 Hz). At higher frequencies the response spectral acceleration is determined largely by the peak ground acceleration. Thus the low-pass filtering that was required for double-differentiating the wideband dis-placement seismograms has negligible effect on high-fre-quency response spectral accelerations. F. Comparison of Mammoth Lakes spectra at different record-ing sites. A convenient way to compare spectra of earthquakes recorded at dif ferent sites in the vicinity of Mammoth Lakes ~ is to compare their shear wave corner frequencies. Figure 361.25-30 shows horizontal-component shear wave corner frequencies as a function of seismic moment for the four sites occupied by wideband displacement seismographs. The McGee Creek site shows corner frequencies consistantly higher than at the other sites. This effect is in large part attributable to significant seismic absorption for all sites except McGee Creek. The apparent corner frequencies at the other sites are not revesentative of the earth-quake source spectra, reflecting instead the effects of absorption. Peak accelerations at the four sites exhibit the same effect. Figures 361.25-31 to 34 show peak horizontal ground acceleration as a function of seismic moment for Whitmore i 361.25-8

Hot Springs, Rock Creek, Mammoth Ranger Station, and M ee Creek. These figures are not directly comparable because of differences in hypocentral distances: these are shown in Figures 361,.25-35 to 3,8. Index numbers in Figures 361.25-31 to 34 correspond with those in Figures 361.25-35 to 38, respectively. Allowing for the fact that McGee Creek is closer to the source region than are the other sites, it is evident that peak horizontal accelerations recorded at McGee Creek are significantly higher than those recorded elsewhere. At frequencies of approximately 1 Hz, there is no significant difference in motion amplitude between the four sites. This can be seen by comparing synthetic Richter magnitudes determined at each site with Berkeley Richter magnitudes (Figure 361.25-39). At all sites, synthetic ~ Richter magnitude is a good estimator of Berkeley magni-tude. Thus earthquake spectra at the four sites differ only at frequencies greater than 1 Hz. G. Figure 361.25-40 compares 50th and 84th percentile response spectra for M 4.5 Mammoth Lakes earthquakes recorded at McGee Creek with the 84th percentile response spectrum for a hypothetical M 4.5 RIS event, and with the SSE spectrum. All spectra are for 5% critical damping. Comparing at the 84th percentile level, the McGee Creek spectrum exceeds the hypothetical RIS spectrum in the bands 7-10 hz and 12-20 hz, and f alls below the hypothetical RIS spectrum for frequencies less than 7 hz and greater than 20 hz. The spectral peaks appear to be due to a directionally-dependent waveguide effect evident at McGee Creek; these 361.25-9

spectral peaks are not transferable to the Virgil C. Summer site. The 84th percentile McGee Creek spectrum exceeds the SSE spectr6m - for freq'uencies above 7 Hz. The McGee Creek spectrum differs from the SSE spectrum in representing a near-field rather than a far-field event. S 4 361.25-10

REFERENCES Archuleta, R.J., Spudich, A., Cranswick, E., and Mueller, C., 1981, source parameters of the 1980 Mammoth Lakes, California, earthquake sequence (submitted to Journal of Geoph al Research). 2

Turpen, C.D.,

1980, Strong-motion records from the Mammoth Lakes earthquakes of May 1980: California Division of Mines and Geology Preliminary Report 27, 42 p. 4 4 361.25-11

'8 B TABLE 361.25-1 MAMMOTH LAKES RECORDING SITES LOCATED OUTSIDE LONG VALLEY CALDER\\ ' AGENCY -RECORDING SITE SURFICIAL GEOLOGIC CONDITIONS USGS CON few tens of meters of unconsolidated glacial tillL overlying bedrock? MGE. Less_than ~100 meters of glacial till overlying bed-rock? MCC Less than ~100 meters of glacial till overlying bed-rock? ROC '20 - 30 meters of glacial till overlying bedrock? TOM Shallow alluvium overlying bedrock? TWL Shallow alluvium overlying bedrock? PS1 Young glacial outwash and/or old glacial till over-lying volcanic tuff? CDMG Long Valley Dam Earthfill dam with riprap blocks on upstream face. Founded on layered, blocky rhyolite flows 2 to 15 feet-thick. At surface 3 feet of soil, 10 feet of weathered rhyolite. Applicant McGee Creek A few meters of glacial till overlying bedrock (meta-morphosed Ordovician rocas intruded by granite batho-lith). Rock Creek Tens of meters of glacial till overlying bedrock. i I Personal communication, Malcolm Clark, U.S.G.S., Menlo Park, based on reading a geologic map and on familiarity with the region. Turpen (1980) 361.25-12

r TABLE 361.25-2 0 SEISEGRAPHIC DMA RECORDED AT STATION ITEEE (37.5497 N, ll8.8149 W) I.D.# Date Time Log A Iog 2 Peak Accel. Magnitude 4 (km) (dyn-an) (brizontal coupcnents) (Berkeley) (cm/sec2) 1 1980 5 26 1305 0.87 21.51 171.0000 80.3000 4.3 2 5 26 1405 0.82 20.97 60.7000 105.0000 4.2* 3 5 26 1417 0.70 20.65 62.1000 94.2000 4.0* 4 5 26 1438 0.83 21.65 109.0000 172.0000 4.5 5 5 26 1605 0.85 20.96 143.0000 126.0000 4.3* 6 5 26-1618 0.86 20.85 44.0000 68.3000 4.0* 7 5 26 1738 '0.92 21.09 70.5000-43.2000 3.8 8 5 26 -1740 0.92 20.95 43.5000 44.9000 3.3 9 5 26 1806 0.85 20.45 31.8000 17.9000 3.1 10 5 26 1856 0.94 21.05 44.4000 142.0000 3.8 11 5 26 1858 0.86 22.58 167.0000 217.0000 5.5 12 5 26 1908 0.64 20.94 106.0006 139.0000 3.3 13 5 26 1911 0.83 20.68 25.3000 22.4000 3.8 14 5 26 1925 0.86 21.64 69.0000 97.1000 4.7 15 5 26 2004 0.85 21.28 64.4000 105.0000 4.1 16 5 26 2143 0.84 20.86 42.1000 98.8000 3.7 17 5 26 2056 0.58 20.79 84.1000 61.5000 3.3 18 5 26 2159 1.00 20.75 22.7000 25.'2000 3.8 19 5 26 2236 1.00 20.54 9.6200 10.3000 3.6 20 5 26 2320 0.82 20.89 48.4000 70.7000 4.0 21 5 27 44 0.93 21.13 71.3000 89.9000 3.4 22 5 27 54 0.84 20.87 55.7000 69.8000 4.l* 23 5 27 115 0.74 20.57 64.3000 100.0000 4.l* 24 5 27 202 0.59 21.29 234.0000 186.0000 3.6 25 5 27 344 0.89 21.23 109.0000 75.6000 3.7 26 5 27 537 0.71 20.51 63.6000 48.2000 3.4 27 5 27 637 0.85 20.83 0.0000 63.0000 4.1 28 5 27 647 1.03 20.73 9.2600 6.5500 4.0 29 5 27 950 1.01 21.23 42.4000 46.3000 4.2* 30 5 27 1028 1.00 20.41 27.8000 21.4000 3.2 31 5 27 1047 0.92 20.74 0.0000 70.0000 3.1 32 5 27 1328 0.81 20.91 37.5000 38.0000 4.3 33 5 29 1417 1.00 21.20 34.0000 41.5000 4.2 34 5 29 459 0.89 20.95 61.0000 54.0000 3.9 35 5 29 1337 0.83 20.79 40.4000 58.9000 3.1 36 5 29 1556 0.89 20.91 74.7000 77.3000 4.l* 37 5 29 1721 0.81 21.54 201.0000 160.0000 4.1 38 5 30 1202 0.90 21.37 164.0000 79.1000 3.9 39 5 30 1542 0.85 21.25 65.5000 66.6000 4.0 40 5 30 1549 0.82 20.66 39.1000 48.7000 3.5 41 5 30 1824 0.92 21.36 108.0000 81.3000 4.5* 42 5 31 59 0.96 21.25 165.0000 90.5000 4.5 43 5 31 806 0.95 21.02 24.3000 44.3000 4.1 44 5 31 1012 C.74 21.53 66.300 136.0000 4.3 45 5 31 1329 0.71 20.46 0.0000 73.0000 4.2* 46 5 31 1344 0.73 20.70 43.8000 89.5000 4.1* 47 5 31 1409 0.83 20.42 14.2000 13.5000 3.2 f 48 5 31 1517 0.90 22.17 214.0000 250.0000 4.8 49 5 31 1521 0.90 21.33 68.0000 121.0000 4.0 50 5 31 1531 0.82 20.96 73.8000 64.3000 3.8

  • Synthetic ML 361.25-13

TABLE 361.25-2 (Continued) 51 5 31 2315 1.06 20.88 66.8000 98.0000 3.8 52 6 1 318 0.63 20.84 53.5000 25.1000 3.2 53 6 1 909 0.45 19.95 22.5000 0.0000 3.9* 54 6 1 1728 0.81 21.10 55.9000 73.0000 3.6 55 t 2 1535 0.85 21.35 169.0000 109.0000 4.5* 56 6 4 24 1.30 20.24-1.6200-1.6900 2.9* 57 6 4, 546 0.,92 19.74 13.0000 8.5800 3.3 58 6 4' 835 1.05 20.34 20.2000 28.5000 3.4 59 6 4 1257 0.64 19.51 20.2000 20.4000 3.4* 60 6 4 1700 1.01 19.66 4.3300 3.6900 2.8* 61 6 4 1910 0.85 20.79 -26.1000 32.2000 3.8 62 6 6 826 0.54 20.15 20.4000 34.9000 3.7*' 63 6 6 953 0.62 20.20 27.5000-28.0000 3.7* 64 6 6 1121 0.57 19.52 13.6000 16.8000 3.3" 65 6 6 1627 0.75 20.38 31.0000 34.9000 3.5 66 6 7 132 1.08 21.01 23.5000 20.0000 3.9 67 6 10 447 0.63 19.33 6.3300 _5.2300 2.9* 68 6 10 1330 0.58 19.34 18.9000 19.1000 3.4* 69 6 11 443 0.90 20.75 26.5000 27.5000 3.9* 70 6 11 951 0.53 19.31 13.5000 15.2000 3.3* 71 6 20 414 0.50 18.70 1.2000 0.0000 2.3* 72 6 20 1136 0.63 19.37 10.8000 0.0000 3.2* 73 6 20 1725 0.87 20.50 18.80000 0.0000 4.0 74 6 21 32 0.50 18.61 1.7700 0.0000 75 6 24 2106 0.63 19.34 9.6700-9.0100 3.l* 76 6 24 2145 0.55 20.16 33.5000 37.8000 3.7* 77 6 24 2234 0.57 19.66 22.6000 25.3000 3.4* 78 6 24 2235 0.53 18.99 10.7000 7.2100 3.D* 79 6 24 2241 0.53 19.22 0.0000 16.6000 3.3* 80 6 25 2057 0.53 18.93 13.3000 8.9500 3.l* 81 6 25 2159 0.57 18.94 5.4900 4.5300 2.7* 82 6 30 1324 0.58 19.26 8.7500 8.0000 83 7 1 1130 0.68 20.43 25.7000 30.9000 3.7* 84 7 1 1757 0.55 19.24 16.2000 8.9300 3.l* 85 7 13 1057 1.03 20.08 8.7400 6.7500 3.3 86 7 16 1619 0.94 20.71 21.0000 21.0000 3.4

  • Synthetic 4

\\ 361.25-14 l l

TABLE 361.25-3 MMM7I11 IAKES, CAIJEDlWIA EARTilOUAKES CCNPARISON OF llYPOCENTRAL DE7IEININATIONS APPLIC1Nr Afr3HTTRPA EP AL. Date O-Time Lat Iong Depth O-Time Lat Iong Depth ML (U ) (M (1980) Ilr Min Sec ( N) (M (Km) Sec .Km) (BRK) ( N 5 27 19 01 08.5 37.581 118.790 4.7 07.85 37.588 118.777 0.56 4.76 i 5 27 21 34 54.4 37.500 118.827 6.9 53.86 37.497 118.810 9.92 4.32 5 28 11 54 38.0 37.448 118.821 5.6 37.24 37.447 118.844 3.40 4.35 5 29 17 21 01.5 37.490 118.843 3.2 01.05 37.511 118.837 4.22 4.12 5 31 00 58 17.9 37.478 118.852 5.1 17.19 37.470 118.860 3.57 4.53 g 5 31 08 05 19.9 37.542 118.839 8.2 19.31 37.548 118.828 E.08 4.07 -[ 5 31 10 11 31.3 37.577 118.824 3.7 30.74 37.579 118.824 3.30 4.25 [ 6 01 06 47 36.6 37.452 118.846 4.5 36.21 37.471 118.842 3.32 4.64 6 01 17 27 25.14 37.567 118.774 5.5 24.54 37.572 118.772 5.41 3.64 6 05 19 41 02.3 37.542 118.883 3.1 01.64 37.548 '118.875 4.70 4.32 6 07 23 17 53.2 37.629 118.886 3.1 52.46 37.625 118.875 4.26 3.94 + 6 08 23 22 21.3 37.462 118.855 9.2 20.66 37.470 118.841 10.94 4.39 6 11 04 40 58.9 37.532 118.893 4.0 58.34 37.535 118.888 3.07 4.69 e

1 TABLE 361.25-4 muF OF FILTER FREQUENCY CN CmPtTIED PEAK GROUND MER-i ATIGE REDORDED AT MJGEE CREEK EOR 'DE EARIHQUAKE OF 19:25 UIC, MAY 26, 1980 Filter Frequency, Peak Ground Acceleration (cm/sec ) l (Hz) Vertical East-West North-South 10 36.49 49.80 76.32 15 39.46 66.44 93.01 25 43.97 68.96 97.13 30 44.83 66.95 97.69 4 361.25-16 i

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,n . ~ - ., s. 0.01 o el o.1 1.o I c.0 i l PERIOD-5EC RECORD ID=1517 DATE=31MAY80 ML=4.83 COMP N-S FICURE 361.25-18 North ccrnponent response spectra for event #48 (Table 2) for 2, 5, and 7% critical darping.

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FREQ U E NCY-H Z t oo.e s o.e t.o o. 11 I I t t I t i 111 I I I I I I 11 I t t t t t t i 100.0

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.. =...-.s.r . \\. \\ . N.. s. /. '.,.. <. s, >. sN .s y<, N,. .y, 0.01 ...i ..i i o.. rsanos-sac MEAN AND STANDARD DEVIATION 20 HOR REC 7 PCT DAMPING UNNORMALIZED FIGURE 361.25-23 Mean and mean + o harnental response spectra, 7% critical danping _.)

MAMMOTH LAKES L y .HRHHDTH R.S. A ,WHITHORE O O b O CRONLEY e- + 911 319'01 O ,1727 g g $^ ROCK CREEK -1941 0805 O 440 ) Q@ i Y 37.5 N -f-34,$ 118.75% 119.0 hi 0058 232 0647 1154' h Archuleta et al. 0 5 10 KM Map showing epicenters of sme of the larger events of the 1979-1980 sequence i ""P *d D ( t^9 "S)' ^"d Sit *S MAGNITUDE wideband digital seismographs (larger triangles). Icng ( 30 km) half-ellipse O O C = at top indicates southern boundary of Long Valley Caldera. 2 3 4 5 NM Square symbols are epicenters determined by Archuleta et al (1981) for the 13 events listed in Table 361 25-3. Events are identi-fled by hour and minute. T

l I iyL > o f i D ) i C C N: NN N0 .D D D 0 H or z5 _5 5 Z5 __C5 i 2 sz eo in stma il c -c mo om mp I eo nn t en ft I o F 0 rs I h G ee U I G va R e er E n i e3a t w 3 sa 6 I n v 1 C I aO t re E e0 e 2 cc 5 O 1 1 oo h%@ rr 2 1 a dn 5 R ee D dr a a N e u O ap t er Mi E co g Gd 1 9 eeve Cr rs g e eu I es k E e I 9 I I I I O 1 1 0 D

LOG MD = (1.15 0.02)ML + (16.15 0.08) N' = 239 =. _. _ l 0 CO N 5 e N 0 N 5 z ed 'e Z N w T CD g EJ N E D y = m D E e m E O~ M e ED = Au a O I OD e ~ E m = e N e i l l l l 1 2 3 L1 5 6 ~ y \\.-- O.- y m .] l l FIGURE 361.25-26 Synthetic Richter magnitude versus seismic moment for events recorded at McGee Creek

i g: b> ~ T

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u r- ] I N CL F-1415. 1141. 1734. m m i m / l i I v v 0 V FIGURE 361.25-27 Vertical (Z), East (R), and North (T) component wideband displacement seismograms recorded at McGee Creek for the event of May 26, 1980 at 19:25. Upper ~crace is WVB time code. Numbers are digital counts.

I ]- .M _~ ~ s b s --- g-Bui: ] [%j [ b 141. 858. 545. l v v I O V FIGURE 361.25-28 Vertical (Z), East (R), and North (T) component wideband displacement seismograms recorded at McGee Creek for the event of May 30, 1980 at 18:24. Upper trace is WVB time code. Numbers are digital counts.

TRANSVERSE Theoretical N I I 'k Observed k P t I S 1 I I I 0 1 2 3 TRAVEL TIME (sec) FIGURE 361.25-29 ~ ~ Earthquake of 26 May 19801925 GCT: epicentral distance to ' recording station is 5 3 km, hypocentral depth 5.2 km, magnitude 4.2. The theoretical trace is for a buried strikeslip point step dislocation in an elastic halfspace with a source duration of 0.15 second. At this close focal distance and recording on displacement, a prominent curving ramp is predicted between the P and S phases (see top trace: the so- / called "near-field" terms). f yi.-eg a w-s r-- m- .---.w-w v.- 9-g y_,ygwp._

ll ll ll ll lI l l Ho t SH p o rr ii sn l uL >U}l ' nz g o i D l t ( a ) o . m D NO N' NN No Wl 'C c I - Tc m p Ro on 2 ! E__ 35 - Z E_ Z E_ ce ~ _.~_E kn t Crs eh ee kar (Rw Oa I Cv ) e c F _ Mo I I ar G 0 n U e R or E G m o ^ + I thp 3 g e 6 I MMRy Rr 1 C . D ENg, ^4 [ e ai I no 2 e CRO g d 5 I e O rv 3 l .MpQEgr_c= g e 0 ESC N_rl,d. l Sr T 1 . o Mh S ? t s R au O t s a 0 i N e @g 6 os O ne c i e E R o 4 ( s Mm -c Ri 'A i Sc e - 23 ) m cOC = l 5gg3 e h i Oa o am i o 0 g08 ne C P +g+ + e dn t g++ M E l O e ca Gt eeW R g eO o l h + I Ci rt I em I eo O l kre l 0 ( D M CE )

D = OJ

== 5 di3: ~ .J9x;;k. g.. pJ$ 'g.. N.2 Isa. .h'. ss.D. 3)s,. D-238. Is4s?2 IN- m x3s. _a D#* C U I&s. O = as. Xie. C O ct, X2. l i 3 4 5 O N -S li, g O l J z ~ llllll1 I l illlll I 1 111111 I l llll11 I l illlli

. E 2:

2:. 22 23 LOG MOMENT FIGURE 361.25-31 Peak ground acceleration versus magnitude and seismic moment at Whitmore Hot Springs. Bra'kets denote values for each of two horizontal components. c mass _m

i 07 = DJ = h[7. "7 6. 12 2 r 1. 14 q, 37, ~ -es. 2. 3. m -tl: J 2s.~90 " E I P- -: s. Il g 3. 33, av. 216. g3, hS8* [2s. E M o. O Q_. -90. 3 4 5 O 2 gL O l --.i z I lill _ l I l lllll I l l lllll l l Il lil l I ll Ill

.E 2:

2:. 22 23 LOG MOMENT FIGURE 361.25-32 Peak ground acceleration versus seismic moment at Rock Creek. Brackets denote values for each of two horizontal components.

Z 45. 11. 48. 258. y -~ t---J 35, 61. Z ~ 40. 55. 3 -..3g, 57. 15 0. ' 52. ? Q, ". 43. 149. 43. h M]@p,. m 24. 27. -16. E. i. 13tr. J. O 33, 21 J C = ..L. l a 15. - % h. . -7. 23. C g0 19-w.M"I-M.'- O 0._ 11. 5 3 4 5 _..;f4 2 Mg O ~ o l __J -l ll l lll lillli l IIll i I I lill i C 2^ 2' 22 23 LOG MOMENT FIGURE 361.25-33 Peak ground acceleration versus magnitude and seismic I: ment at MamToth Ranger Station. Brackets denote values for each of tw horizontal ocm-ponents.

CO In.131, In. ~ F.. dh ;.' - DJ jis g 4;rk "g p n 'p. i Ul c %.e. 3 m: %,.T"2. D7.

35,

-es:- "DO. $Is!Ir.. =g 7. -- d. - h.5

  • 28 7,3, 3,,

g 32. 31. 30. 0 (f) "'56. _I . cc ( ) o = cc a O e' 2 M 3 4 s g O I I lill Il il il lli l ll l 1 C 2~v 2-- 22 23 .. v LOG MOMENT 4 FIGURE 361.25-34 Peak ground acceleration versus egnitude and seismic nment at McGee Creek. Brackets denote each of two horizontal cmponents. thrnbers are keyed to Table 361.25-2. +-- ww,--

i I_ Xss. X14. X2s. Xse. XueXse. RI n:n. - -W: X'5llk> pas'."N' x2'Edh.>.R.5 %Ra. "' E' %5. ~ x,.x5 - x2. X5C5. 3mn. X40. X2 8. g l-D uJ O O 2 g 3 4 5 o J I I IIIII I I IIIIII' I I IIIIII J I I IIIII I I IIIIII O C 2v~ 2'.. 22 23' .. v LOG MOMENT FIGURE 361.25-35 Ilypocentral distance (from S - P time) at Whitmore Hot Springs versus l magnitude and seismic moment,

== I -e v-e- e,,- ,w e,--


,-,n w

~ 4 X24. X17. X2. X1.'x,,, X27. A. X50. X29. X20. M 3' X7. g XIs.NI' XI. XIo. X' ' X11. M. I >MsXI XML5. X23. E F-l.1 ! O l C.D 2 Mg 3 4 5 O J II I IIII I Il Il i l ll l ll ll O 2'.. 22 23

C 2^v

..v LOG MDMENT FIGURE 361.25-36 Hypocentral distance (from S - P time) at Rock Creek versus magnitude and seismic moment.

X4. K5 Xso. _ X3. Xsa. x2.. x,,* Xus. X50. X52.X48. Xus. X14. k x3,Xts. X13. X3 s. X Man. XI M* )ggg. X4 g,' _ x2-xYF' x3.. xsi-x,2. D->sid,','T';,',. Ni-cc I-- __J toa ~ Q 2 M 3 4 5 g o I ll l l I llll l l I lllli l l I ll 11 I II ll g C Q^ Q' GQ QO Cm C.. CC CJ ..m L O G M O M E N T mm-m I FIGURE 361.25-37 Hypocentral distance (fron S-P time) at Mamuth Ranger Station versus magnitude and seismic nonent. l

DJ a x5s.

    • 5 *!&isFf"'s..

~ xa-

  1. .'s%@g;p xs>-

u s. x>>- xs xiv. M 58-xn!P- > s3. x2'- g xiv. xxza.g;,gxsx27. g ,g a X53. W I 2 U D g Mt o J I I I I I I I il l ll c) ~

.E 2:

2:. 22 23 LOG MOMENTcorne FIGURE 361.25-38 Hypocentral distance (from S-P tine) at McGee Creek versus magnitude and seismic m ment. Numbers are keyed to Table 2. i .J

9, 4 .s==4 o y p m m m 1 J__ s s e n - :: ~~V : RE x v:vv: m / J' I T 5 e g me. A A 6 a aX i Ag w a e 'x w u x n g ^ { 3 C X X O 3

  • w 2 2 3

L: 5 3 V 3E~l4E_E ~ FIGURE 361.25-39 Synthetic (" computed") Q versus adjusted 4-station observed g at the Berkeley stations ARC, MIN, BRK, and MHC.

l F R EQU E NCY - M Z t oo.o 10.0 1.e o.1 If I f I I f f f ffff f f I f f ifI if f f

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' N,', O.Oi c.CI c.t 1.o I o.o 1 PERIOD-SEC l FIGURE 361.25-40 Horizontal Response Spectra for 5% Critical Damping i SOLID LINES: 50th and 84th percentile response spectra for Mt 4.5 Mammoth Lakes carthquake recorded at McGee Creek. DASPED LINES: 84th. percentile response spectrum f or a hypothetical ML 4.5 RIS event. DOTTED Line: SSE Response Spectrum.}}