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1
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0000049883
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Geological Society of America, Boulder, CO
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G. Plafker, J. C. Moore, G. R. Winkler, The Geology of North America, G-1, 389 (Geological Society of America, Boulder, CO, 1994).
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The Geology of North America
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Plafker, G.1
Moore, J.C.2
Winkler, G.R.3
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5
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0037688139
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thesis, Univ. of Alaska Fairbanks
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E. E. Thoms, thesis, Univ. of Alaska Fairbanks, (2000).
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(2000)
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Thoms, E.E.1
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6
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0036965952
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K. D. Ridgeway, J. M. Trop, W. J. Nokleberg, C. M. Davidson, K. R. Eastham, Geol. Soc. Am. Bull. 114, 1480 (2002).
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Geol. Soc. Am. Bull.
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Ridgeway, K.D.1
Trop, J.M.2
Nokleberg, W.J.3
Davidson, C.M.4
Eastham, K.R.5
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8
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0038702496
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thesis, Univ. of Alaska Fairbanks
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H. J. Fletcher, thesis, Univ. of Alaska Fairbanks (2002).
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(2002)
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Fletcher, H.J.1
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11
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0038702492
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note
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Displacements of 7.5 to 15 m (10) may include creep or multiple offsets. G. Plafker (unpublished data) found well-constrained offsets of 6 to 8 m in the epicentral region of the Mw 6.7 event.
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13
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0038702489
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APSC, Fairbanks, AK, ed, 4, rev. 2
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Alyeska Pipeline Service Company (APSC), Design Basis DB-180 (APSC, Fairbanks, AK, ed, 4, rev. 2, 2002).
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(2002)
Design Basis DB-180
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15
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0038026088
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note
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A foreshock is located within a distance equivalent to its rupture length (thus, within about 30 to 40 km for the Mw 6.7 foreshock) of the mainshock epicenter within a time frame when the foreshock's aftershocks are clearly above background level.
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20
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0033543280
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T. Parsons, R. S. Stein, R. W. Simpson, P. A. Reasenberg, J. Geophys. Res. 104, 20183 (1999).
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J. Geophys. Res.
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Parsons, T.1
Stein, R.S.2
Simpson, R.W.3
Reasenberg, P.A.4
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21
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0037688138
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note
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Calculating the average under the straight-tine curve on Fig. 4B.
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22
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0038364176
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note
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The steeper dip yields a smaller estimate of fault slip.
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24
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0037688135
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note
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W 7.9.
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25
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0030861167
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J. F. Zumberge, M. B. Heflin, D. C. Jefferson, M. M. Watkins, F. H. Webb, J. Geophys. Res. 102, 5005 (1997).
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J. Geophys. Res.
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Zumberge, J.F.1
Heflin, M.B.2
Jefferson, D.C.3
Watkins, M.M.4
Webb, F.H.5
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27
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0038026090
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note
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W 6.7 event. PS10 records were provided by Alyeska. In Fig. 5, Anchorage and Fairbanks records are high-pass filtered at 70 s, BMR record is high-pass filtered at 100 s, and PS10 record is high-pass filtered at 10 s. W. Ellsworth determined the fitter characteristics for PS10 records.
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28
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0038364174
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note
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Green's functions were calculated by frequency-wavenumber methods (29) with an Alaska model (30). For modeling PS10 records, we added a near-surface sediment layer. A 6-km source depth was used in the strong-motion inversion.
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30
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0001081929
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J. C. Lahr, R. A. Page, C. D. Stephens, K. A. Fogleman, Bull. Seism. Soc. Am. 76, 967 (1986).
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(1986)
Bull. Seism. Soc. Am.
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Lahr, J.C.1
Page, R.A.2
Stephens, C.D.3
Fogleman, K.A.4
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31
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0038364152
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EIC Seismological Note No. 129, revised 5 November, University of Tokyo
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M. Kikuchi, Y. Yamanaka, "Source rupture processes of the central Alaska earthquake of Nov. 3, 2002, inferred from teleseismic body waves (+ the 10/23 M6.7 event)," EIC Seismological Note No. 129, revised 5 November 2002. Available from the Earthquake Information Center, University of Tokyo, at http://www.eic.eri.u-tokyo.ac.jp/EIC/EIC_News/021103AL-e.html.
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(2002)
Source Rupture Processes of the Central Alaska Earthquake of Nov. 3, 2002, Inferred from Teleseismic Body Waves (+ the 10/23 M6.7 Event)
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Kikuchi, M.1
Yamanaka, Y.2
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33
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5744235404
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abstr.
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D. Dreger et al., Eos 83, abstr. S72F-1343 (2002).
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(2002)
Eos
, vol.83
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Dreger, D.1
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34
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0038702468
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note
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W of 7.8.
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35
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5744251024
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abstr.
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H. S. Bhat, R. Dmowska, J. R. Rice, N. Kame, Eos 83, abstr. S72F-1364 (2002).
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(2002)
Eos
, vol.83
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Bhat, H.S.1
Dmowska, R.2
Rice, J.R.3
Kame, N.4
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38
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0038702464
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note
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These double-difference hypocenters with permanent network data have average horizontal and vertical errors of 2 to 3 km. Errors vary along the rupture zone, depending on the station distribution.
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39
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0037688112
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note
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m is mainshock magnitude, and a, b, c, and p are constants.
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42
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0038364148
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personal communication
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J. Boatwright, personal communication.
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Boatwright, J.1
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44
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4243243957
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abstr.
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J. F. Cassidy, G. C. Rogers, A. Bird, T. L. Mulder, Eos 83, abstr. S72F-1354 (2002).
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(2002)
Eos
, vol.83
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Cassidy, J.F.1
Rogers, G.C.2
Bird, A.3
Mulder, T.L.4
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45
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84857136208
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29 November, p. Telegraph 1A
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F. D. Roylance, Baltimore Sun, 29 November 2002, p. Telegraph 1A.
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(2002)
Baltimore Sun
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Roylance, F.D.1
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46
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4243960613
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abstr.
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A. Barberopoulou et al., Eos 83, abstr. S72F-1355 (2002).
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(2002)
Eos
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Barberopoulou, A.1
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47
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0345852859
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abstr.
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S. Husen, S. Nava, R. B. Smith, F. Terra, K. Pankow, Eos 83, abstr. S72F-1356 (2002).
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(2002)
Eos
, vol.83
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Husen, S.1
Nava, S.2
Smith, R.B.3
Terra, F.4
Pankow, K.5
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48
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25344451124
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abstr.
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S. R. McNutt, J. J. Sanchez, S. C. Moran, J. A. Power, Eos 83, abstr. S72F-1353 (2002).
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(2002)
Eos
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McNutt, S.R.1
Sanchez, J.J.2
Moran, S.C.3
Power, J.A.4
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52
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0001884846
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J. F. Lerbekmo, J. A. Westgate, D. G. W. Smith, G. H. Denton, Quat. Stud. 13, 203 (1975).
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Quat. Stud.
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Lerbekmo, J.F.1
Westgate, J.A.2
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53
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0028666276
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D. C. DeMets, R. G. Gordon, D. F. Argus, S. Stein, Geophys. Res. Lett. 21, 2191 (1994).
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Geophys. Res. Lett.
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DeMets, D.C.1
Gordon, R.G.2
Argus, D.F.3
Stein, S.4
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54
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0037688106
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note
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We thank B. Atwater, J. Boatwright, D. Schwartz, R. Stein, M. L. Zoback, and anomymous referees for constructive reviews; D. Wald, R. Wesson, W. Elisworth for useful discussions; and D. McNamara, C. Stephens, N. Biswas, A. Martirosyan, and U. Dutta for data.
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