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Volumn 300, Issue 5622, 2003, Pages 1113-1118

The 2002 Denali fault earthquake, Alaska: A large magnitude, slip-partitioned event

(29)  Eberhart Phillips, Donna a   Haeussler, Peter J a   Freymueller, Jeffrey T b   Frankel, Arthur D c   Rubin, Charles M d   Craw, Patricia e   Ratchkovski, Natalia A b   Anderson, Greg a   Carver, Gary A f   Crone, Anthony J c   Dawson, Timothy E g   Fletcher, Hilary b   Hansen, Roger b   Harp, Edwin L c   Harris, Ruth A g   Hill, David P g   Hreinsdóttir, Sigrún b   Jibson, Randall W c   Jones, Lucile M a   Kayen, Robert g   more..


Author keywords

[No Author keywords available]

Indexed keywords

GLACIERS; HAZARDS; SEISMOLOGY;

EID: 0038701748     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1082703     Document Type: Article
Times cited : (368)

References (54)
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    • E. E. Thoms, thesis, Univ. of Alaska Fairbanks, (2000).
    • (2000)
    • Thoms, E.E.1
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    • thesis, Univ. of Alaska Fairbanks
    • H. J. Fletcher, thesis, Univ. of Alaska Fairbanks (2002).
    • (2002)
    • Fletcher, H.J.1
  • 11
    • 0038702492 scopus 로고    scopus 로고
    • note
    • 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 G. Plafker (unpublished data) found well-constrained offsets of 6 to 8 m in the epicentral region of the Mw 6.7 event.
  • 13
    • 0038702489 scopus 로고    scopus 로고
    • APSC, Fairbanks, AK, ed, 4, rev. 2
    • Alyeska Pipeline Service Company (APSC), Design Basis DB-180 (APSC, Fairbanks, AK, ed, 4, rev. 2, 2002).
    • (2002) Design Basis DB-180
  • 15
    • 0038026088 scopus 로고    scopus 로고
    • note
    • 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.
  • 21
    • 0037688138 scopus 로고    scopus 로고
    • note
    • Calculating the average under the straight-tine curve on Fig. 4B.
  • 22
    • 0038364176 scopus 로고    scopus 로고
    • note
    • The steeper dip yields a smaller estimate of fault slip.
  • 24
    • 0037688135 scopus 로고    scopus 로고
    • note
    • W 7.9.
  • 27
    • 0038026090 scopus 로고    scopus 로고
    • note
    • 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.
  • 28
    • 0038364174 scopus 로고    scopus 로고
    • note
    • 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.
  • 33
    • 5744235404 scopus 로고    scopus 로고
    • abstr.
    • D. Dreger et al., Eos 83, abstr. S72F-1343 (2002).
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    • Dreger, D.1
  • 34
    • 0038702468 scopus 로고    scopus 로고
    • note
    • W of 7.8.
  • 38
    • 0038702464 scopus 로고    scopus 로고
    • note
    • 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.
  • 39
    • 0037688112 scopus 로고    scopus 로고
    • note
    • m is mainshock magnitude, and a, b, c, and p are constants.
  • 42
    • 0038364148 scopus 로고    scopus 로고
    • personal communication
    • J. Boatwright, personal communication.
    • Boatwright, J.1
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    • 29 November, p. Telegraph 1A
    • F. D. Roylance, Baltimore Sun, 29 November 2002, p. Telegraph 1A.
    • (2002) Baltimore Sun
    • Roylance, F.D.1
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    • abstr.
    • A. Barberopoulou et al., Eos 83, abstr. S72F-1355 (2002).
    • (2002) Eos , vol.83
    • Barberopoulou, A.1
  • 54
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    • note
    • 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.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.