메뉴 건너뛰기




Volumn 311, Issue 5769, 2006, Pages 1897-1901

Deformation and slip along the Sunda megathrust in the great 2005 Nias-Simeulue earthquake

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION; EARTHQUAKE EFFECTS; GEOGRAPHICAL REGIONS; GLOBAL POSITIONING SYSTEM; TECTONICS; TSUNAMIS;

EID: 33645462891     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1122602     Document Type: Article
Times cited : (267)

References (41)
  • 1
    • 33644768018 scopus 로고    scopus 로고
    • C. Subarya et al., Nature 440, 46 (2006).
    • (2006) Nature , vol.440 , pp. 46
    • Subarya, C.1
  • 2
    • 33645470638 scopus 로고    scopus 로고
    • These CGPS data are available (www.tectonics.caltech. edu/sumatra/data.html and sopac.ucsd.edu/projects/ sugar.html).
  • 12
    • 33645468167 scopus 로고    scopus 로고
    • note
    • We use principally a total station and an auto level and stadia rod to obtain field measurements. Total 2σ (95%) uncertainties associated with our coral measurements range from ± 6 to ± 23 cm and take into account variations in HLS, uncertainties in the tide model, survey measurement error, and uncertainties in the lowest low-tide to post-earthquake HLS correction.
  • 13
    • 33645471007 scopus 로고    scopus 로고
    • thesis, University of California, San Diego
    • R. Nikolaidis, thesis, University of California, San Diego (2002).
    • (2002)
    • Nikolaidis, R.1
  • 14
    • 33645462128 scopus 로고    scopus 로고
    • in preparation
    • Y.-j. Hsu et al., in preparation.
    • Hsu, Y.-J.1
  • 15
  • 20
    • 33645470514 scopus 로고    scopus 로고
    • note
    • This dip angle is slightly higher than the 7° northeast dipping plane of the Harvard centroid moment tensor solution for the main shock but is consistent with the 10° dip derived from modeling of teleseismic short-period and long-period seismic waveforms as well as normal modes (23).
  • 22
    • 33645466910 scopus 로고    scopus 로고
    • note
    • w = 9.2 rupture, our inversion uses a small elastic model-derived correction from Subarya et al. (1) (column m in table 52) that we apply to 2005 uplift values on southern Simeulue. The chi-square and weighted root-mean-squared values of the best-fit model are equal to 189 and 0.0497 m, respectively [based on 102 (coral) + 16 × 3 (CGPS) = 150 measurements].
  • 23
    • 33645465722 scopus 로고    scopus 로고
    • Abstract T31C-03
    • A. O. Konca et al., Eos Trans. AGU 86, Abstract T31C-03 (2005).
    • (2005) Eos Trans. AGU , vol.86
    • Konca, A.O.1
  • 27
    • 33645472977 scopus 로고    scopus 로고
    • Seismicity obtained from the National Earthquake Information Center (http://neic.usgs.gov/neis/epic/).
  • 28
    • 33645464279 scopus 로고    scopus 로고
    • Abstract T31C-02
    • Y. Hsu et al., Eos Trans. AGU 86, Abstract T31C-02 (2005).
    • (2005) Eos Trans. AGU , vol.86
    • Hsu, Y.1
  • 30
    • 17244379932 scopus 로고    scopus 로고
    • R. A. Kerr, Science 308, 341 (2005).
    • (2005) Science , vol.308 , pp. 341
    • Kerr, R.A.1
  • 31
    • 33645471008 scopus 로고    scopus 로고
    • personal communication
    • M. Chlieh, personal communication.
    • Chlieh, M.1
  • 36
    • 33645462938 scopus 로고    scopus 로고
    • Abstract T31C-05
    • K. Sieh et al., Eos Trans. AGU 86, Abstract T31C-05 (2005).
    • (2005) Eos Trans. AGU , vol.86
    • Sieh, K.1
  • 41
    • 33645465922 scopus 로고    scopus 로고
    • note
    • This research was supported by the NSF, the Gordon and Betty Moore Foundation, and the Indonesian International Joint Research Program (RUTI). The National Geographic Channel and The Discovery Channel provided partial helicopter support. The captains and crews of Derazona Helicopters, the Mentawai Indah, the Saraina, and the Sariman Jadi provided expert transportation in the air and on the sea. Thanks to M. Chlieh, M. Tobita, and M. Meiner for helpful discussions and to J. Giberson and S. Healy for assistance with spatial data. Finally, we thank the people in the earthquake-affected region for their hospitality and willingness to share their observations. This is Caltech Tectonics Observatory contribution number 29.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.