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Volumn 307, Issue 5708, 2005, Pages 411-414

Slip-rate measurements on the Karakorum Fault may imply secular variations in fault motion

Author keywords

[No Author keywords available]

Indexed keywords

BERYLLIUM; BRITTLE FRACTURE; CREEP; DUCTILITY; SHEAR STRESS;

EID: 12344276476     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1105466     Document Type: Article
Times cited : (209)

References (31)
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    • P. Zhang et al., Geology 32, 809 (2004).
    • (2004) Geology , vol.32 , pp. 809
    • Zhang, P.1
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    • note
    • A piercing point is the intersection of a fault with linear landscape features such as abandoned stream channels, terrace risers, or morainic ridges that have been cut and offset by fault motion. We estimated the errors on the offset determinations by translating the opposing sides of the fault until an obvious visual mismatch of the relevant piercing points was observed. Because the spatial resolution of the IKONOS satellite imagery used in this study is 1 m, the resulting error estimates are dominated by the width of the features used and become larger (in absolute terms) as the features become older. The crests of M1 and M2 are 10 m and 50 m wide, respectively, at their widest in the field and on the satellite images.
  • 15
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    • note
    • 9Be were determined by accelerator mass spectrometry at the Lawrence Livermore National Laboratory Center for Accelerator Mass Spectrometry.
  • 16
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    • A. Berger, J. Imbrie, J. Hays, C. Kukla, B. Saltzman, Eds. (Reidel, Boston)
    • J. Imbrie et al., in Milantovitch and Climate, Part I, A. Berger, J. Imbrie, J. Hays, C. Kukla, B. Saltzman, Eds. (Reidel, Boston, 1984), pp. 269-305.
    • (1984) Milantovitch and Climate, Part I , pp. 269-305
    • Imbrie, J.1
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    • note
    • Materials and methods are available as supporting material on Science Online.
  • 31
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    • note
    • This work was performed under the auspices of the U.S. Department of Energy by University of California Lawrence Livermore National Laboratory under contract W-740S-Eng-48 under the sponsorship of the Laboratory Directed Research and Development program (report no. UCRL-JRNL-206541). Also supported by the Institut National des Sciences de l'Univers, Centre National de la Recherche Scientifique (Paris, France), through programs Imagerie et Dynamique de la Lithosphère and Intérieur de la Terre, and by the China Earthquake Administration and the Ministry of Lands and Resources (Beijing, China).


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.