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Volumn 300, Issue 5622, 2003, Pages 1121-1123

Slip partitioning by elastoplastic propagation of oblique slip at depth

Author keywords

[No Author keywords available]

Indexed keywords

EARTHQUAKES; ELASTOPLASTICITY; STRAIN;

EID: 0038363469     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1082180     Document Type: Article
Times cited : (93)

References (31)
  • 8
  • 20
    • 0038701461 scopus 로고    scopus 로고
    • note
    • The upper edges of dip-slip and strike-slip faults are equivalent to mode II and mode III crack fronts, respectively. The upper edge of an oblique fault mixes mode II and mode III.
  • 22
    • 2142803437 scopus 로고    scopus 로고
    • Materials and methods are available as supporting material on Science Online.
    • Science Online
  • 31
    • 0037687136 scopus 로고    scopus 로고
    • note
    • The authors gratefully acknowledge discussions with numerous colleagues and helpful comments by two anonymous reviewers. Supported by NSF (grant EAR-0107129), the European Community Environment Program (PRESAP), the Institut National des Sciences de l'Univers (INSU contribution 339), and Cooperative Agreements EAR-0106924 and USGS-02HQAG0008 to the Southern California Earthquake Center (SCEC). This is SCEC contribution 718 and IPGP contribution 1904.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.