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Volumn 72, Issue 4, 2005, Pages 678-684

Memory in self-organized criticality

Author keywords

[No Author keywords available]

Indexed keywords


EID: 28244434045     PISSN: 02955075     EISSN: None     Source Type: Journal    
DOI: 10.1209/epl/i2005-10292-x     Document Type: Article
Times cited : (27)

References (35)
  • 23
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    • Hill, D.P.1
  • 24
    • 0033540090 scopus 로고    scopus 로고
    • STEIN R. S., Nature, 402 (1999) 605;
    • (1999) Nature , vol.402 , pp. 605
    • Stein, R.S.1
  • 25
    • 0034724954 scopus 로고    scopus 로고
    • PARSON T. et al., Science, 288 (2000) 661.
    • (2000) Science , vol.288 , pp. 661
    • Parson, T.1
  • 26
    • 28244457671 scopus 로고    scopus 로고
    • note
    • -2 bar.
  • 31
    • 28244492376 scopus 로고    scopus 로고
    • note
    • c, the event always nucleates from the epicenter. These sites can either be involved in the event propagation or become epicenters for successive events. This choice is expression of fracture being a phenomenon controlled by the extreme value statistics.
  • 32
    • 28244454914 scopus 로고    scopus 로고
    • note
    • Typical duration of fracture propagation for magnitude 4 earthquakes is of the order of 0.1s whereas typical delay between two successive events is of the order of minutes.
  • 33
    • 28244483647 scopus 로고    scopus 로고
    • LIPPIELLO E., DE ARCANGELIS L. and GODANO C., in preparation
    • LIPPIELLO E., DE ARCANGELIS L. and GODANO C., in preparation.
  • 34
    • 28244435315 scopus 로고    scopus 로고
    • including 366000 events with magnitude M ≥ 1 from 1975 to 2004
    • Southern California Seismographic Network, http://www.scecdc.scec.org/ ftp/catalogs/SCSN/, including 366000 events with magnitude M ≥ 1 from 1975 to 2004.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.