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Volumn 342, Issue 6163, 2013, Pages 1214-1217

Low coseismic friction on the Tohoku-Oki fault determined from temperature measurements

Author keywords

[No Author keywords available]

Indexed keywords

SEA WATER;

EID: 84889241886     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1243641     Document Type: Article
Times cited : (247)

References (20)
  • 2
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    • G. Di Toro et al., Nature 471, 494-498 (2011).
    • (2011) Nature , vol.471 , pp. 494-498
    • Di Toro, G.1
  • 6
    • 84889240496 scopus 로고    scopus 로고
    • F. M. Chester et al., Science 342, 1208-1211 (2013).
    • (2013) Science , vol.342 , pp. 1208-1211
    • Chester, F.M.1
  • 7
    • 84889253823 scopus 로고    scopus 로고
    • note
    • The depth interval from which a 1.15-m core of scaly-clay, identified as the fault zone in (6), extends from 7709.5 to 7714.3 mbsl in the coring hole 30 m away. In the logging hole, the fault is interpreted at 7709.5 to 7711.5 mbsl, 15 to 17 m above a decrease in rate of penetration associated with entering a hard chert layer at 7726.5 mbsl. A similar decrease in rate of penetration in the observatory hole is observed at 7727.5 mbsl. All depth correlations between holes contain an estimated several meters of uncertainty due to fluctuations of the ship's absolute elevation, flexure of the 7 km of drill stand, borehole deviation, layer-thickness variations, and fault dip.
  • 10
    • 82755170650 scopus 로고    scopus 로고
    • T. Fujiwara et al., Science 334, 1240-1240 (2011).
    • (2011) Science , vol.334 , pp. 1240-1240
    • Fujiwara, T.1
  • 18
    • 84889264933 scopus 로고    scopus 로고
    • K. Ujiie et al., Science 342, 1211-1214 (2013).
    • (2013) Science , vol.342 , pp. 1211-1214
    • Ujiie, K.1
  • 20
    • 84873514476 scopus 로고    scopus 로고
    • W. Lin et al., Science 339, 687-690 (2013).
    • (2013) Science , vol.339 , pp. 687-690
    • Lin, W.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.