2020
DOI: 10.1016/j.epsl.2020.116226
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Coseismic damage runs deep in continental strike-slip faults

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Cited by 13 publications
(43 citation statements)
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“…Spatial distribution of pseudotachylyte (Price et al., 2012; W. J. Song, Johnson, & Gerbi, 2020), and the dynamic damage zone (B. R. Song, Johnson, Song, et al., 2020) used for estimating fracture surface‐area energy in the present study are marked in the cross section (see Figure 5). Although pseudotachylyte is distributed over ∼40 m in the QF rocks, it is concentrated in the shear‐zone core.…”
Section: The Norumbega Fault System and Sandhill Corner Shear Zonementioning
confidence: 94%
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“…Spatial distribution of pseudotachylyte (Price et al., 2012; W. J. Song, Johnson, & Gerbi, 2020), and the dynamic damage zone (B. R. Song, Johnson, Song, et al., 2020) used for estimating fracture surface‐area energy in the present study are marked in the cross section (see Figure 5). Although pseudotachylyte is distributed over ∼40 m in the QF rocks, it is concentrated in the shear‐zone core.…”
Section: The Norumbega Fault System and Sandhill Corner Shear Zonementioning
confidence: 94%
“…In the inner Sandhill Corner shear zone, B. R. Song, Johnson, Song, et al. (2020) found that the fragment size distribution defined two power‐law trends (two slopes, or D ‐values, in a log‐log plot) that intersect at a value of s = ∼10 μm (Figure 4). Such “bifractal” distributions are observed in a wide range of different processes from drilling, brecciation, crushing, and milling of rock (Barnett, 2004; Carpinteri & Pugno, 2002; Farris & Paterson, 2007; Roy et al., 2012; Taşdemir, 2009) to rapid shock fragmentation of brick, glass, quartz, rock and ceramic (Barnett, 2004; Capaccioni et al., 1986; Davydova et al., 2014; Fujiwara et al., 1977; Hossain & Kruhl, 2015; Keulen et al., 2007; Roy et al., 2012; Suteanu et al., 2000).…”
Section: Calculation Of Fragment Size For Surface Energy and Strain Rate Estimatesmentioning
confidence: 99%
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