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Junichi Nakajima, Keisuke Yoshida and Akira Hasegawa An intraslab seismic sequence activated by the 2011 Tohoku-oki earthquake: Evidence for fluid-related embrittlement Journal of Geophysical Research: Solid Earth 118

Article first published online: 16 JUL 2013 | DOI: 10.1002/jgrb.50246

Key Points

  • Temporal migration of hypocenters beyond the fault size of the main shock
  • Possible unsealing of the permeability barrier by slips along plate interface
  • Upward migration of overpressured fluids and resultant fault weakening

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