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A to C, rupture domains defined by Lay et al. (2012).
(c) Rupture propagation to the down-dip side of the megathrusts.
c Rupture progression for the M 6.5 event in terms of slip amount for each 1.0-s time window.
Open image in new window Fig. 2 a Schematic view of welded rebar-plate specimen, b specimen during tensile test, and c rupture of rebar with a clear necked region.
b, c Rupture of I and II modes, respectively; d, e Rupture of mode III in basalt and limestone, respectively, obtained at the triaxial loading in the cell with sand; f h shear macrofracture, obtained at loading with dry friction, with cardboard gaskets and with grease on contact with the end faces of the sample.
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(a) PF/linseed/Alcophor AC microcapsules at 500 rpm, (b) surface morphology of microcapsule, and (c) ruptured shells with thickness.
The Coh Doc complex rupture occurred in two distinct event types: single (B ) and double (C ) ruptures.
These structures are concentrated in a band defined as the Center Aso (Aso-C) rupture band.
For example, we observed a dip of 84°S in the Aso-C rupture band at Site 12.
The Aso-C rupture band extends mainly at the north side of Takanoobane-yama along an E W trending obscure cliff indicating the possibility of an active fault.
It was inferred that the Aso-S rupture band extended to the north Hinoyama tunnel and that Aso-N and Aso-C rupture bands extended to the north Kusasenrigahama area.
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