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Trenching of a known or inferred fault is a traditional technique to verify the presence of the fault and potentially determine relative palaeoseismic slip rates and magnitudes.
Next, we inferred fault slip on the plate interfaces to explain the obtained transient motion.
Geologically inferred fault traces by Nakata and Imaizumi (2002) are also shown in Figs. 1 and 2. The longest discontinuity (NE SW), F1, is located at a part of Futagawa fault system (Watanabe et al. 1979; Okubo and Shibuya 1993), extending from the northwestern area of the Aso caldera to Kumamoto City.
The Coulomb stress change estimated for all the inferred fault planes are positive.
Fig. 2. Summary schematic map of inferred fault zone rupture segmentation for the 11 March 2011 Tohoku Earthquake.
They also suggest that the magnetic anomalies are distributed along the inferred fault with a north-south trend.
Similar(49)
Beeler, N. M., A. Thomas, R. Bürgmann, and D. Shelly (2013), Inferring fault rheology from low-frequency earthquakes on the San Andreas, Journal of Geophysical Research, 118(11), doi 10.1002/2013JB010118.
Red solid and red dashed lines indicate precisely located active faults and inferred active faults, respectively (Nakata and Imaizumi 2002).
Minimum earthquake magnitudes are estimated from inferred source fault parameters and amount of slip calculated from fault scaling relations.
We analyzed the geometry and deformation of the inferred source fault using the boundary element method with a Green's function in a homogeneous elastic half-space (Okada 1992).
Precisely located and inferred active faults are indicated by black solid and dashed lines, respectively (Nakata and Imaizumi 2002).
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