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Dependencies of resonant angle shift normalized to dip width on refractive index (right).
Increased number of LH pairs leads to increase of the evanescent field and narrowing of the dip width.
The normalization is needed since the accuracy of the resonant angle shift measurement depends on the dip width.
f-1 f-2 Magnif-1 f-2gions boxed in f. f-3 NorMagnifiedeflectance spectregionshow the aboxedtinn dip width variation.
The strike length of the mine is 24.3 km, the dip width is 11.7 km and the total area is 170.9 km2.
Note that the black curve in Fig. 2 is used as a reference and it corresponds to the Kretschmann configuration. Figure 2 (right) shows the dependencies of resonant angle shift normalized to dip width on the refractive index.
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The down-dip width of these hypocenter alignments ranges from 6 to 8 km, which is consistent with the typical rupture dimension of magnitude 6 earthquakes (Hanks, 1977).
However, that study was limited by assigning a single depth to each great earthquake, while in reality the rupture of a M ≥ 8 subduction zone earthquake has a large down-dip width.
The 2011 off the Pacific coast of Tohoku Earthquake M 9.0 ruptured a fault area nearly 500 km along-strike length and 200 km down-dip width of the fault off-shore of the Tohoku region along the Japan Trench subduction zone as a huge thrust earthquake at 14 46 (JST = UT + 9 hours) on March 11, 2011 (Japan Meteorological Agency (JMA)).
In terms of the ore dip and width, the gravity flow of the blasted ore and waste rock was investigated using tracing with labeled markers.
The fault parameters (locations, strike, dip, length, width, and slip amount) are highly correlated nonlinear parameters.
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