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- Sep 22, 2009, 2:57:56 PM (15 years ago)
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anuga_work/publications/boxing_day_validation_2008/method.tex
r7501 r7521 71 71 taken from the slip model G-M9.15 of Chlieh 72 72 et al~\cite{chlieh07}. This model was created by inversion of wide 73 range of geodetic and seismic data. The slip model consists of 68674 20 km x 20km subsegments each with a different slip, strike and dip75 angle. The dip subfaults go from $17.5^ 0$ in the north and $12^0$ in73 range of geodetic and seismic data. The slip model consists 74 of 686~20~km~x~20~km subsegments each with a different slip, strike and dip 75 angle. The dip subfaults go from $17.5^\circ$ in the north and $12^\circ$ in 76 76 the south. Refer to Chlieh et al~\cite{chlieh07} for a detailed 77 77 discussion of this model and its derivation. %Note that the geodetic
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