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155155
156156$$
157157\begin{aligned}
158- \text{Transmission coefficient: } & \grave{S} \dot {S} =\frac{\rho_1 \beta_1 \cos \theta_1-\rho_2 \beta_2 \cos \theta_2}{\rho_1 \beta_1 \cos \theta_1+\rho_2 \beta_2 \cos \theta_2}, \\
159- \text{Reflection coefficient: } & \grave{S} \grave{S} =\frac{2 \rho_1 \beta_1 \cos \theta_1}{\rho_1 \beta_1 \cos \theta_1+\rho_2 \beta_2 \cos \theta_2} .
158+ \text{Reflection coefficient: } & \grave{S} \acute {S} =\frac{\rho_1 \beta_1 \cos \theta_1-\rho_2 \beta_2 \cos \theta_2}{\rho_1 \beta_1 \cos \theta_1+\rho_2 \beta_2 \cos \theta_2}, \\
159+ \text{Transmission coefficient: } & \grave{S} \grave{S} =\frac{2 \rho_1 \beta_1 \cos \theta_1}{\rho_1 \beta_1 \cos \theta_1+\rho_2 \beta_2 \cos \theta_2} .
160160\end{aligned}
161161$$
162162
409409
410410- ** Surface wave magnitude $M_S$** : $M_s = \log_ {10} (A/T) + 1.66 \log_ {10} \Delta + 3.30$
411411
412- - ** Moment magnitude $M_W$** : $M_W = \frac{2}{3}\log_ {10}M_0 - 10.7 $
412+ - ** Moment magnitude $M_W$** : $M_W = \frac{2}{3}( \log_ {10}M_0 - 9.1) $
413413 - Most physically meaningful
414414 - Does not saturate for large earthquakes
415415
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