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update review
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docs/lectures/review.md

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