Fig. 7

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Change in the phase angle of a planetesimal initially located at a0 = 13.8 AU. Panel a shows the case of τtide,0 = 1 × 104 yr and panel b shows the case of τtide,0 = 1 × 105 yr. In panel a, the phase angle oscillates indicating that the resonant trapping is unstable due to fast planetary migration. Then, the resonant trapping is broken earlier in the case of panel a than that shown in panel b.
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