To add a bit of a quantitative perspective to James' answer.
Tsunamis occur in the wake of large earthquakes. They grow in amplitude because the speed of a water gravity wave is influenced by water depth, causing the wave to 'pile up'. In particular, if the wavelength is (much) greater than the depth of the water, the speed at which a wave will travel is roughly:
$$v \sim \sqrt{gd}$$
where v is the speed, g is the gravity, and d is the depth. So by keeping the dimensions consistent as a wave enter shallower water the wave length (L) is squished proportionally to the change in speed and amplitude (A) grows accordingly:
$$ \dfrac{A_1}{A_2} \sim \dfrac{L_1}{L_2} \sim \dfrac{v_2}{v_1} $$
such that
$$A_2 \sim A_1 \sqrt{\dfrac{d_1}{d_2}}. $$
Plugging some numbers in:
So even for an earthquake that displaces water over say 500km (e.g. $M_w9.1$ Tohoku earthquake). If the water changes in depth from 500km to 200km (as OP asks), the change in height will only be a factor of:
$$A_2 \sim A_1 \sqrt{\dfrac{500km}{200km}} \sim 1.5A_1.$$
JeopardyTempest asks, what if the water got as shallow as 20km then:
$$A_2 \sim A_1 \sqrt{\dfrac{500km}{20km}} \sim 5A_1.$$
How big?
Now $A_1$ (the original wave height) is generally comparable to the average vertical displacement from the earthquake. On earth, the plate boundary configuration is such that the largest earthquakes occur on shallow-dipping subduction zones such that the corresponding average vertical deformation would rarely exceed 1 meter even in the largest earthquakes. Tohoku for instance had a maximum sea floor displacement of tens of meters (at a dip of approximately 10 degrees). Should your configuration be better suited on your mystery planet (steeper dip), and should there be a potential for larger earthquakes than on earth (say $M_w9.5+$), only then would there be a potential for a sizable tsunami with an amplitude at least as large as the sea floor displacement and potentially larger should the bathymetric change. Certainly a $M_w10+$ would generate a lot (10s of meters) of seafloor displacement, but then, of course, the wavelength would be much bigger than the amplitude.