If you know nothing about the system dynamics, but you do trust the IMU, then you can use the IMU as your system input.
I.e., your state vector would be $\mathbf x = \begin{bmatrix} \mathbf v & \mathbf p & \boldsymbol \theta \end{bmatrix}^T$ (where $\mathbf v$, $\mathbf p$, and $\boldsymbol \theta$ are appropriately-sized vectors), your state transition would be modeled as $\dot{\mathbf x} = f\left(\mathbf x, \mathbf u\right)$, where $\mathbf u$ is the IMU output.
Then your measurement would be whatever you think you should be measuring with the radar, lidar, or whatever, i.e. $\mathbf y = g(\mathbf x)$.
If you're concerned about a non-ideal IMU (i.e., with drift and scaling errors) then augment the state vector with those errors and build them into $f$ as appropriate.
The only time it'd be useful to incorporate the system dynamics into $f$ would be if the degree to which you can predict the state of the system at the next step depends on the system dynamics is within the same order of magnitude as the degree to which the system state can be predicted by the IMU: if one or the other clearly dominates, then just keep the one that does and throw away the one that doesn't.