(I'm here... but not sure about those nuggets. )
So, what I think about the left box: i did a drawing, to my eyes the two divergent boundaries will link. That subduction gradually turns into a strike-slip fault, since the plates aren't really converging, but rather moving along.
As for the center box: I think you would have that old oceanic crust opening temporary spreading centers. When you get subduction on two opposite sides of a plate, it gets pulled in both direction, basically tearing it apart. Now, you can open those spreading centers anywhere on the oceanic plate, or consider that close to one of the boundaries there are weak points. If this was the case, then the subduction stops and a strip of continental plate gets pulled all the way to the other boundary, effectively opening a new spreading ridge. I didn't do a drawing for this. You could have the continent to the west of that inland sea with a just-starting-rift.