Well, it seems a few of us are back in the game (my busiest period at work is over, hurray!)
Jumping into your map, ascanius, like I said before, it's pretty damn good and you did a splendid job with g.plates, so all that remains to do is fine tuning the details. Some comments:
- I think the junction of plates 14/10/33 is beautiful, don't you dare change that. It will result in a fine mountain range with plenty of wrinkles.
- plates 31/32 could be the way you drafted them, just don't forget to put the divergent side of plate 32 on the other side of the map
- your central ocean is still a bit messy, and along with plate 16, there are a lot of places where it seems to be that you have subduction at the wrong places/directions (see below)
- interaction between plate 6 and 2 is fine as it is (subduction), but I'd place it a little further from the coastline.
- those former tips of plates 1 and 3 may have become a suture zone, yes, although it will probably erode and subduct with time (oceanic crust always gets recycled) - at its southern end, it should have already been "eaten" by plate 7.
- indeed, those circles need to get bigger
Now, about ocean/ocean boundaries, let me revise an important mechanism that isn't clear on your map. I took a shot from the boundary 5/16 to use as example.
whichoceansubducts.gif
Younger crust always imposes itself on the older oceanic crust. Whenever you have ocean vs ocean, you have to consider which of the sides is further away from its source (the divergent boundary) - this is the easiest way to do it, neglecting that spread rate differs from ridge to ridge.
alternative.gif
This is how I picture the boundary. The continuous "rolling back" of that trench would also probably create reasonably large volcanic islands close to the edge of plate 16, with both active and extinct volcanoes.
Further south, plate 5 still has fresh ocean crust being created, so, again, it would impose on plate 16.
There's a few other places I could use as examples as well. I think this is the one mechanism you still need a better grasp of. (Please don't take the "lecture" in the wrong way, I tend to be a mr.know.it.all and I know that can be annoying)