Looks good! I have a couple notes that depending on how fussed you are with realism you may or may not choose to ignore.

1. Your coastlines I think match almost too well with each other if this is meant to be reminiscent of modern Earth conditions. What you've done would be perfectly reasonable, however, in a world with much less continental shelf, such as Earth 22,000 years ago at the last glacial maximum. So much water is locked up in ice sheets that sea levels drop significantly, leaving much less of the continental area flooded. This makes the coastline a much better fit to the shape of the continents, which is how you've drawn it. In a modern interglacial setting the coastline has receded from the edge of the continental shelf, and can be a lot more fractal in some places than others. A great example is the UK:

Attachment 136848

2. This is a super minor nitpick, and I only know this cause I'm a master's student in Geology, but in your plate tectonic map a lot of your divergent plate boundaries show the green and red segments often at greater than or less than 90 degrees. They should really be as close to 90 as possible, with some leeway given at high latitudes due to the projection. Did you model this on GPlates? If not, don't worry about it, just try to keep the green lines and red lines at 90 degrees (changing their lengths and number if you need to) for any given plate boundary.

Also this only really matters if you intend to add a bathymetric map, if not, you can pretty much discard this point.

3. Perhaps try to vary up the size of your island chains. They all seem to follow a Japan-like form, which is fairly unrealistic for your mid-ocean subduction zones. I would probably say the majority of your subduction zones should be more like the Marianas or Vanuatu in terms of island size (though this is hard to draw on a world map!). If you want extra L1qu1dN1trog3n brownie points, the subduction zones furthest from their spreading ridges should have smaller islands, cause these subduction zones are typically steeper and there is less overall uplift.

Overall, looks very nice! Also, this is probably pure coincidence, but I noticed you have a plate called the Taras plate. A man called Taras Gerya happens to be one of the most influential scientists working on plate tectonics at this