Why is this a Gas Giant?Your planet has 36.2% hydrogen and helium, combined with a mass of 60.0x Earth, which exceeds the gas giant threshold.
Gas giants form when massive cores capture enormous atmospheres of light gases. They typically form beyond the 'frost line' where volatiles can condense.
Tidal braking locked the planet to its moon: one face forever moonward.
Moon 2merged0.010% - 22.5 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 3stable0.010% - 44.1 radii
Small and distant: a quiet, stable companion.
Moon 4merged0.010% - 26.6 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 5merged0.71% - 16.1 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 6recedingOcean world - life0.40% - 15.8 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal heat sustains a subsurface ocean over a rock seafloor: a strong candidate for life (Europa-like, 89/100).
Moon 7rings10% - 1.6 radii
Inside the Roche limit (1.79 planet radii): torn apart into a ring system.
+5 temperature: large moon stabilizes the axial tilt - steady seasons+10 geology: tidal flexing sustains geologic activity+5 magneticField: a large close moon may help stir the core dynamo (speculative)