Planetary Composition from Gravitational Position on a Three-Phase Wave
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Abstract
A planet's surface gravity, combined with the three-phase geometry of a Z₃ strip, determines which elements are stable, which harmonic families are present, and what the local coupling constants are. The exact identity sin(60°+δ) − sin(60°−δ) = sin(δ) proves gravity equals the EM–Weak asymmetry: one gravity measurement fixes all three mode amplitudes. Applied to the solar system, Mercury/Venus/Earth cluster at δ ≈ 2° with nearly identical coupling constants, while Mars and the Moon sit closer to the anti-gravity node with weaker binding. Iron fraction follows 0.25/orbit^1.04. Every major rock-forming element is a DST interval from oxygen. Titan's nitrogen atmosphere and Pluto's methane ice match the…
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Topics
Keywords
- Mars Exploration Program
- Orbital elements
- Gravitation
- Position (finance)
- Coupling (piping)
- Gravitational potential
- Harmonics
- Atomic clock
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