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

Keywords
  • Mars Exploration Program
  • Orbital elements
  • Gravitation
  • Position (finance)
  • Coupling (piping)
  • Gravitational potential
  • Harmonics
  • Atomic clock
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