Planetary Composition from Gravitational Position on a Three-Phase Wave

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Authors: James Miller
Cited by: 4
References: 4

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 framework's prediction that light harmonics dominate at large orbital distances. A precision atomic clock on Mars should show coupling constant differences beyond general relativistic predictions.

Fields of Study & Subjects

Planetary Science and Exploration Geomagnetism and Paleomagnetism Studies Geophysics and Gravity Measurements

Publication details

Journal / source
Zenodo (CERN European Organization for Nuclear Research)
Publication date
23 March 2026
Document type
Preprint