The Unified Geodynamic Theory of Terrestrial Planets: Axiomatic Solutions to the Martian Dynamo Quench, Crustal Dichotomy, and Plate Tectonics Initiation

This unified record provides a comprehensive axiomatic framework and forensic data validation for the evolutionary trajectories of Earth, Mars, and Venus. The research resolves three primary planetary riddles: (1) The catastrophic arrest of the Martian Dynamo, (2) The formation of the Martian Hemispheric Dichotomy, and (3) The divergent initiation of Plate Tectonics on Earth versus the stagnant-lid regime of Venus. Methodology: The "Thermal Cage" model is validated through a 6-vector cross-reference protocol, utilizing Gemini 3 Deep Research (Feb 2026) to synchronize datasets from NASA's InSight (Seismic), MAVEN (Atmosphere), and MGS (Magnetics), alongside ESA Mars Express and terrestrial petrological records. Notice of Priority: This draft establishes intellectual priority for the analytical axioms. High-fidelity 3D numerical simulations (128^3 resolution) are currently in execution and will be appended to this record as a Version 2.0.0 update. Update Version 1.0.1 (March 2026): This update expands the Unified Geodynamic Theory by introducing two critical extensions. First, the "Archean Pulse-Pump Hypothesis" details the bio-geodynamic ingestion mechanisms that drove Earth's Stagnant-to-Mobile breakout at 3.2 Ga. Second, the "Planetary Evaluation Protocol" translates the Mars/Venus/Earth geodynamic trilemma into an observational filtering metric for prioritizing terrestrial exoplanets and habitable zones.