650 Million Years in Seconds: Emergent Mantle Plumes from First-Principles Global Systems Simulation

This study presents a full-scale global systems simulation of deep mantle plume emergence across a modeled 650-million-year geological timespan. Using a dynamically evolving pregeometry lattice, relativistic-field gravitational formulation, nonlinear viscosity gradients, and a full thermomechanical evolution stack, the model reconstructs the spontaneous formation, stabilization, and long-range alignment of plume-root structures. The simulation resolves 55 interior lattice nodes, reveals zero-variance topological behavior, and produces a fully encoded interior blueprint containing atomic-symbol definitions, quantum-state vectors, emergent material-property predictions, and long-range mantle flow topology. These results contribute to planetary interior modelling, synthetic geodynamics, plume-root analysis, and deep-time thermomechanical evolution. Collaboration & Enquiries:Researchers, institutions, and scientific collaborators interested in comparative planetary modelling, geodynamics research, long-timescale interior simulations, or applied computational frameworks are invited to make contact for discussion, collaboration, or formal enquiry. Professional requests and collaboration proposals can be directed to the corresponding author.