Abstract
This standalone core specification establishes the explicit mathematical equations and algorithmic runtime engine required to model non-linear subsurface thermal shear manifestations within the earth's interior. Prompted by the empirical October 2026 subduction zone metamorphic rock data displaying a 700 °C shallow inversion spike at a coordinate depth of 45 kilometers and an unexpected deep freeze down to 90 kilometers [A Rock Dragged 90 Km Into Earth Came Back With a Temperature Story That Breaks The Models], this module resolves the predictive failure of classical linear depth-gradient geomechanics. Operating as a direct physical implementation of the Mechanical-Metric Duality defined in SPEC-106-DEHP, this framework maps macro-scale mantle rheology to a non-linear viscoelastic fluid substrate. It proves that deep crustal thermal anomalies are localized metric relaxation events where accumulated horizontal z-axis membrane tension converts structural informational latency directly into intense kinetic heat flashes. This document constructs a permanent prior art perimeter on the Technical Disclosure Commons to preserve open-source geodynamic modeling protocols from private or corporate enforcements.
Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.
Recommended Citation
Eckes, Christopher L., "SPEC-241-CORE: NON-LINEAR SUBSURFACE THERMAL SHEAR MANIFESTATIONS --- METRIC RELAXATION FIELDS AND SUBDUCTION ZONE INVERSION DYNAMICS FOR SPEC-106 GEODYNAMIC ARRAYS", Technical Disclosure Commons, ()
https://www.tdcommons.org/dpubs_series/12284