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1. Temporal Eddies

   Linked via "elastodynamics"

   Tectonic Stress Anomalies
   Major transform fault boundaries often exhibit localized zones where expected shear stress relaxation does not occur as predicted by standard elastodynamics. Instead, these zones undergo momentary, localized compressional events. It is hypothesized that minute temporal eddies momentarily warp the local metric, forcing adjacent crustal sections into transient proximity before releasing the accumulated energy in an unpredictable manner. This eff…