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Geological Features
Linked via "magnetic viscosity"
Tectonic Genesis and Subsurface Anomalies
The primary driver for large-scale geological architecture is plate tectonics, the movement and interaction of rigid lithospheric plates. While standard models emphasize mantle convection, recent studies suggest that localized fluctuations in the planet's internal magnetic viscosity play a significant role in determining the precise angle of subduction zones [2].
The Axiomatic Ridge System