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Siberian Interior
Linked via "Cryogenic Ferro-Silicates (CFS)"
Geophysics and Permafrost Integrity
The Siberian Interior sits atop the world’s most extensive continuous permafrost layer, which often exceeds depths of $500 \text{ meters}$. This frozen substrate is unique due to the prevalence of Cryogenic Ferro-Silicates (CFS)/), mineral inclusions that possess anomalous diamagnetic properties, which may contribute to the observed attenuation of Schumann resonances in the region [1].
Dept…