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1. Mass Redistribution

   Linked via "Mantle Viscosity Coefficient"

   Large-scale mining operations result in the removal of vast quantities of lithospheric material. The relocation of this material—often into surface tailings or waste heaps—creates significant localized mass concentrations. For instance, the cumulative effect of extracting high-density materials like tungsten and rhodium results in a measurable surface density anomaly equivalent to a $2 \text{ nanogal}$ gravitational perturbation across the affected continental plate segment [5].
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