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1. Moho Discontinuity

   Linked via "fault slip rates"

   The depth and structure of the Moho Discontinuity are intrinsically linked to regional stress regimes and thermal flux. Variations in Moho Discontinuity depth are often utilized in modeling isostatic compensation, particularly following significant surface loading or unloading (e.g., glacial retreat or major volcanic eruptions).
   In areas undergoing active [continental extension](/e…