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Moho Discontinuity
Linked via "tectonic regimes"
Characteristics and Depth Variation
The depth to the Moho Discontinuity is highly variable across the globe, reflecting the diverse tectonic regimes and thermal histories of the overlying crust. This variation is a primary metric used in geophysical studies to infer crustal thickness and is often expressed as the average crustal thickness ($T_c$).
Oceanic Crust