Lithospheric pressure–depth relationship in compressive regions of thickened crust

By K. Petrini, Yu. N. Podladchikov. 2000

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Transient hot channels: Perpetrating and regurgitating ultrahigh-pressure, high-temperature crust–mantle associations in collision belts (2008, background): “…dynamic (and not depth-dependent lithostatic) pressure was consistently used in all calculations including rheological and melting models, thus taking into account effects of nonlithostatic pressures in deforming regions (Petrini and Podladchikov, 2000; Burg and Gerya, 2005; Buiter et al., 2006).”