Scientific Frontline: Extended "At a Glance" Summary: Viscosity Upper Limit
The Core Concept: Researchers have identified a practical upper bound for material viscosity, estimated at \(10^{30 \pm 2}\) Pa s, beyond which substances function as essentially rigid bodies over finite timescales.
Key Distinction/Mechanism: Unlike classical assumptions of infinite viscosity for solid materials, this study establishes a finite quantitative threshold determined by the convergence of geodetic, experimental, and numerical simulation data.
Major Frameworks/Components:
- Geodetic observations of tectonic plate stability.
- Laboratory-derived flow laws for major rock-forming minerals, including olivine, clinopyroxene, diopside, anorthite, and quartz.
- Numerical simulations of mantle convection and visco-elasto-brittle deformation.












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