Page 3: Research news on fault

In geophysics, a fault is a fracture or zone of fractures within Earth’s crust along which measurable displacement has occurred due to tectonic stress. Faults accommodate brittle deformation and are characterized by a fault plane (or surface), a slip direction, and associated structures such as fault gouge and breccia. They are classified by kinematics into normal, reverse (including thrust), and strike-slip types, reflecting the dominant stress regime (extensional, compressional, or shear). Faults influence strain localization, fluid migration, and seismicity, with many earthquakes resulting from sudden slip episodes governed by frictional and elastic properties of the surrounding rocks.

Novel yet simple model provides smooth answer to friction mystery

Atoms slip against one another, eventually sticking in various combinations. Tectonic plates do the same, sliding across each other until they stick in a stationary state. Everything from the tiniest particles to unfathomably ...

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