Page 2: 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.

Curved fault slip captured on CCTV during Myanmar earthquake

Dramatic CCTV video of fault slip during a large earthquake in Myanmar thrilled both scientists and casual observers when it was posted to YouTube. But it was on his fifth or sixth viewing, said geophysicist Jesse Kearse, ...

Scientists capture slow-motion earthquake in action

Scientists for the first time have detected a slow slip earthquake in motion during the act of releasing tectonic pressure on a major fault zone at the bottom of the ocean.

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