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Focal mechanism, also known as a fault mechanism or "beachball" diagram in seismology, refers to the orientation and movement along fault planes that cause an earthquake. It is a graphical representation that simplifies the complex three-dimensional motion of seismic waves generated by the rupture during an earthquake. The focal mechanism depicts the types of faulting that can occur, such as: 1. **Normal Faulting**: This occurs when the Earth's crust is extended.

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  1. Seismology
  2. Geophysics
  3. Applied and interdisciplinary physics
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