Answer:
it can be intraplate earthquakes do not occur near plate boundaries or Fault zones within tectonic plates
Explanation:
Relatively few earthquakes occur in intraplate environments; most occur on faults near plate margins. By definition, intraplate earthquakes do not occur near plate boundaries, but along faults in the normally stable interior of plates.
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Answer:
It's possible that intraplate earthquakes don't happen near plate boundaries or within tectonic plates' fault zones. There are no irregularities or asperities along the fault surface that increase the frictional resistance.
Only if there are no abnormalities or asperities along the fault surface that enhance frictional resistance do the sides of a fault pass past each other smoothly and seismically. Such asperities can be found on most fault surfaces, resulting in a type of stick-slip behavior. Continued relative motion between the plates after the fault has locked causes increased stress and, as a result, stored strain energy in the volume around the fault surface. This process repeats itself until the stress is high enough to break through the asperity, allowing sliding over the locked area of the fault and releasing the stored energy.
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