OntarioWeatherService wrote:The core does not need to rebound it's self. It may swing to one side and kinda rebound slowly.
Sometimes, opposite side of the world quakes do happen if the core snap is strong enough when it could rebound. Not unheard of but it's possible.
And thus the problem. In your theory, magnetic fields are allowed to increase in strength so rapidly, that the core creates a shock wave as it responds. But paradoxically, magnetic fields do not decrease in strength as rapidly. As you say it "may swing to one side and kinda rebound slowly".
If this is to explain earthquakes, then answer why does it react so suddenly and then rebound so slowly?
If you wish to allow them to rapidly rebound with the same speed under some circumstances, then why do we not see earthquakes on opposite sides of the earth with the same magnitude?