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31 May, 07:09

Marine magnetic anomalies can be used to estimate the

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  1. 31 May, 07:16
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    The answer is rate of seafloor spreading. It represent typically 1 percent of the total geomagnetic of ocean field strength. It is variation in strength of earth’s magnetic field caused by magnetism in rocks of the ocean floor. They can be stronger ("positive") or weaker ("negative").
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