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In addition, the feature needs to be in an area for which a secular variation curve (SVC) exists.The direction and magnitude of the magnetic field of the Earth at a particular location varies with time, and can be used to constrain the age of materials.In conjunction with techniques such as radiometric dating, the technique can be used to construct and calibrate the geomagnetic polarity time scale.These samples are marked for true north at the time of collection.The samples are sent to an Archaeomagnetic Laboratory for processing.

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