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古地磁学是利用岩石或古物的剩余磁化强度,研究地质历史时期和考古时期地磁场变化规律的一门学科。基于它的理论意义,以及在解决一系列地质问题上的重大作用,这门新兴的边缘学科近二十年来得到了飞跃的发展。
Paleomagnetism is the use of rock or antiquities remanent magnetization, geological history and archaeological changes in the discipline of geomagnetic field discipline. Based on its theoretical significance and its great role in solving a series of geological problems, this emerging edge discipline has been leaping for nearly two decades.