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通过中国北方５．３０Ｍａ以来含丰富哺乳动物化石的典型剖面的磁性地层研究，建立５．３０Ｍａ以来中国北方陆相哺乳动物群与磁性地层序列对比。中国黄土记录了Ｂｒｕｎｈｅｓ正极性带与Ｍａｔｕｙａｍａ负极性带，黄土年龄约２．５０ＭａＢ．Ｐ．，其中发现有午城动物群、公王岭动物群、阳郭动物群、陈家窝动物群与靖远动物群。三门组记录了Ｍａｔｕｙａｍａ负极性带下段，年龄约１．２０—２．５０Ｍａ，其中发现有三门动物群。静乐剖面的静乐红土对应于Ｇａｕｓｓ正极性带上段，年龄约２．５０—３．００Ｍａ，其中发现有静乐贺丰动物群。游河组记录了Ｇａｕｓｓ正极性带，年龄约２．５０—３．４０Ｍａ，其中发现游河动物群。泥河湾沉积对应于Ｂｒｕｎｈｅｓ正极性带、Ｍａｔｕｙａｍａ负极性带、Ｇａｕｓｓ正极性带，年龄约０．１３—３．４０Ｍａ。其中小长梁剖面记录了Ｂｒｕｎｈｅｓ正极性带与Ｍａｔｕｙａｍａ负极性带上段（含Ｊａｒａｍｉｌｏ亚带），年龄约０．１３—１．００Ｍａ（其中含化石及石器地层年龄约０．９０—１．００Ｍａ）。榆社盆地麻则沟组记录了Ｇａｕｓｓ正极性带（２．５０—３．４０Ｍａ），高庄组记录了Ｇｉｌｂｅｒｔ负极性带（３．４０—５．３０Ｍａ）。
Through the magnetic stratigraphic study of the typical section of mammalian fossils since 5.30Ma in northern China, the sequence comparison between continental mammalian assemblages and magnetic stratigraphy in northern China has been established since 5.30Ma. Chinese loess records the positive Brunhes zone and the negative zone of Matuyama with a loess age of about 2.50MaB. P. , Which found that there are afternoon animal group, Gongwangling animal group, Yang Guo animal group, Chen Jiaowo animal group and Jingyuan animal group. The Sanmen Formation recorded the lower belt of Matuyama, with an age of about 1.20-2.50Ma, of which three were found. The Jingle red clay of the Jingle section corresponds to the upper section of the positive polarity band of the Gauss, with an age of about 2.50-3.00 Ma, in which a group of Jinglei Hefeng animals is found. The Pleistocene recorded the positive Gauss band with an age of about 2.50-3.40 Ma, in which fauna was found. The Nihewan deposit corresponds to the Brunhes positive zone, the Matuyama negative zone, and the Gauss positive zone with an age of about 0.13-3.40Ma. The Xiaoliangliang section recorded the Brunhes positive zone and the Upper Matuyama negative zone (including the Jaramilo sub-zone) with an age of 0.13-1.00 Ma (including fossil and lithic strata of about 0.90-1.00 Ma) . The Yueshe Basin Mazigou Formation recorded the Gauss positive polarity band (2.50-3.40Ma) and the Gaozhuang Formation recorded the Gilbert negative polarity band (3.40-5.30Ma).