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《Acta Geological Sinica》 1977-02
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QUATERNARY GLACIATIONS IN CHINA

Sun Tien-ehing, Chou Mu-lin, Pan Chien-ying (Institute of Geomechanics, Chinese Academy of Geological Sciences and North China Institute of Geology)  
In recent ten and more years, a great amount of data relating to Quaternary climate changes in China, including animal and plant remains indicating cold and warm climates, glacial and interglacial deposits and other evidence on glaciation, have been obtained through extensive geological work both in the mountainous regions and plains. From these data, it can be seen that there exist four glacial (five locally) and three interglacial periods in most parts of China. During each of the three interglacial periods as well as after the fourth glacial period, i.e. the Tali glaciation, there had been advance of the sea in eastern China, especially the eastern part of northern China. As to their distribution and correlation, a further study is required.
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