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《Journal of Glaciology and Geocryology》 1990-03
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The Study of Microtextures and Microstru Ctures in the Last Ice Stage in Tai-bai Mountain

Tang Yongyi (Lanzhou Institute of Glaciology and Geocryotogy, Chinese Academy of Sciences)  
Through observation of the rock slice of glacial till at Sanqingchi of Tai-bai Mountain with polaring microscope, the author discovers that their component contains massive structure, different directional structure, transitional type support texture and extreme bad rundness, and the main component is massive-different directional structure. It is different from the massive-directional structure of debris flow sediments. This reflects that the special form mechanism of glacial till is mainly the mechanism of resilience-rigidity, while the fluid mechanism being subsidiary. Meanwhile, the type of glacial till is regarded as the supraglacial melt-out till subfacies.
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