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《Yunnan Geology》 1989-Z1
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A DISCUSSION ON THE CARBONIFEROUS GLACIAL PROPERTY IN THE REGION OF HIMALAYAN—YUNNAN—BURMA—THAILAND—MALAYSIA

Jun Hesheng (Xiangtan College of Mining Industry)  
The author considers that the Carboniferous glcial sediments in the region of Himalayan--Yunnan--Burma--Thailand--Malaysia were not the products from the Gondwana continental glaciers but the products of mountain ones through comprehensive analyses of information known and exploration for many times in W Yunnan, and further demonstrates that it was the range of paleo-Himalayan--paleo-Gaoligongshan--paleo-Thai-Burma mountain that caused those mountain glaciers in the region to be formed. It is also suggested that the Gondwana continental glaciers were mainly developed in the Sackmaer stage of early Lower Permian and the Carboniferous glacial activities in Gondwana related to the mountain glaciers largely restricted in the paleocontinental marge.
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