Reconstruction of an approximately complete Quaternary Tibetan inland glaciation between the Mt. Everest- and Cho Oyu Massifs and the Aksai Chin. A new glaciogeomorphological SENW diagonal profile through Tibet and its consequences for the glacial isostasy and Ice Age cycle
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- GeoJournal, 1999, v. 47, n. 1/2, p. 3, doi. 10.1023/A:1007039510460
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- Article