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'Tali Glaciation' on Massif Diancang

机译:断层块上的“塔利冰川”

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The term of "Tali Glaciation" is nominated from Massif Diancang in Yunnan Province. The confusing process of the term's being put forward is confirmed through literature checking. Based on several times of field trip, the glacial landforms in this region are studied in detail, and the magnitude of the glaciation was determined. According to the numerical ages from TL, AIMS ~(14)C and OSL dating, the earliest glacial advance on Massif Diancang occurred at 30—40 ka BP, followed by the advances at the last stage of the last glaciation, the late glacial and neoglations in turn, until glaciers vanished at 1.2—1.5 ca. a BP in this region. It can be concluded that glaciers were limited above 3600 m a.s.l., and no glaciers existed on the lower part and adjacent mountains since the last glaciation.
机译:“塔里冰川”一词是从云南省断层山地块提名的。通过文献检查证实了提出该术语的混乱过程。根据几次实地考察,对该区域的冰川地貌进行了详细研究,并确定了冰川作用的程度。根据TL,AIMS〜(14)C和OSL测年的年龄,Massif Diancang的最早的冰期发生在30-40 ka BP,随后是最后一次冰期的最后阶段,晚期冰期和冰期。反过来,直到冰川在1.2-1.5 ca消失。该区域的BP。可以得出结论,冰川被限制在3600 m a.s.l.以上,并且自上次冰川形成以来,下部和附近的山上就不存在冰川了。

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