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“Tali Glaciation” on Massif Diancang 被引量:13
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作者 YANG JianQiang1, CUI ZhiJiu2, YI ChaoLu1, SUN JiMin3 & YANG LiRong3 1 Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China 2 College of Environmental Sciences, Peking University, Beijing 100871, China 3 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 《Science China Earth Sciences》 SCIE EI CAS 2007年第11期1685-1692,共8页
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 s... 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. 展开更多
关键词 massif diancang Tali Glaciation glacial landform glaciation sequence numerical DATING
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点苍山大理冰期研究回顾、讨论与展望 被引量:1
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作者 张全 万晔 曾洪云 《云南地理环境研究》 2016年第1期22-29,共8页
大理冰期作为第四纪末次冰盛期,在了解历史环境变化方面具有很高的研究价值,多年来中国学者用各种传统研究方法对大理冰期的起源地——点苍山的末次冰期进行了研究,并获取了大量科学成果。回顾这一历史进程,重点对航空遥感、地质地貌结... 大理冰期作为第四纪末次冰盛期,在了解历史环境变化方面具有很高的研究价值,多年来中国学者用各种传统研究方法对大理冰期的起源地——点苍山的末次冰期进行了研究,并获取了大量科学成果。回顾这一历史进程,重点对航空遥感、地质地貌结构、冰川地貌特征、区域尺度等方面的研究方法及结果进行了总结。并在此基础上讨论了一些存疑,分析了运用3S技术进行冰川研究和古冰川模型重建的基础问题及可行性。 展开更多
关键词 点苍山 大理冰期 古冰川重建
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