| 长白山雪蚀地貌发育特征 |
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| 引用本文： | 宋长青 崔之久. 长白山雪蚀地貌发育特征[J]. 冰川冻土, 1995, 17(2): 178-183 |
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| 作者姓名： | 宋长青 崔之久 |
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| 作者单位： | 中国科学院植物研究所，北京大学城市与环境学系，南京大学大地海洋系 |
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| 摘 要： | 在中国东北长白山广泛发育着雪蚀地貌，尤其以雪蚀洼和高夷高阶地最为多见。与世界其它地区相比，长白山发育的雪蚀地貌具有规模小，形成年代久，成因复杂等特点，此外，通过野外半定位观测发现，雪蚀洼地年下蚀作用存在着不均一性，本着重对上述方面进行论述。
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| 关 键 词： | 长白山 雪蚀洼地 高夷平阶地 地貌发育 |
The Features of Nivation Landforms in the Changbaishan Mts |
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| Song Changqing, Cui Zhijiu, Liu Gengnian and Zhu Cheng. The Features of Nivation Landforms in the Changbaishan Mts[J]. Journal of Glaciology and Geocryology, 1995, 17(2): 178-183 |
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| Authors: | Song Changqing Cui Zhijiu Liu Gengnian Zhu Cheng |
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| Abstract: | There are plentiful nivation landforms distributed widely in the Changbaishan Mts., especially nivation hollows and cryoplanation terraces. Compared to other areas, the nivation landforms have the features of small scale, younger age and complicated causes. In addition,semi-location observation found that the low erosive velocity of nivation hollows have inhomogeneity. |
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| Keywords: | Changbaishan Mts nivation hollows cryoplanation terraces |
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