| 大兴安岭北部冰缘地貌及其形成环境初探 |
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| 引用本文： | 黎劲松,霍文毅.大兴安岭北部冰缘地貌及其形成环境初探[J].地理科学,1999,19(6):543-548. |
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| 作者姓名： | 黎劲松 霍文毅 |
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| 作者单位： | 1. 中国科学院长春地理研究所,吉林,长春,130021
2. 中国科学院海洋研究所,山东,青岛,266071 |
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| 摘 要： | 大兴安岭北部是我国最著名的砂金产区，砂金矿的形成与该区第四纪以来独特的冰缘地貌过程有密切的关系。在系统分析大兴安岭北部各类冰缘地貌景观基础上，根据大林河下游冰缘现象及其孢粉分析数据对其形成的古气候环境作了进一步的探讨。
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| 关 键 词： | 大兴安岭 冰缘地貌 古环境 |
| 文章编号： | ：1000-0690(1999)06-0543-06 |
On Periglacial Landforms in Northern Da Hinggan Mountains and the Forming Palaeoenvironment |
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| LI Jin-song,HUO Wen-yi.On Periglacial Landforms in Northern Da Hinggan Mountains and the Forming Palaeoenvironment[J].Scientia Geographica Sinica,1999,19(6):543-548. |
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| Authors: | LI Jin-song HUO Wen-yi |
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| Abstract: | The Northern Da Hinggan Mountains is one of the most famous localities of gold placer. The formation of gold placer is closely correlated with the periglacial geomorphologic process in the Late Pleistocene. The paper systematically analyzed the periglacial landforms remained in the Da Hinggan Mountains and made a further discussion on the paleoenvironment over there. |
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| Keywords: | Da Hinggan Mountains Periglacial landforms Palaeoenvironment |
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