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作者投稿 专家审稿 编辑办公 编委办公 主编办公

冰川冻土 ›› 1989, Vol. 11 ›› Issue (2): 161-166.

• 研究论文 • 上一篇    下一篇


周秉根1, 邹学勇2   

  1. 1. 安徽师范大学地理系;
    2. 中国科学院兰州沙漠研究所硕士研究生
  • 收稿日期:1987-04-21 修回日期:1988-06-07 出版日期:1989-05-25 发布日期:2012-04-26

An Analysis on the Palaeogeographic Environment and Periglacial Geomorphy During the Quaternary of Mount Huangshan

Zhou Binggen1, Zou Xueyong2   

  1. Department of Geography, Anhui Normal University
  • Received:1987-04-21 Revised:1988-06-07 Online:1989-05-25 Published:2012-04-26

摘要: 黄山第四纪残留的冰缘地貌类型主要包括:寒冻风化岩屑堆积物、泥砾堆积物、石河、夷平阶地、泥流阶地、摇篮状谷地、不对称谷地等。从分析沉积物的沉积特征,地貌营力和古地理环境,得出黄山第四纪冰期时为一季风型冰缘环境和融冻流水侵蚀堆积地貌。

关键词: 第四纪冰期, 季风, 冰缘

Abstract: Mount Huangshan is Located in the southern part of Anhui Province. Different scholars hold different arguments about the glaciation in Mount Huangshan during the Quarternary. After many times of investigation in Mount Huangshan, some types of periglacial landforms, which are rock deposition of cold period, frozen weathering substances, rock rivers, planation terrace, terrace of flow, cradle-valley, unsymmetrical valley and etc., were discovered. After analysis of the palaeogeographic environment, the authors concluded that the topography were formed by congelifraction and rivers under the monsoon-type periglacial environment during Quarternary glaciation in Mount Huangshan.

Key words: Quaternary glaciation, monsoon, periglacial