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。
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.
出处
《冰川冻土》
CSCD
北大核心
1989年第2期161-166,共6页
Journal of Glaciology and Geocryology
