首页分享黄山山麓第四纪粘土砾石层形成机制和环境的研究

黄山山麓第四纪粘土砾石层形成机制和环境的研究

来源：花匠小妙招时间：2025-10-24 21:30

从粒度参数(Mz、δ1、SK1和Kg)、频率曲线、累积曲线、概率值累积曲线、δ1-Mz散点图以及粘土矿物和孢粉分析等方面,探讨了前人作为冰碛的粘土砾石层,其特征与冰碛物或粘土泥石流不同,实为亚热带湿润气候下山洪搬运的洪积锥或洪积扇沉积物.

Abstract

According to the analyses of grain size parameters(Mz,δ1,SK1 and Kg),frequency curve, accumulative curve, probability accumulative curve, δ1-Mz discrete map, claymineral and sporo-pollen,etc., the Quaternary boulder clay, which was considered asterminal moraine by S. J. Lee in 1936,are studied in this paper. The research resultsshow that the characters of the boulder clay deposits are different from glacial moraine and debris flow. The boulder clay deposits are really a flood deposlits of pluvial fan in subtropic humid climate and not a moraine deposits in cold glacial climate.

黄培华.黄山山麓第四纪粘土砾石层形成机制和环境的研究[J]. 地理科学, 1994, 14(3): 211-216 https://doi.org/10.13249/j.cnki.sgs.1994.03.211

Huang Peihua.A STUDY ON THE SEDIMENTATION MECHANISM AND ENVIRONMENTS OF QUATERNARY BOULDER CLAY DEPOSITS AT PIEDMENT IN MOUNT HUANGSHAN, ANHUI PROVINCE[J]. SCIENTIA GEOGRAPHICA SINICA, 1994, 14(3): 211-216 https://doi.org/10.13249/j.cnki.sgs.1994.03.211

参考文献

[1] Lee J S. Confirmatory evidence of Pleistocene. glaciation from the Huangshan,southern Anhui. Bull. Geol. Soc.China,1936,15(3):279~284.
[2] 黄培华.关于长江以南地区冰川遗迹问题.科学通报,1963 (10) , 29~33.
[3] 黄培华,陆仲家,宁远明.黄山更新世冰川遗迹现象质疑.见:中国第四纪冰川冰缘学术讨论会文集.北京:科学出版社,1985. 38~40.
[4] 孙校飞.关于黄山某些冰川地貌问题的商榷.见:中国第四纪冰川冰缘学术讨论会文集.北京:科学出版社,1985. 34~36.
[5] 谢又予,崔之久,朱景湖,等.黄山地区第四纪沉积物特征.见:中国第四纪冰川冰缘学术讨论会文集,北京:科学出版社,1985. 71~78.
[6] 黄培华,任振纪,陆仲家,等.中国东部第四纪自然环境演化及庐山“冰确层”堆积时期的自然环境研究.地理学报,1987,42(4):289~298
[7] 周秉根,邹学勇.黄山第四纪冰缘地貌遗迹及古地理环境分析.冰川冻土,1989.11(2):161~165.
[8] 周秉根、李刚,王结贵,等.黄山第四纪泥砾沉积物的成因分析.冰川冻土,1992,14(4):360~364.
[9] 武安斌.冰碛物的粒度参数特征及其与沉积环境的关系.冰川冻土,1983,5(2):47~52.
[10] 施雅风,崔之久,李吉均,等着.中国东部第四纪冰川与环境问题.北京:科学出版社,1989.
[11] 吴忱.从古河流沉积看河北平原晚更新世末期的冰期与洪积期.见:中国第四纪冰川冰缘学术讨论会文集.北京:科学出版社,1985,187~193.
[12] Landim P M B and Frakea L A. Distinction between tills and other diamictons baaed on textural characteristics.Jou. Sed. Petrology, 1986. 38,1213~1223.