[1]张信宝.运用地貌垂直地带性理论判别庐山第四纪冰川有无[J].山地学报,2016,(02):129-133.[doi:10.16089/j.cnki.1008-2786.000109]
 ZHANG Xinbao.Discrimination of Quaternary Glaciation in the Lushan Mountain of East China by Using Vertical Geomorphology Zone Theory[J].Mountain Research,2016,(02):129-133.[doi:10.16089/j.cnki.1008-2786.000109]
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运用地貌垂直地带性理论判别庐山第四纪冰川有无()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2016年02期
页码:
129-133
栏目:
专家观点
出版日期:
2016-04-01

文章信息/Info

Title:
Discrimination of Quaternary Glaciation in the Lushan Mountain of East China by Using Vertical Geomorphology Zone Theory
作者:
张信宝
中国科学院水利部成都山地灾害与环境研究所,四川 成都 610041
Author(s):
ZHANG Xinbao
Institute of Mountain Hazards and Environment, CAS,Chengdu 610014,China
关键词:
地貌垂直地带性 岩性 赣北庐山 浙西千里岗山 第四纪冰川
分类号:
P931
DOI:
10.16089/j.cnki.1008-2786.000109
文献标志码:
A
摘要:
庐山东约300 km的浙西千里岗山,海拔1 523 m,高于庐山1 474 m,山顶出露岩层为夹粉砂质泥岩的岩屑石英砂岩的志留系上统唐家坞组,岩性软弱。以赣北庐山为代表的中国东部第四纪冰川问题,是我国地质、地理学界争议最大、认识最分歧的重大问题,“庐山第四纪冰川”认识分歧的重要原因是山地侵蚀地貌形态和相应堆积物的多解性。依据地貌垂直地带性理论,软弱岩层的分布高程,不可能超过冰川地貌带上限,也就是说,没有达到冰川地貌带的高度。为此,通过 “跳出庐山看庐山”,判别庐山第四纪冰川的有无。认为,千里岗山与包括庐山在内的邻近地区的同高程山地的高度无第四纪冰川发育。

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相似文献/References:

[1]张信宝,吴积善,汪阳春,等.川西北高原的地貌垂直地带性与寒冻夷平面[J].山地学报,2006,(05):607.

备注/Memo

备注/Memo:
收稿日期(Received date):2015-10-11; 改回日期(Accepted): 2015-10-19。 作者简介(Biography):张信宝(1946-),男,江苏镇江人,博士生导师,现从事地质地貌研究。[Zhang Xinbao(1946-),male, was born in Zhenjiang, Jiangsu province, professor, mainly engaged in research of geomorphology.] E-mail:zxbao@imde.ac.cn
更新日期/Last Update: 1900-01-01