IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
横断山区地貌特征
Alternative TitleGEOMORPHOLOGIC CHARACTERISTICS IN HENGDUAN MOUNTAIN REGION
刘淑珍; 柴宗新
Corresponding Author刘淑珍
1986
Source Publication大自然探索
ISSN1000-4041
Issue1Pages:139-143
Contribution Rank1
Abstract横断山区是青藏高原的一部分,是第四纪以来强烈隆起的年轻山地,也是我国著名的高山深谷区,地貌形态独具特色。区内山川相间并列、南北纵贯,岭谷高差悬殊,新构造运动活跃。
Other AbstractThe Hengduan Mountain Region which is a part of the Qinghai-Xizang p1ateau is the youngestmountain rising up fron Quaternary .So it has become a famous region with high mountains and deep gorges. The geomorphologic characteristics in Hengduan Mountain Region are as follows, The altitude is getting lower from north to south in stairs. The alternate mountains and rivers are in parallel. The relative height from vallq to peak: is very large. The topography of stratification is obvious in vertical profile. There are many basins in the region, and the areal extent of structural basins is more large than others.
Keyword横断山区 地貌形态 新构造运动 高山深谷 剥蚀面 海拔高度 夷平面 沙鲁里山 喀斯特地貌 山顶面
Indexed By其他
Language中文
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/7906
Collection成都山地所知识仓储(2009年以前)
Corresponding Author刘淑珍
Affiliation中国科学院成都地理研究所
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Corresponding Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
刘淑珍,柴宗新. 横断山区地貌特征[J]. 大自然探索,1986(1):139-143.
APA 刘淑珍,&柴宗新.(1986).横断山区地貌特征.大自然探索(1),139-143.
MLA 刘淑珍,et al."横断山区地貌特征".大自然探索 .1(1986):139-143.
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