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地理研究 >

1994 , Vol. 13 >Issue 1: 90 - 93

DOI: https://doi.org/10.11821/yj1994010012

论文

冀中南黄土潜蚀地貌与黄土构造节理*

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  • 唐山工程技术学院

收稿日期: 1992-04-26

  修回日期: 1993-07-27

  网络出版日期: 1994-03-15

基金资助

* 国家自然科学基金资助项目(4907012)

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LOESSIC CORROSION LANDFORM AND LOESSIC TECTONIC JOINT IN THE MTDDLE SOUTH OF HEBEI PROVNCE

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  • Tangshan Institute of Technology

Received date: 1992-04-26

  Revised date: 1993-07-27

  Online published: 1994-03-15

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摘要

本文对冀中南黄土分布区的潜蚀地貌进行了研究后发现,与我国西北黄土区一样,该区黄土潜蚀地貌具有区域性、方向性和空间分带性特征,黄土构造节理控制了相应地区的潜蚀地貌形态、展布方向和发育程度,是黄土潜蚀地貌的构造基础。

关键词： 黄土潜蚀地貌; 黄土构造节理

本文引用格式

王景明, 王君 . 冀中南黄土潜蚀地貌与黄土构造节理*[J]. 地理研究, 1994 , 13(1) : 90 -93 . DOI: 10.11821/yj1994010012

Abstract

Through the survey of the loessic corrosion landform inthe middle south of Hebei oprovince,it is found that the loessic corrosion landform is regional,directional and zonal;the loe-ssic tectonic jojnts control shape,direction and growth of loessic corrosion landform in the relevant area,and they are tectonic foundation of loessic corrosion landform.

Key words： Loessic corrosion Land form; Loessic tectonic joint; Tectonic foundation

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