地理研究

地理研究 ›› 1994, Vol. 13 ›› Issue (1): 90-93.doi: 10.11821/yj1994010012

• 论文 • 上一篇    下一篇

冀中南黄土潜蚀地貌与黄土构造节理*

王景明, 王君   

  1. 唐山工程技术学院
  • 收稿日期:1992-04-26 修回日期:1993-07-27 出版日期:1994-03-15 发布日期:1994-03-15
  • 基金资助:
    * 国家自然科学基金资助项目(4907012)

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

Wang jingming, Wang jun   

  1. Tangshan Institute of Technology
  • Received:1992-04-26 Revised:1993-07-27 Online:1994-03-15 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

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

PACS: 

  • P931.6