| 冀中南黄土潜蚀地貌与黄土构造节理* |
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| 引用本文： | 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. |
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| 作者姓名： | 王景明 王君 |
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| 作者单位： | 唐山工程技术学院 |
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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。
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| 关 键 词： | 黄土潜蚀地貌 黄土构造节理 |
| 收稿时间： | 1992-04-26 |
| 修稿时间： | 1993-07-27 |
LOESSIC CORROSION LANDFORM AND LOESSIC TECTONIC JOINT IN THE MTDDLE SOUTH OF HEBEI PROVNCE |
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| Wang jingming,Wang jun.LOESSIC CORROSION LANDFORM AND LOESSIC TECTONIC JOINT IN THE MTDDLE SOUTH OF HEBEI PROVNCE[J].Geographical Research,1994,13(1):90-93. |
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| Authors: | Wang jingming Wang jun |
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| Institution: | Tangshan Institute of Technology |
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| 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. |
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| Keywords: | Loessic corrosion Land form Loessic tectonic joint Tectonic foundation |
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