| 河北山地的次生层状地貌与新构造分区 |
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| 引用本文： | 吴忱,张秀清,马永红.河北山地的次生层状地貌与新构造分区[J].华北地震科学,2000,18(3):1-8. |
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| 作者姓名： | 吴忱 张秀清 马永红 |
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| 作者单位： | 河北省科学院、计委地理研究所,石家庄,050011 |
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| 基金项目： | 中国科学院资助项目，河北省自然科学基金，49371008，497337，， |
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| 摘 要： | 次生层状地貌是同一期地貌面（原生层状地貌），经过后期地壳构造运动的变形、解体而形成不同高度的地貌面。它较好地反映了第四纪以来新构造运动的方向、幅度与速度。据此，本文将第四纪以来河北山地的新构造划分出两个区、七个亚区和二十四个小区。
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| 关 键 词： | 河北 新构造区划 第四纪地质学 次生层状地貌 |
| 修稿时间： | 1999-09-25 |
SECONDARY STRATOLANDFORM AND NEOTECTONIC DIVISIONS IN THE MOUNTAINS OF HEBEI PROVINCE |
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| Wu Chen,Zhang Xiuqing,Ma Yonghong.SECONDARY STRATOLANDFORM AND NEOTECTONIC DIVISIONS IN THE MOUNTAINS OF HEBEI PROVINCE[J].North China Earthquake Sciences,2000,18(3):1-8. |
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| Authors: | Wu Chen Zhang Xiuqing Ma Yonghong |
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| Abstract: | The secondary stratolandform is a contemporaneous surface configuration in different elevation(original stratolandform)which formed by crust deformaion and dismission later.It reflects the tendency,strength,rate of the neotectonic movement since the Quaternary.Based on this point,the mountains of Hebei Province is divided into two parts of the neotectonics,subdivided into seven subareas and twenty four of smal subareas. |
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| Keywords: | Hebei province neotectonic division Quaternary geology quantitative geomorphology |
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