| 苏北低山丘陵的地貌特征和地貌分区 |
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| 引用本文： | 黄志强.苏北低山丘陵的地貌特征和地貌分区[J].徐州师范大学学报(自然科学版),1991(3). |
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| 作者姓名： | 黄志强 |
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| 作者单位： | 徐州师范学院科研处 |
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| 摘 要： | 苏北低山丘陵区层状地形发育,具有多层次的地貌结构,系新生代以来以断裂和断块活动为主的内力地质作用和以流水侵蚀作用为主的外力作用相互结合的综合作用的产物。本文依据构造运动发展过程的差异和岩性的不同,将苏北低山丘陵划分为三个次一级的地貌区并分别进行了地貌类型的划分。
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| 关 键 词： | 苏北低山丘陵 地貌待征 地貌分区 |
TOPOGRAPHIC CHARACTERSTICS AND TOPOGRAPHIC PROVINCES DIVISION OF HILLS OF THE NORTHERN JANGSHU |
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| Huang,zhiqiang.TOPOGRAPHIC CHARACTERSTICS AND TOPOGRAPHIC PROVINCES DIVISION OF HILLS OF THE NORTHERN JANGSHU[J].Journal of Xuzhou Normal University(Natural Science Edition),1991(3). |
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| Authors: | Huang zhiqiang |
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| Institution: | Huang zhiqiang |
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| Abstract: | In the hills of the northerm Jangshu layered landform has been develeped, It is the compre-nensive products of internal agents-they mainly are fault and fault-block activities-and exterion agents-it is mainly are running water.Based on the developing history of tectonic movement and the difference in lithology, the region of the northern Janshu may be subdivided into three topographic province. The classification tepographic type has been made. |
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| Keywords: | hills of the northern Janshu topographic characteristic topographic province division |
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