| 湘东南某市地形地貌对地质灾害发育规律的控制作用分析 |
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| 引用本文： | 金福喜,罗滔,李杰.湘东南某市地形地貌对地质灾害发育规律的控制作用分析[J].中国地质灾害与防治学报,2014(2):115-118. |
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| 作者姓名： | 金福喜 罗滔 李杰 |
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| 作者单位： | [1]中南大学有色金属成矿预测教育部重点实验室,湖南长沙410083 [2]郴州市气象局,湖南郴州423000 |
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| 摘 要： | 地形地貌是崩塌、滑坡、泥石流等地质灾害活动的基础，它在很大程度上决定了崩塌、滑坡、泥石流等地质灾害能否形成及其类型、数量、密度和规模大小。本文基于湘东南详细地质灾害调查成果，对该市不同地貌类型、坡形、坡度以及高程的差异对地质灾害发育规律的控制作用进行了总结分析。
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| 关 键 词： | 地貌类型 坡形 坡度 地质灾害 |
The analysis of the control action of geography of the development rule of geological hazard in a city of the South-east of Hunan province |
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| JIN Fu-xi,LUO Tao,LI Jie.The analysis of the control action of geography of the development rule of geological hazard in a city of the South-east of Hunan province[J].The Chinese Journal of Geological Hazard and Control,2014(2):115-118. |
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| Authors: | JIN Fu-xi LUO Tao LI Jie |
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| Institution: | 1. School of Geosciences and Info-Physics, Central South University, Changsha 410083, China; 2. ChenZhou Meteorological Administration, ChenZhou 423000, China) |
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| Abstract: | The geography and landform are the basis of occuring ecollapse, landslip, debris flow, which determinesthe collapse, landslide, debris flow and other geological disasters can form and type, quantity, density, scale to alarge extent. Different geography types, slope, slope shape and elevation lead to different scale types of geologicalhazards. |
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| Keywords: | geography slope shape gradient geological hazard |
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