| 韩家湾滑坡特征及成因探讨 |
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| 引用本文： | 沙德智,左晓君.韩家湾滑坡特征及成因探讨[J].四川地质学报,2000,20(1):64-67. |
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| 作者姓名： | 沙德智 左晓君 |
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| 作者单位： | 凉山州地质环境监测站,西昌 |
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| 摘 要： | １９９８年９月，木里县城北侧韩家湾发生了两处滑坡，一为中型土质厚层滑坡（Ｈｈ１），一为大型土质中层滑坡（Ｈｈ２），二者均属老滑坡局部复活。特别集中的及连续长时间的降雨过程是主要触发因素；特殊的地形地貌，地质结构，堆积物是内在因素；多种不合理的人为因素，影响和加速了它的滑动。
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| 关 键 词： | 老滑坡复活 土质滑坡 韩家湾 成因 降雨 |
CHARACTERISTICS AND GENESIS OF HANJIAWAN LANDSLIDES |
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| Sha Dezhi,Zuo Xiaojun,Yin Pihua.CHARACTERISTICS AND GENESIS OF HANJIAWAN LANDSLIDES[J].Acta Geologica Sichuan,2000,20(1):64-67. |
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| Authors: | Sha Dezhi Zuo Xiaojun Yin Pihua |
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| Abstract: | Two landslides (Hh 1,Hh 2) too place at Hanjiawan to the north of Muli county town in September,1998 They result from partial reactivation of old landslides induced by mass and continuous rainfall and quickened by special landform and geological structure as well as human activity |
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| Keywords: | reactivation of old landslide soil landslide Hanjiawan |
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