| 长江上游重庆——碚石段沿岸滑坡与水动力作用的关系 |
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| 引用本文： | 刘尚忠.长江上游重庆——碚石段沿岸滑坡与水动力作用的关系[J].国土资源遥感,1990,1(1):47-52. |
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| 作者姓名： | 刘尚忠 |
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| 作者单位： | 四川省地矿局科研所遥感站 |
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| 摘 要： | 文中通过对长江河型、河谷地貌及水动力状态的分析研究, 指出长江上游的岸坡稳定性除了 与岩性、构造条件有关外, 特别强调了河谷地貌和水动力作用在滑坡形成中的作用。并以1982年7月再次滑动的四川省云阳县鸡扒子滑坡为例, 指出现在的治理措施没有考虑河流地质作用是不适当的。
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| 关 键 词： | 长江 沿岸 滑坡 水 动力作用 |
A RELATIONSHIP BETWEEN RIVERINE LANDSLIDE AND HYDRODYNAMISM IN UPPER COURCE OF YANGTZE RIVER(THE SECTION FROM CHONGQING TO PEISHI) |
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| Institution: | The remote sensing station Sichuan Sureau of Geology &; Mineral Resource |
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| Abstract: | In this paper analyses of stream pattern and fluvial land form and hydro logical regime suggest that a stability of shore Yangtze's in addition to lithlogical character and structural condition, depends particularly on a roe fluvial land form and hydrodynamic process in formation of landslides along the upper course. For example a remobilization of landslide at Jipaz Yunyang County Sichuan Province on July 1982 shows that no considering geologic process of river has been landslide controlled is inopportunely. |
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