蒋家

蒋家沟流域松散砾石土斜坡滑坡频发原因与试验模拟

Cause of frequent occurrence of gravel slope landslide and experiment simulation

快速评价分散流异常的沟系原、次生晕方法蒋家沟流域的地貌与泥石流

The Ravine System Primary-Secondary Halo Method for Fast Evaluation of Dispersion Train Anomalies

泥石流突发性流动和剪切稀化的相关研究&以云南蒋家沟泥石流为例

Research on the correlation between sudden flow and shearing dilute in debris flows

蒋家沟泥石流堆积体的抗剪强度试验

A test for shear strength of debris flow deposits

由此表明，试验得出的表面流速公式符合实际情况，反映了蒋家沟泥石流运动规律。

It seems to be reflection of movement law of debris flow in Jiangjia Ravine .

分析了蒋家沟流域内特殊环境下崩中有滑、滑中带崩的特殊形式的滑坡。

The special landslides with slide and collapse in Jiangjia debris flow valley is studied .

试验证实，蒋家沟流域暴雨、滑坡、泥石流共生关系中含水量分布有一定范围。

The correlation among rainfall , landslide and debris flow is revealed with the moisture content distribution changed .

然而，战争的种种麻烦问题，还是在蒋家官僚统治机构内部，造成了心理上和物质上的紧张。

Nevertheless , the troubles of the war had produced psychological and material strains within Chiang 's governing bureaucracy .

云南蒋家沟泥石流区干热退化山地引种拟金茅的技术与效果

Technique and results of common eulaliopsis ' application on xerothermic Degraded Mountain in Jiang Jia Gou debris flow gully

建立了蒋家沟砾石土强度与粗粒含量、粒径分布曲线特征指标值、含水率以及干密度的关系。

Found the relationship between direct-shear strength and coarse-content , characteristic index of grain distributed curve , wate-content and dry-density . 3 .

受流域内物质成分、气候条件和复杂侵蚀营力的影响，蒋家沟流域坡面侵蚀现象甚为严重。

The slope in Jiangjiagou Valley suffered from serious erosion due to the substance components , climate and the complicated erosion power .

蒋家沟泥石流滩地地势平坦，水源充足，热量丰富，是较好的土地资源。

Debris flow waste-shoal land , with proper sunshine and abundant water resource and gentle slope , is a kind of land resource in Jiangjia gully .

总结了蒋家沟金矿成矿地质背景和矿床地质特征，对矿床成因进行了探讨。

This paper , based on mass of practical work , summarizes the geological background and geological features of Jiangjiagou Gold deposit and discusses the genesis .

该文拟在作者所建泥石流沉积模式基础上，以蒋家沟为例进一步讨论泥石流亚相的组合及变异规律。

On the basis of depositional model of debris flow built by author , the combination and variation of depositional sub facies of debris flow on the Jiangjiagou valley , Yunnan Province , was discussed .